River Bazaja, Krasnoyarsk Territory, Russia. Geological Essay - Museum of Geology Middle Siberia River Bazaich Water consumption for seasons Hydrograph

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Name	A type	Transport	Distance	schedule
Maganskaya	stopping point	a train	12 km.	schedule
Berezovka	stopping point	a train	12 km.	schedule
Lugovaya	stopping point	a train	13 km.	schedule
Shushun	stopping point	a train	14 km.	schedule
Kamas	stopping point	a train	14 km.

Bazaha

at the wedding of a speleologist Sasha Torgashina

Torgashinsky surname
Krasnoyarsk on it
Founders of Siberia.
Live in which

And do not believe - here are examples
And see like a movie
Torgashinsky Cave
And village Torgashino

In the edge of unknown and wild
Ancestors with don got
Build red born
Prafundam in our life

And cut down this city
That in which we live
Time turns the gate of life
You twist it together

Good memory is disturbing
Persena Pradedov Lichy
Save and multiply
Nice genus Torgashina

Remember the great-grandfather examples
And not just like a movie
Torgashinsky caves
And village Torgashino

Another miracle of the Krasnoyarsk nature is covered by the green curtain of the Torgashinsky ridge - the suburban park of the Bazaja River.

Bazaha, Bazaja
Siberian beauty
In the blue Dahl wwel
Like the girl's maiden
(Tourist Song)

According to the folk legend, Bazaha - Princess, the eldest daughter of Tsar Yenisei, which Prince Tokmak did not want to take into his wife for the temper the grumpy and violent. And indeed, the moral river at the river is cool: it swells, flouring the stones and washing the bridges, then it hits the state of a solid fusion. At the end of the autumn, there is a long fighting, not inferior to frost, all in patterned wormwood - for rapid diver birds: black water sparrows-Olenapok. Even in the winter sleep, the wayward river suddenly splashes over the ice shell, turning the winter paths of people into icy swamps. Bazaja begins in the Mansk district at the Krasnoyarsk Range - an amazing maternity hospital, the place of the eternal birthday of four suburban rivers: Bazai, Berezovka, Esaulovka, Fish. The origins of the Bazaaa - the enchanted edge for the researchers of underground worlds.

Here are known: a beautiful partisan cave, vertical caves - traps, a crystalline cave, dried with transparent plates of Icelandic spam, a hydrothermal cave with unique spheracts formed in hot pairs of an uptrestic mineral source in hot pairs of an uptreten mineral source. In the cave, the underground graveyard on the ground was found on the ground. There is a mountain crystal field, endangered streams, fields of karst funnels, vocal sources - natural siphons feed on underground watercourses.

All of its 128 kilometers of Bazaha rushes to the north-west, but at the same time, loops continuously, as if trying to confuse the trail. Embedded hinges (Meandra) Memory that once the river was a languid, flat lace, slowly twisting from the side to the side towards whimsical loops of the steppe waltz. Slowing the territory forced the river to bite into rock rocks, bruting the memory of an ancient plain into the mountains.

Even recently, the inverent princess was a slave of a man of challenged it for a forest with a lot of dams, dams woven from cables and logs of giant ropes - Bon. Now Bazaaha is a free mountain-taiga beauty, to which a person comes mostly only to visit: to travel in Siberian Gres, to go fishing, buying.

In the upper reaches of the river on the site of an ancient settlement, Herlybvka is a stationary recreation camp, and several villagers adapted under the cottages, and only rare forest cordons are only rare eighty kilometers below the river. In the lower reaches from the marble career, cottages are walking, at the very border of the reserve, and the former country of pioneer has stretched out, a chain of children's holiday camps, ending with the camp "Krasnoyarsk poles".

Bazaja - Border River, separating the Torgashinsky Ridge and Kuysum Mountains, it from the mouth of Great Injul is the northeastern border of the "Pillars" reserve and enters His security zone.

Traveling around Bazaha all year round: in winter skiing, in the summer of Peshe Brod, in May alone on the rowing ships. Here you do not build up like on mana. Fast, narrow hiding watercourse makes it constantly wary, not releaseing oars from the hands. The main danger is "Combs": the underworn trees capable of "combat" all from the decks, and the rubber vessel to be existed in shreds. It happens that if the whole crew is smoking, someone one reaps a lot of cigarettes every time and carefully picks up everyone in his teeth, so that smoke went.

However, a modern alloy does not compare with water fun 50s. Water tourism has not yet existed, the river was blocked by cascade of watelling dams and at the time of resetting the water of the Bazaja turned into a roaring stream with artificial waterfalls, with jumping and routing logs, many of which sailed to the mouth of the cortex.

What kind of need could make it go to this ice, roaring hell, albeit with the sun? But what Russian does not like quick ride? And what was the ride in those pores: neither horses, no cars, except from the top of the "feathers" to rush on their shoulders. Some unknown sage thoughtful to weigh a narrow fleet - Sallic of car cameras and the matter went. There was nothing: neither rescue vests, nor casak, nor cheerful, not the slightest concept about alloy technique. I wrapped with short poles, chopping from the clashes, small places and logs. At the entrance to the throat of the water-boss, the dam standing on the nose was to have time to spread the water-locking bars on the go, and here he is a flexible film on the ridge of the waterfall. At the fact that the oncoming tree overthrew the raft, and everyone turned out to be under water. They danced, raft saddled and with a cheerful laughter and Gicani rushed on a furious Bazaha to the next dam, to the next flight. Now it seems strange, but for some reason no one is shattered and did not even bete in the snow.

In the spring there are 2-3 days when the famous Siberian Harius rushes to spawning from Yenisei to the basehouse. This time is easy to determine the frequent figures of fishermen, lowering square meshs - screens that are suspended with thin poles. This forbidden method strongly undermines fishing. A lucky poacher for the spring night climbs up to five hundred fishes, which otherwise you can't call the genocide. Harius Fish in all respects is wonderful, one of the living symbols of the purity of Siberia. In a warm, quiet, muddy, dirty river, the Harius is not found, it gives crystal mountain streams. Among the residents of the underwater kingdom of Harius can be safely considered a climbing champion. It happened, puffing from the last strength, will take a two-kilometer Sayan pass to the upper border of life. Circle snow, yes a stone, and only rare insects and lichen. And suddenly, in the source of a ring key, in a stone jam with a bucket size ... Harius. Each autumn Carius "rolls" into large rivers, where and winter, like a bear, in some quiet, deep waters - the fishing kingdom of Morpheus. How many kilometers sailed in the spring this fish, overcoming the rigs, thresholds, waterfalls, jumping along the coastal stones bypassing especially high waterfalls so that here in a tiny stone aquarium, in the most underground snow to bring offspring? Real fishing on Harius, without any grids and wisdom of ships, high poetic art, and the sport is a fry of the nobility hunt. Instead of a medieval bolad fuss of confusion of a doomed beast - Mountain fishing, elegant, almost honest game of the mind and muscles of a person with the harsh beauty of nature. What is the ability to make a snag in the form of some insect of the most incredible girlfriend. There are masters, months, pursuing some red peasant to raise one or two curl of a fiery beard. It is necessary to have a fiery passion for freedom, legs and breath of deer to get up to dawn, go all day along the river cascades, Shiver, presses. Over the lured cattle, a flieper must dissolve in the landscape, so that the fish will not see the shade or the slightest movement. Then the masterfully played the scene of the fluttering flies. And here it is a bright moment, sparkling the silver lightning of the fish, exploding the water surface! Strong, rapid fish is often breaking off the hook in flight and even on the shore, time to go into the water. Fisherman who caught all day thirty smoking, happier from people. And this is a sparkling miracle, Sayan Silver Lightning, exterminate thousands right in the city near the bus stops.

Bazaha, with all its hemacities, urmanans, the floodplain - the most interesting natural complex for those who learn to read the live book of nature. Together with the border of the reserve along the river, the boundary of the dark coniferous taiga (left, protected bank) and secondary, clarified forests with a predominance of pine trees along the arid Torgashinsky ridge. All significant tributaries (Corrikik, Golev, Injul, Namurt, Sonzhul, Kaltat, Mokhovaya) fall on the left, and Torgashinsky right bank gives only stingy tears of small keys (Bulgarian, War, Yahontov, Cheerful, Ilkin Key). Thanks to the nature reserve, there are all animals of representatives of the South Siberian taiga, but the Torgashinsky shore in turn enriches the living palette of the reserve.

There are plants that are not characteristic of this area of \u200b\u200bthe mountains: Yellow Alpine Maks, Alpine Asters, Kuril Tea, Edelweissy, Gonia Limana, some orchids and lilies. There are also plants of Khakass steppes and plants characteristic of West Siberian lowland. These plants are a living memory of other geological epochs, and are called relic.

The same typical mixing of borders and fauna for redaries, reigns in the bird's kingdoma. During the year, it is possible to observe up to two hundred species of birds related to the Siberian fauna (white oatmeal, oatmeal Remez, bakingbird oatmeal, black thunderbreaker). To the Chinese fauna (hedge of gray-headed, oatmeal-dubrovnik, South Asian revenger Zhulan). To the European Fauna (Oriole, Schegol, Singer Drozd, Forest Horse).

Some birds belong to the mixed Siberian-Chinese fauna (a deaf cuckoo, a mukholovka small, foam-kings, drooping of an earthen, nightingale-redish, nightingale whistles, nightingale blue). There are views of the Siberian fauna related fauna North America (Lapland to riot, three-pailed woodpecker, checkl).

The Valley of Bazahai is also interested in the fact that the Krasnoyarsk archeology began here. At the beginning of the 1880s, Krasnoyarsk Teacher A.S. Elenekh in the lower reaches of the Bazaai at the rocks of the Kyzi at the mouth of the mossy spread the gun of the man's era of early iron.

Light, surface strokes, we turned around the circular panorama of the Krasnoyarsk neighborhood, so that it was clear that if the Krasnoyarsk poles are diamond, then this diamond is concluded in a decent frame. The talented and wise father-founder of Krasnoyarsk, driven by the Divine Nativity, placed us in the beautiful bowl of the flowering of life, in the magic vessel of all the existing, created for flowering and knowledge and name to her "Krasnoyarsk Academy of Live Nature". Here every step opens the depths of knowledge, calling to creation. The amazing crossing of the living nerves of the planet, the space body of the feelings existing to talk with the universe, mind, God. Unfortunately, wildlife disappears so rapidly that it is already time to declare the entire Krasnoyarsk bowl by the reserve by and large. Not a prohibitive zone with non-painful and mercenary governors, but a protected area open to humans and to educate humanity.

Leonid Petrenko. Krasnoyarsk Madonna. Wildlife Academy of Arts. Bazaha

Owner: Petrenko Leonid Timofeevich

Provided: Petrenko Leonid Timofeevich

Collection: Leonid Petrenko. Krasnoyarsk Madonna.

The source of the Bazai River is located in the Mansk district, in the Krasnoyarsk Range, but most of her channel runs through the territory of the Berezovsky district. River Slazier mountain arrays And flows into the Yenisei.

Basaha - the right influx of Yenisei, the length of the water branch is almost 128 kilometers. Next to the source of the river is the abandoned village dry Bazaha. Mountain streams, rods and a few small rivers: Dolgin, Korbik, Namurt, Golevik and Kalgat are falling into the base. All these rivers are its right tributaries.

The mountainous terrain on which Bazaha is flowing is very beautiful. High mountains covered with coniferous and mixed taiga, sheer brown and reddish rocks, Kurubniki fit straight to the water. In many places, the cutting rivers resemble the canyons.

The river is fast, water has a swamp or brownish tint due to the abundance of clay particles and yals. During summer rains, water is greatly rises and the course becomes rapid. From Namurt, the river bed significantly expands, the river is wriggled, forming Meandra and leaving the old men.

The Bazaja River (middle and lower current) is the natural border of the "Pillars" reserve.

Bazaha is rich in fish. In her waters, Harius, Lenok, Elets, Nalim, Ersh, Pike, Okun, in the middle of the river and the upper reaches are taped. Even an inexperienced fisherman will never remain here without catching, so Bazaha is a favorite fishing destination residents of Krasnoyarsk and its satellite cities.

At the Bazaha, the top bauzaah, hectic and Zhistik are standing on the river, on the river you can find and abandoned village, which wears the name of the Corrick.

Krasnoyarsk is a millionth city and regional center. The lower flow and mouth of the Bazaaa are located in the urban feature of Krasnoyarsk (areas of Laretino and Bazaja).

You can get to the river from Krasnoyarsk, through the "Pillars" reserve, as well as on forest roads, bonding villages, standing on the banks of Bazai.

Country

Russia, Russia

Region To: Alphabetically rivers: Water objects according to the alphabet to: rivers up to 500 km long to: River card: Fill out: Coordinates of the source of the river over one hundred km Bazaha (river) of Bazaha (river) to: River card: Fix: source height

Description of the river

The average annual water consumption is 5.0 m³ / s. The largest tributaries: Namurt, Caltat, Dolgin, Great and Corbik.

On the banks of the river, when a falling in Yenisei, in 1640 the village of Bazaich was founded. The village was adjacent to a high mountain ledge, which was called the settlement, or mountain sofa. In the XVII century, the Tatar fortress, which the Russians called the "serpentine settlement" were located on the flat top of the mountain, the sofa.

In the XIX century, on the banks of the river, the residents of Krasnoyarsk built their cottages.

In 1931, the construction of a woodworking plant began in the area of \u200b\u200bthe river in the village of Bazaich, after which the village was included in the devil of Krasnoyarsk.

On the left bank of the Bazaha, next to Bolgshov, on the territory of the post reserve, a marble quarry worked.

Tourism

The river is suitable for tourist alloys during the spring flood. The tourist route of the second category of complexity began from the village of Yrelykovka. At the threshold, Absatak was carried out by kayakovnikov competitions.

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Literature

• Velichko M. F. Little travel around a big city. - Krasnoyarsk: KN. Publishing house, 1989. ISBN 5-7479-0148-6

Links

Notes

Inflows (from 100 km) Big Yenisei · Small Yenisei · Elecest · Chemchik · Us · Cantieger · Oya · Abakan · Tuba · Fold · Kill · Sisim · Derba · Mana · Bazaha · Kacha · Esaulovka · Kan · Buzim · Shilka · Yulodkina · Angara · Kem · Big Pete · KIA · Pucheglazic · Purity · TIS · CAS · Galaktionich · Smoke · Spoon · Dubsch · Podcatent Tunguska · Big Varlamka · Bacht · Sachchikha · Upper Abbank · Yezhoguy · Komsa · Artugina · Nizhny Abbak · Fatyaniha · Paculikha · Dry Tunguska · HPP Channels

Excerpt that characterizes Bazaha (river)

Arriving home, Pierre gave orders to his all knowledgeable, everything who knows how to know the whole Moscow to Evstafyevich that he goes to Mozhaisk to the army and so that his riding horses were sent there. All this could not be done on the same day, and therefore, according to Evstafyevich, Pierre had to postpone his departure to another day, in order to give the time to the stands to go to the road.
The 24th point cleared after bad weather, and on this day after dinner Pierre left Moscow. At night, the change of horses in Perhushkov, Pierre found out that this evening was a big battle. They told that here, in Perhushkov, the earth was trembling from shots. Pierre's questions about who won, no one could give him a response. (It was the battle of the 24th day at Shevardine.) At dawn, Pierre drove to Mozhaisk.
All Mozhaisk's houses were busy standing by the troops, and at the inn of the courtyard, on which Pierre met his Beretor and Kucher, there was no place in the hillside: everything was full of officers.
In Mozhaisk and for Mozhaisk, the troops were stood and went. Cossacks, hiking, equestrian soldiers, wagons, drawers, guns visible from all sides. Pierre rushed to go ahead more, and the further he drove away from Moscow and the deeper the troops in the sea deeper, the more he was anxious anxiety and not yet experienced a new joyful feeling. It was a feeling similar to the one he experienced in the Slobodo Palace during the arrival of the sovereign - a sense of necessity to take something and sacrifice something. He now experienced a pleasant feeling of consciousness that all that makes the happiness of people, ease of life, wealth, even the lifetime, there is a nonsense, which is nice to lean in comparison with something ... with what, Pierre could not give a report, and She tried to understand myself for whom and for what he finds a special beauty to donate to everyone. He did not occupy what he wants to sacrifice, but the most sacrifice was a new joyful feeling for him.

On the 24th, there was a battle in Shevardinsky, the 25th there was not a single shot with any other side, the Borodino battle occurred on the other side of the 26th.
Why and how were the battles in Shevardine and Borodina were given and taken? What was the Borodino battle for? Neither for the French, nor for the Russians, it did not have the slightest meaning. The result of the nearest thing was and should have been - for the Russians that we approached Moscow (which we were afraid most in the world), and for the French, the fact that they approached the death of the whole army (which they were also afraid most in the world) . This result was then obvious, and meanwhile, Napoleon gave, and Kutuzov accepted this battle.
If the commander was headed by reasonable reasons, it seemed that it should have been clear for Napoleon, which, by going for two thousand versts and taking a battle with a probable accident of the loss of a quarter of the army, he walked to the faithful destruction; And as clear it would have to seem to be Kutuzov, that, taking the battle and also risking to lose a quarter of the army, he probably loses Moscow. For Kutuzov, it was mathematically clear how it is clear that if I have less than one checker in my checkers and I will change, I will probably lose and therefore should not change.
When the enemy has sixteen checkers, and I have fourteen, then I only on one eighth weaker than him; And when I change thirteen checkers, he will be three times stronger than me.

In the neighborhood of Krasnoyarsk, sedimentary rocks are widely developed - stratified formations of a variety of composition and genesis and a wide age range - from Rhypsian to Quaternary.

Upper Aprif Eratea (R 3)

The deposits of the upper reef (430-600 million years) are developed in the Basins of the River Man and Bazaja. Three suites are distinguished by lithological features: Umanskaya, Manx and Bakhtinskaya. Contacts with more ancient sediments are ubiquitous tectonic; The relationship between the suites in its composition consonants.

The URHAN retinue (R3UR) is composed of grayish-green, dark gray quartz-chlorite-sericite, chlorite-chlorite-chlorite, activated, carbon-siliceous, siliceous, chlorite-quartz-limestone and other shale, meta-penetrations with interlayers of marbled limestones, rarely dolomites. Breeds are often sulphidized and collected in small isoclinal folds. Power more than 200 m.

The mank retinue (R3mn) is composed of crystalline limestones with dark gray and black, tile, sometimes linked, with siliceous and phyllithoidal clay slates (with a capacity of up to 12 m), less often of metapplies. Power more than 600 m.

In the area of \u200b\u200bthe Krasnoyarsk, the Umansky and Mansk Sweet breed is limited, in small tectonic wedges in the area of \u200b\u200bthe lower flow r. Basaha. Limestones of mank suite in contact with the column array marbled.

The Bakhtinsky retinue (R3BH) is distributed in the vicinity of the city of Krasnoyarsk limitedly in the southern and southwestern part of the square (in the area of \u200b\u200bthe Northern contact of the Stolpan array near the observation platform of the "Poles" reserve above the "Bobrov Log"). Here it is developed exclusively in tectonic wedges, and the foundations of its breed are oroging under the influence of the columnist intrusion. In the adjacent territories, the Bakhtinsky retinue lies in the mank.

The Bakhtinsky retinue is comprehensive mainly by metabazaltami. At the bottom of the sewage in the bottom of Effusives, there are relaxes of bull-color and crystallastic tuffs of the main composition, chlorite-serisite shale and black silicon thin-dollar shale, less often - touffurgomerates.

For breeds of the Bakhtinsky suite, green, greenish-gray or dark-green color is characteristic, often they are declared and green-film changes are intense. Primary-magmatic minerals are usually practically aimed at epiidot, chlorite, serisite and carbonates. In the stratopic area opposite the village of Bakht and on the right bank of the River Mana, the retinue is represented in the lower part of basalts, laverebells of basalts, Andesibazaltami and their tuffs with rare interleavers of marbled limestone, dolomites and siliceous shale.

Power Sweet reaches 2000 m.

VENDAN SYSTEM (V)

Widespread on the square of the tube retin (VTB). Its deposits are made on both the right and left sides of the Yenisei River. On the left bank of the River Yenisei (in the vicinity of the village of Successful and below the mouth of a dog's river), the breed of the Sweet is francmed the extended lane strip and crumpled into complex folds.

Artificial exposure of sandstones Tubil Sweets by the road in the village of Successful. South stop

Calcite streaks in sandstones

Greenish gray sandstone color on fresh chop

On the right bank of the Yenisei, they are involved in the structure of the Grassaly Syncline. Separate fields are known along the Bazaja River, on the left bank of which the breeds are harvested under the influence of the column array.

Caltat fold. Right bank of Yenisei, not far from the mouth of the Kaltat River

Sweet is composed of polyminyt, mica, limestone sandstones, aleuroliths, clay shale, grave and black limestones. The painting of terrigenous rocks is dark gray, dirty green or greenish-brown. Texture is massive or layered. Layered parallel and wavy. Wedding signs of ripples and traces of raindrops. Serisite is often developed according to the planes. Limestones are dark gray, layered, bituminous, often clay. In general, the retinue is characterized by the thinthicular structure of the flesh type.

Budenzing structure

The breed of suite is often substantially declared. So, in a major artificial exposure on the right bank of the river. Bazaaha (near her mouth) There are intensive disjunctive dislocations of sediments of the suite and the fracture of several directions. The total capacity of the division is 950 - 1100 m.

The tube retinue is overlapped by Ovsynkovsky retinue. With the undermining sediments, the contacts are tectonic.

In the top of the suites, small skeletal residues of the tubular shape were found. Such fossils are found from Venda. The age of Sweet is adopted by the late owner (570-555 million years).

Ovsyankovskaya retinue (VOV). Sweet breeds create an extensive field in the vicinity of the villages of oatmeal and mucznevo. They are common in the area of \u200b\u200bthe village of Borovoye, as well as in the riverfire of the River Large Sliznevoy - Ruyech, where the nuclear part of the Majalyznevsky syncline is found.

The Dolomites, dolomitis limestones, lime dolomites, dolomite breccisses, rarely limestones, quartzites are found.

Kurumnik not far from the village of Osseanka

Dolomite rocks are diverse in color and texture. All shades of gray are observed (from light gray to dark gray), sometimes breeds are yellowish. Textures are massive and layered. A notable feature of dolomites are abundant microfitolites, especially oncolites and bubble cata charts. When weathered, the internal parts of the microfitolithol glats are leached, and empty shells are saved from them, because of which the breed acquires a porous appearance.

Plots of the breed of suite are crushed into complex folds and are broken by numerous disjunctivations, often they are very recrystallized or quarling. The power of the suite is estimated at 1000-1100 m.

Contacts Sweets with underlining sediments are mainly tectonic, however, in the river River of the Large mucneum and the rug of the ROOEV in the nuclear part of the Majols, its consonant in the tubing retinue is established.

Paleozoic Eratea (PZ)

Cambrian system (€)

Lower department (€ 1)

In the vicinity of Krasnoyarsk to the Lower Department of Cambria belongs to the Ungu and Torgashinsky Sweets.

Ungute retinue (€ 1UN). Allocated by I.P. Zhuiko and V.V. Uzabetov in 1959. Passionate is located in the village of Village Big Uward.

Due to the fact that the composition of the individual parts of the UNNWAN Sweets is different and the variability of it on strike is noted, the types of cuts are allocated, for which its local names are taken.

The Karaulin type of cut is represented by carbonate sediments, developed along the Karaul River, as well as above and below its mouth along the left side of the Yenisei River. In addition to natural yields, the species breed here are opened by a quarry located in the left side of the Karaul River near the place of its sign in the River Yenisei. This type of incision has a single limestone composition, with dolomites in the lower part of the incision and the characteristic horizon of oncolite limestones with the "floating pebbles" - in the middle. The capacity is 800 - 920 m. Overlapping sediments are present only in one point - on the Karaoul River - and presented the thickness of the limestone conglomerates of problematic age (Cambrich?).

Artificial exposure. UNNWORD SWITE, CALTAT TYPE TYPE. Related limestone and aneurolite

Diggers of mudflows

Dike

The Caltat type of the Cultural Sweet is developed on the right bank of the Bazaja River, where its breeds are extended from the mountain red stone in the eastern direction at a distance of almost 12 km. Here, the retinue is predominantly dark limestones, greenish-gray and multi-color aleurolithic, marlamles and rare dolomites. For breeds, horizontal layers are characterized, even layering planes and abundant terrigenous impurity (Zadorozhnaya, 1974). The visible power of deposits in a typical section against the mouth of the Kaltat River - 263 m. The relationship of the suite in the Bazai River basin with underlying sediments is everywhere tectonic, with overlapping Torgashinsky retinue - consonants.

Many organic residues were found in the UNNGUT SPEET breeds. In the Karaulin type of section, it is, first of all, a small-glass fauna, the remains of ancient skeletal organisms ("Smallshellyfossils" or SSF). Among them are identified angryiocreides, holiths, gastryports, Tommotiyda, crustaceans of the tomot yarus (Sosnovskaya, Shurinova, 2003). The fossils are determined by the age of accompanying their deposits as the Rannectery (Tomotsky Century).

Torgashinsky retinue (€ 1TR) was highlighted by V. Zlatkovsky in 1885 by passionithizer is the incision of the Speat of the Torgashinsky Range. Here, its deposits, often creating high rock ledges (Mount Commelier, Mount Pioneer, etc.), occupy a significant area and are found as an axial part of the ridge and its slopes. Sweet deposits are also known on the left side of the Bazaich River. In contact with the rocks of the pillar intrusion, they turned into marbles.

The best incision of the suite is on the right bank of the Bazaja River, against the mouth of the Kaltat river. Due to the good nude and the presence of numerous organic residues, he has repeatedly visited by geologists, conducted by geological-filmmaking and thematic work on this territory. The main volume of sweates is composed with gray and light gray massive organogenic limestones. The subordinate role is played by layered limestone. In the upper part of the incision there are dolomites.

Crystal calcite

Calcite

Based on the cut, a peculiar pack of a bundle, which has a local name - Bazaika, is distinguished. It is folded by purple, light pink and gray lime grave, sandstones, thresholds and light-rose limestones. In the terrigenous rocks, angular debris of algae limestone are abundant. Cement carbonate with an abundant impurity of iron hydroxisals, with which the blocker color is connected. Below the mouth of Caltata among the motley-colored deposits there is a powerful reservoir of dark gray thin-dollar limestone and mergels with clay and dolomite assesses. In addition, in the pack of packs there are single algae bio-camels that form in the relief isolated rock outputs. In general, the breeds of the Bazaima pack are characterized by coarse slagness, wave row signs, abundant surfaces of erosions, poor drilling and sorting of the debris material. Outputs of packs stretch along the bottom of the southwestern slope of the Torgashinsky ridge, where its motley-colored rocks are clearly visible on the mountain red stone. On his northern slope of the bundle breed is known for the Panikovka stream and at the exit of the Cheremukha Log on the terrace of the River Yenisei. Its power up to 250 m.

According to N.M. Dororal (1974) Limestone Torgashinsky Sweets form a complex organogenic structure, which can be considered as a reef complex consisting of smaller elementary organogenic buildings (bio-genes and biosters) and concomitant breccchy and layered limestone.

Torgashinsky retinue is characterized by a very large number of birth and species of archeocyat and other groups of fossil organisms represented by complexes of various horizons of the Atdaban, Botomsky and Toyon tiers of Lower Cambrian. She lies according to the underlying sediments of the Ungu (Caltat) suite. But in some areas of the right bank of the Bazai River, their contact is complicated by the series of the main composition. In the Dead Development Field, layered carbonate rocks are intensively crumpled into the folds with the incidence angles on the wings from 30to to 85o. Above dackes are calm, with no more than 10 o. On the northern slopes of the Torgashinsky Range of the formation of Torgashinskaya suite, according to the Chessy retinue of the Middle Cambrian.

The total power of the sweet reaches 900 - 1000 m.

Limestone Sweets are also known in the area of \u200b\u200bthe Krasnoyarsk reservoir, where there are high picturesque rocks on the bays of the Bourish.

Fold. Rock redhead (creepy), southern slope of the Torgashinsky ridge

The carbonate composition of the suite and fracture developed in its sediments contribute to the manifestation of karst processes, including the formation of karst caves. The remaining karst relief with grottoes and arches is developed on the right slope of the Bazai River opposite the marble career. In the water-seed part of the Torgashinsky ridge there are funnels. There are eight caves here, the largest of which are Torgashinsky (length 3 km, depth 165 m) and ice (length of 720 m, depth 32 m).

Middle Department (€ 2)

The department includes carbonate sediments of the Chessy Sweet.

Shakhmatovsky retinue (€ 2sh) highlighted V.I. Popov and L.V. Yakakyuk in 1961. Passionithip is located in the upper course of the Bazaja River in the area of \u200b\u200bthe village of Chekhmatovo (outside the area of \u200b\u200bthe site).

In the area of \u200b\u200bthe training practice of the breed, the Sweets lay down the northern slopes of the Torgashinsky ridge. The retinue is represented by gray layered limestones, bright dolomites and dolomitic limestones, red-color aleurolites. The latter are rarely found in the form of unbearable concerns with a capacity of no more than 2-3 m. Due to the impurities of manganese carbonates, the suites often have a pink color. The power of the division is less than 300 m.

The limestones identified the trilobites of Olenoides convexuslerm., ErbiagraNulosa, E.Sibiricalerm., Amgaspis CF.Medius N.Tchern., A. Sp., Gaphuraspissp., Kooteniellasp., Proasaphiscussp., Proshedinellaerbiesissiv. et al., as well as algae epiphytonfruticosumvol., RenalCisGranosusvol.

Relationships of suite with the underlying Torgashinsky retinue consonants. The border is gradual and is carried out conditionally in a pack of limestones containing a reliable fauna of the trilobite of the lower part of the Middle Cambrian. More young sediments of Devon run disagreement or with tectonic contacts. The age of suites are determined by the finds of the trilobitis by the AMGINA century of the Middle Cambrian.

Ordigrian system (o)

Mid-Upper Departments (O2-3)

Iramskaya retinue (O2-3im). Volcanogenic breeds of suite, together with submulcanic formations, are part of the IMIR volcanic complex and are widespread within the Kachin-Shumihin depression, which is located in the north-western framed of the folded system of East Sayan. This structure is extended in the latitudinal direction 50 km west of the outskirts of the city of Krasnoyarsk and has a width of up to 30 km along the meridian. In the western part of depression (in the area of \u200b\u200bthe city of Divnogorsk), the Volkanogenic rocks of the Iramskaya Sweet studied in detail V.M. Gavrichenkov and A.P. Cosorukov. In the northern part of the territory, within the list of O-46-XXXIII, the cuts of the volcanogenic rocks of the Ordovik age were first described by E.I. Berzon and V.E. Barsegian (Burson et al., 2001). And in the eastern part of the depression, on the slopes of the ridge, the long mane, subshir, stretching to the west from the mountain Nikolaev (first) Sopka - M.L. Makhlayev and O.Yu. Perfilova (Makhlayev et al., 2007; Perfilova, Makhlayev, 2010). According to the petrographic composition and structural-tectonic position, the volcanic complex of Kaczynsko-Shumykhin depression over the past few decades has been compared with the Byskar series of minusinsky deflection and belonged to early or early Middle Devon. But subsequently on the effusions of the northern part of depression and submulcanic bodies from the Divnogorsk section and were obtained by fairly reliable isotopic dates, according to which the age of the complex is medium-Lategorovik.

Nikolaev (first) hill

The breed of suitees with a sharp structural disagreement are listed on more ancient complexic education, and disagreely overlapped with red-colored sediments of the Middle Devon.

In general, at the bottom of the cut of the suite, moderately alkaline basaltoids predominate, in the upper effusions of the medium and moderate-sour-source (lava and tuffs of the foils, trachidacites, trachiriodocytes). The high power of the volcanogenic cut is characteristic. Only one continuous section along the Yenisei River near the city of Divnogorsk, in detail of the studied V.M. Gavrichenkov and A.P. Cosorukov, it is at least 2800 m.

Two subheads are allocated: Nizhneimymskaya trachibasalt-andesibasalt and uppermimemist trachyandzite-trachit-trachidacite.

Nizhneyimirovskaya litter (O2-3im1) in the rivers pools smooth and cool kaches, Bol. Minojul is composed by lava flows and seals of olivine, olivine-agitovy, AVGIT-plagioclase and plagiolazal trachibasant, trachyandezibazalt, less frequently traitnesitis with a capacity of 1 - 5 to 30 - 40 m. For the breeds of the central parts of the flows are characterized by a high degree of clarity, microdolerm structure and almost complete absence Glass Basis. In the direction of the roof and the sole of the stream increases the glass content. In the edge parts of the flows of volcanites, they have mainly pylotaxite structure. In the roof streams texture of rocks, as a rule, almoperative. There are few leather, vitro and crystallastic psammitic, psephite and psimmontal tuffs, tubes, tufoalurolites, vulcanic sandstones, are observed. In the lower part of the suite, the propellands of the tuberonelites and touffurgomerates are noted, which contains fragments of limestone Torgashinsky Sweet and Dolomites, probably oyshane suite. Cement Basal, basal pore carbonate pelite with chlorite admixture, clay-carbonate, carbonate, zeolite and clay and iron.

The total capacity is the details - from 350 to 1000 m.

Verkhneimimir system (O2-3IM2) is composed of lava flows and cover of fools, trachidocytes, trachiriodocytes, less often by trachryirolys, andesitis and trachibasant, as well as their tuffs and tuffs. The border between the lower and the upper subimits is carried out by E.I. Berzon et al. On the change of substantially basaltoid vulcanites by the rocks of the middle and sour. Often, at the base of the top subimbat, there are tuffs of mixed composition.

As part of the upper backwards in the northern part of the depression in the Kasual and smooth river basins, lava flows predominate (with a capacity of 10-110 m) of fools, trachidacites, trachyrocytes, less often trachryolytes, as well as their tuffs. The breed of the upper backs are mainly painted in various shades of red and brown. Porphyry varieties prevail. Power subheads - up to 1800 m.

In the area of \u200b\u200bthe city of Divnogorsk, moderately alkaline acids (trachidacites, trachiriodocytes), which are missing in the eastern part of depression. Foils for this part, on the contrary, are not typical. The total power of the effusive cut here is somewhat larger than in the eastern part - at least 2800 m. Thus, the volcanogenic thicker is characterized by lateral non-abruptness, sharp fluctuations in the capacity of individual bodies by stretch.

The absolute age of the foils according to RB-SR isochronous dating amounted to 447 + 6 million years, and K-AR - 464 + 11, 452 + 11 and 467 + 11 million years. Previously, the age of these Effusion RB-SR was determined by the method - 442 ± 2 million years.

A number of geologists challenges the attribution of volcanogenic formations of Kaczynsko-Shumykhinsky depression to the Iramskaya retinue and proposes to allocate them under the local name Divnogorskaya stratum with the same age O2-3. (Kruk et al., 2002; Makhlayev et al., 2007,2008; Perfilova, Makhlayev, 2010).

Objects with uranium uranium-molybdenum formations and numerous manifestations of fluorite on both shores of the Krasnoyarsk reservoir are associated with the rocks of the Iramskaya Sweet. Volcanic rocks (fuchitis, trachidacites) in their physicomechanical properties meet the requirements of industry and were widely used to eliminate railway mounds and automobile roads. Some varieties of large-rigid volcanogenic rocks of the Iramskaya Sweet are decorative enough and can be used as a facing stone.

Devonian system (D)

Devon's deposits are widely developed in the territory of Krasnoyarsk and in its surroundings. They fulfill the Rybinsk depression, stretching from the North-Western suburb of Krasnoyarsk in the eastern and southeast direction, and are represented by all three departments of the Devonian system.

Lower department (D1)

Karymovskaya retinue (D1KR). The Karymovsky retinue begins the incision of Devonian deposits of the Rybinsk. Its deposits are stretched by a strip along the northeast foot of the Torgashinsky ridge from the village. Torgashino on the southern outskirts of the city of Krasnoyarsk in the direction of Mountain Black Cock and Petryshino station and further in the South direction.

The lower part of the cut has the terrigenous composition and is either allocated as Nizhnekaryum submissions (D1KR1) or is considered as an independent retinue - Assafyevskaya (D1as). Its deposit with structural disagreement is locked on a deeply blurred surface of the carbonate sediments of the Lower Middle Cambrian. This border and the above basal horizon of Assafyevskaya Sweets were opened in the eastern wall of the Career "Wavembar" opposite Krasnoyarsk CHP-2. Here, developed on limestones, the Torgashinskaya Sweets, the surface of the erosion with deep (up to 0.8 m) pockets above which are lower than the photolurah terrigenous sediments. "Pockets" in limestones are filled with poorly sequential nonlocheliy aleurolites of gray-green color. Above the incision of the basal horizon is increasing with fine-mediated sandstones with parallel and oblique lamination. Sands of sandstone sandstone and burgundy coloring. In yellow sandstones, there are numerous propelipidaphyphite (rhinoofite) flora. The power of sandstones is about 1.5 m. The abovely sorted gravel-conglomerates with sandy cement and gravel-pebble-beclosed wreckage of underlying rocks, with a capacity of at least 2 m. A few years ago, this exposure was destroyed during construction work.

Fingerprints rhinofitis

In general, at the bottom of the incision of Nizhnekarymovskaya, sandstones are predomined by sandstones with a yellow, pinkish gray and red-color color, with parallel or directed slagness. At various levels, they contain assesses and lenses of polyminamic gravites and conglomerates or the convergence of green or red-colored aurolithic and argillite. The power of the lower part of the cut submissions more than 100 m.

Above the cut occurs a thumbnail package. Its incision is represented by the overlaping of finely, medium and large-ground (sometimes with an admixture of the wedllow material) of conglomerates. Occasionally there are bauddes and lenses of gravites and sandstones. Conglomerates polyminic Pebbles are composed with a variety of magmatic and sedimentary rocks: shenites, granite porphyres, diorites, gabbroids, effusions of various composition, limestone, etc. The total capacity of Nizhnekaryum submissions (Assafyevskaya Sweet) is at least 400 m.

You can observe the deposits of Nizhnekarymovskaya subheads in numerous small outputs along the foot of the Torgashinsky Range (in the area of \u200b\u200bTorgashino and Vodkov villages).

Above the incision of Karymovskaya subimbates increases substantially by volcanogenic formations, the cuts of which are exposed in the Berezovka River Bores in the Petryshino station. Here are illegally versed, often the alkalius of the seduced and lenzide bodies, mainly the lava formations of a moderate-alkaline composition, in the range from basaltoids of increased climbing to the trachiriodocytes. The subordinate role is played by the conjunction of red-color sandstones and polyimict conglomerates. The total power of the volcanogenic part of the cut in the vicinity of Petryshino station is at least 100 m.

Artificial exposure of Karymovskaya suite. Mountain is sharp from Petryshino platform
Chips of tonsidiamental basalts in red-colored sandstones and conglomerates

Basalt Mindobymenny

Basalt Mindobymenny

Agglomerate from volcanic bombs

Volcanic bomb

More precisely, the age of terrigenous sediments of Karymovskaya suite is defined as Nizhnevonsky on numerous propteriduous residues (renyophyte) flora. The largest is Torgashinsky location, open in the 1930s. And in detail the largest connoisseur of propteriduous flora A. R. Ananyev, widely known in world literature, which is located in the former career "Sweat Merities". There defined Protohyeniajanovii, Prototaxitesforfarensis (KidstonetLang.), MinusiaantigmaTschirk., ZosterophyllummyretonianumPenh., DistichophytummucronatumMagdefrau, Sawdoniaornate (Daws) Hueber, Margophytongoldshmidtii (Halle) Zakh., PectinophytonbipectinatumAnan., PtotobarinophytonobrutscheviiAnan., Ienisseiphytonrudnevae (Peresv.) Anan., Drepanophycus spinaeformis Goepp., Platyphyllum Fasciculatum Anan., Enigmophyton Hoegii Anan., Broeggeria Laxa Anan., RELLINIIA THOMSONII (DAWS.) LECLERC ET BON., HUGMILLERIA LATA HUGMILLERIA LATA (?) STORMER (?). Unfortunately, currently this location is not available for observation, as it was covered in the construction of the dam of the ashistant of the Krasnoyarsk CHP-2, despite the fact that it was listed by a protected monument of nature.

Middle Department (D2)

Pavlovskaya retinue (D2PV) with blurred and angular disagreement lies on the rocks of the Karymovskaya Sweet of Lower Devon. Its deposits are stretched by a strip from the northwestern outskirts of the city of Krasnoyarsk, through the central part of the city to its southeast suburbs (area of \u200b\u200bZykovo station) and further. The postposition of Pavlovsk Sweets along the river Kacha is best naked, especially according to the southern slope of the Pokrovskaya Mountain. It is on cliffs, folded red-colored rocks of this suite ("Red Yamra"), the city of Krasnoyarsk received his name.

r. Kacha

"Red Yar" for quality

Drozhinskaya Natka.

At the top of the Drozhinsk

Pavlovskaya retinue is composed of exclusively by sedimentary rocks of the terrigenous, partly of carbonate composition: sandstones, aleuroliths, grave, conglomerates, marlamles and limestones. According to lithological features (to the largest maintenance of carbonate rocks), it is divided into 3 subheads.

Nizhnepavlovskaya subhead (D2Pv1). The deployment of the lower subimbates are highlighted most of the cut of the suite and are represented by sandstones, conglomerates, aleurolites, mergeles with rare limestone lenses. These breeds are exposed at Durier villages, Lukino, Kuznetsovo and in the eastern part of Krasnoyarsk. In its foundation there is a pack of sandstones, with an admixture of sandy-gravel material and small pebbles of volcanic rocks. There are containing bails and lenses of carbonates. Above the powerful (up to 70 m) bundle of conglomerates and sandstones with rare germinal mergel assesses.

The middle part of the bottom subimbers is composed of frequently overlaid markels and sandstones. Mergeli greenish-pink and pinkish gray fine grained, red and pinkish gray sandy, sometimes red-burgundy strong with small scales of mica. Sandstones are greenish-pink fine-grained with the bauddes of gravel sandstones and burgundy-red dense weakly mergels.

Above the cut again predominate sand-conglomerate sediments with low-power assault and mergel lenses. Small weakly catalyst pebbles are represented by silicon rocks, shenites and effusions of the main composition.

The total capacity of Nizhnepavlovskaya subimbers 350 - 400 m.

The midpadavlovsk system (D2Pv2) is a marking thickness and traced at a significant part of the Rybinsk depression. The lower boundary was carried out by the appearance of a sewer of limestone layers containing the scan of red chalcedone. It is composed mainly by red-brown, less often in greenish-gray merryls, among which there are bastards and lenses of limestone, sandstones and individual lenses of conglomerates. This subhead is the most saturated carbonate rocks. Promotions of limestones that occur among the less resistant to weathering are formulated, sometimes stepped and cooler form of relief.

Marking horizon of limestone at the village of Kuznetsovo

Marketing horizon of chip limestone (calcarenites) on the Pokrovskaya Mountain

3 km south-east of the village of Durovno, on the left bank of the Kachi River, among the yellow sandstones, there is a low-power (0.3 m) layer of fine sandstone with plants. Dawsoniiandrewsetal. and etc.

The power of the Mid-Pavlovsk road subimbed about 120 m.

Verkhnepavlovsk system (D2Pv3) on a lithological composition is close to Nizhnepavlovskaya and differs from it by a few more limestone concerns and the presence of argillite. The incision of the subimbers with a precisely acetrate open the trenches traveled in the north-northeast direction from the chapel (the tops of the guard mountain) for about 650 m. Mergeli predominates in the composition of deposits, among which in the form of low-power (from 0.2 to 2 m) lenses and interlayers Sandlings and small conglomerates lie. The power of the deposits of the top back to 120 m.

The age of Pavlovsk suite is defined as the Middle Eastonian on the basis of the finds of Flora Flora near the village of Durovno.

Upper Devon (D3)

Kungus Sweet (D3KN) enjoys in the neighborhood of the city of Krasnoyarsk wide distribution. Its deposits are stretched southeast of the village. Solontsy through the territory of the Soviet district of the city to the village of Lopatino. The rocks of the Kungus Sweet in general is unstable to weathering and are poorly naked. Their exits can be observed in the terrace base on the left bank of the Yenisei below Medical Academy. In addition, the deposits of the suite were opened by numerous wells in the process of engineering and geological research at the beginning of the construction of the microdistrict "Treeting".

Kungus retinue in accordance with Pavlovskaya. The lower limit is carried out conditionally on the change of mergels of the upper part of Pavlovskaya suite with a pack of gravel-sandstone rocks containing the assault of grayish-white sandstones. Above the cut is observed a versatility of brick-red, less frequently, green aleurolites and mergels, often sandy, with sandstone, argillite, grave, limestones.

Pereshadnaya sandstones, Gravelites and Aleurolites
Kungus Sweets at the village of Solonsy

Red-color Alevrolytes and Gravelites at the village of Solonsy

Gravelit

Grave with calcite crystals

The limestone conglomerates are characteristic of Kungus, called "icium" limestones. They consist of flat and rounded limestone and mergel salule size in diameter from 1 to 5 cm. The cement of limestone conglomerates is limestone-clay material.

Buried volitional niche

Buried Ozrag.

Devonian Tajras

The upper part of the sweet is blurred before the accumulation of overlapping deposits of carbon. The power of the suite in the area of \u200b\u200bthe city of Krasnoyarsk is more than 300 m, in the adjacent parts of the Rybinsk depression reaches 600 m.

From the lower horizons, the sweets are collected by flora defined as Pseudoborniacf. Ursinenath., and Archaeopterissp., Archaeopteriscf. Fimbrriaatanath. et al. In greenish gray sandstones from the middle part of the Kungus Sweet, the scales of shell fish were found, defined as BothriolepiscF. Sibiricaobr., In limestone conglomerates, remnants of shell fish were found defined as osteolepidae. All these finds define the belonging of the suite to the top Devon.

Coal system (C)

Lower department (C1)

The Chargin Sweet (C1ČR) lies with a blurring on the underlying sediments of the Upper Devon. They are distributed to the Right Bank of Yenisei in the East outskirts and in the adjacent part of the suburban zone of Krasnoyarsk. The breeds of the lower part of the Chargin Sweet, observed on the right bank of the Berezovsky River near the platform dry and along the road between the village of Voznesenskiy and the village of Lopatino. In the context of the platform, the dry base of the suite is not opened, but a fragment of the lower part of the sweat has a capacity of about 80 m. In the context, sandstones and aleurolites (mostly limestone) are rhythmically alternate, grave and conglomerates, sometimes limestone. The latter often contain a stuff and assessed orange silicon. Characterized by sharp boundaries between lithological differences; Frequency wavy surfaces of the erosion. The power of the layer of change is noted, there are cases of sequencing them by strike. Widespread directional slags. Among limestones are distributed debris differences - calcarenites. In the lower part of the cut, red-color coloring are dominated, and greens become more increasingly distribution. Also up the incision increases the fraction of carbonate rocks.

The higher part of the cut of the suite is represented by the transfer of greenish markels, brick-red aleurolites and limestone conglomerates. In the upper part, limestone conglomerates and limestones are dominated with the inclusions of Halcedon. Among them are the convergence of limestone sandstones, aleurolites and argillites. Coloring colorful with illegal alternation of greenish and red and red color differences. It is often observed a replacement for stretching limestone conglomerates with greenish-gray sandstones with a large number of wreckage of quartz, chalcedone and lopery wreckage of Mergel, as well as fine-grained sandstones - aleuroliths.

Power suite more than 450 m.

In the fall of green-color aleurolites from the top of the cut of the suite, along the road Voznesenskoye - Lopatino, numerous plant prints were found: AsterocalamitessCrobiKulatossch. and HelenielTheodorizal., Determining the age of deposits as the Early Industrial (Tournai).

Krasnogorievskaya Sweet (C1KR) is developed in the vicinity of Krasnoyarsk a narrow sub-loss traced from the village of Berezovka to the village of Voznesenskoe. It increases increasing incision of the underlying Chargan Sweet and with a deep blurred and angular disagreement overlapped by the deposits of the lower Yura, and therefore its incision in the area is incomplete.

Motley Moveless Aleurolites, Sandstones, Gravelites
Krasnogoryevskaya Sweet at the village of Voznesenka

Layer of green aleurolites and argillite

The retinue is represented by translating pinkish-yellow, yellowish-green sandstones with subordinate subsidies of green aleurolites and argillite. There are interlayers of ashes of acidic composition, tuffs, tufoots. The most representative fragment of the lower part of the Sweet is opened by the roadside career in the southeastern outskirts of the village of Voznesenskoe, along the road to the village of Lopatino. Here are naked, yellowish often mica small and medium heated sandstones of quartz-field-sifted composition. Sandstones are often limestically, areas are enriched with calcium phosphate. They are often present there are lopery fragments of bluish-green argillites and well-preserved residues of a large lepidodendronous flora. Above the cut, they are replaced by greenish coarse-grained quartz-field-satellite sandstones. The upper part of the suite is composed of finely and medium-trimmed greenish-gray and greenish-yellow sandstones with baking-green argillite assesses. Power of Krasnogorievsk Sweets more than 300 m.

Fingerprint lepidodendron

Imprint lepidodendronous flora

According to the remnants of the lepidododendron flora PorodendronCristatumchachl., PorodendronPlicatumchachl., Knorriasp. and others. Age Sweet is defined as the early manner.

Mesozoic Erathema (MZ)

Jurassic System (j)

Jurassic sediments are distributed in the territory of the northern and eastern parts of the city of Krasnoyarsk and in the surrounding surroundings. The precipitation of this level is represented by a continental coal-like formation, the most important feature of which is its rhythmic structure. Elementary sedimentation cycles are usually sandstiles, less often by grave or conglomerates. Up the cut of the sandstones is replaced by aleuroliths and argillites. And finally, these cycles are often crowned with layers and bastard of brown coal. All Jurassic deposits of the city of Krasnoyarsk belong to eastern zone Chulymo-Yenisei depression. The Jurassic sediments of the territory of the city and its nearest surroundings belong to the two departments of this system - lower and medium. The Lower Yura is represented by Makarovskaya and Ilaska Sweets, the average - Itatian retinue, and the overlay deposits are already developed on a significant distance from the city.

In the Jurassic sediments of the district of Krasnoyarsk, a facial variability is shown. In the direction from the east to the west, the number of elementary cycles and, accordingly, usually crowded coal reservoirs and the interlayers increase.

Lower department (J1)

Makarovskaya retinue (j1mk). The deposits of Makarovskaya suite are common on the right bank of the Yenisei on the eastern outskirts of the city of Krasnoyarsk. They disagree on the rocks of the Paleozoic and are represented by conglomerates, sandstones, aleuroliths, argillites with several low-power plastics of brown coal. The most complete incision of the suite is observed in the coastal exposures on the right bank of the Yenisei River, below the northern end of the island of Tatyshev.

At the base, the suite lie yellowish-gray weak-cemented conglomerates with poorly sorted, but well-retired pebbles of siliceous and volcanic rocks, less often granites, quartzovoid sandstones, metamorphic shale, gneisses. The pebbles of kaolinized rocks occurs, which is associated with the processes of transitioning formations formed at the end of the Triassa - the beginning of Yura area of \u200b\u200bthe weatherariness. The power of conglomerates is 30 m, their outputs are also encountered dry dry.

Above the cut conglomerates through a pack of yellow and gray-green medium-grained sandstones with gaps of grouts are gradually replaced by the rhythmic sealing of predominantly serous fine-grained sandstones, aleurolites and argillites with buoy coal swords. In the very upper part of the section, greenish-gray argillites are dominated by the pretties of fine sandstones and three reservoirs of brown coal with a capacity of up to 1 m. The total power of the deposits of Makarovskaya suite in the Krasnoyarsk area is about 100 m, in the western regions of the region, it increases to 200 or more meters.

In the sediments of Makarovskaya Sweets found plants, Elatocladusmanchurica (LokoJame) Labe. Of these, representative sprinkled complexes are highlighted, in which pollen of ginkgy, benetite, coniferous, disputes of fern, characterizing the age of suite in the Sineural and Plinsbakh tiers of the Lower Yura.

Ilan retinue (J1il). Sweet deposits are pulled out by a narrow strip from the eastern outskirts of the city of Krasnoyarsk to the village of Vrhahatovo. Here, the Ilan Sweet lies with a blurry on different horizons of Makarovskaya Sweets and on the underlying paleozoic sediments. It does not contain industrial coal deposits, unlike the underlying and overlapping sediments. There are only low-power (up to 1.6 m) of precipitation of cooler breeds, less often brown coal. The lower border of the peel is carried out along the roof of the carbonaceous rocks, which occur in the upper part of the Makarovskaya Sweet, or on the change of predominantly sand factions of Makarovskaya Sweet to the overrading of the aurolites, argillites and sandstones. It was composed of an Ilan retinue by aleuroliths, sandstones and argillites, with interlayers and lenses of argillites of coarse, less often - brown coals. Characterized gray-green colors tones.

The deposits of Ilaska Sweet are characterized by sprinkled complexes of the Taroic Tarus of the Lower Jura. Its shared power up to 180 m.

Middle Department (J2)

Itatian retinue (J2it). The formation of the Ilanian Sweets is found in the area of \u200b\u200bKrasnoyarsk. Extensive areas on the left bank of the Yenisei, within the microdistricons Green Grove, North, Sunny, in the vicinity of the Kraz and the village of Peschanka. Its basal layers with erosion lay on various horizons of Ilanian suite, and in the edge parts of the chulymo-yenisee, and on more ancient deposits. The rocks of Itatse sweets can be observed in the coastal exposures of the Yenisei below the city of Krasnoyarsk, in the area of \u200b\u200bthe villages of Corkino, Kubekovo, Dwonogovo. It is folded by rhythmically translating sandstones, aleuroliths, argillites, carbonaceous aleuroliths and argillites, with interlayers and lenses of conglomerates and grave, coal layers.

Springs, aleurolites, argillites, carneal aleurolites and argillitis, interlayers and lenses of conglomerates, graveite, coal layers are involved in the onset. Based on the cyclicity of the cutting structure, the switch is dissected for three subheads, each of which begins with the deposits of substantially sandy composition with abandonment and lenses of threatening breeds, and ends predominantly fine-lumpy (alageargillite) rocks with reservoirs and brown coal. Sweet deposits are characterized by representative sporing complexes of Central Yura (Nizhneitatskaya subtitus - Aalen Tier, the Midneitat Site - the Bayos Tier, Verkhneitataya - Batsky Tier).

Verkhneitataya subhead is characterized by a rich complex of flora and fauna. The incoming chain, where organic residues were found, stretches from the village of Kekuzovo 7 km and ends below the village of Dwonogovo. The remnants of gamotors Ginkgo, Bajtra, Phoenicopsis, Czekenowckia, CONIOPTERIS, CLADOPHLEBIS Fernants, Equisetites, and others, etc. are known. insects. The rest of their residues are detected at the top of the section of the Upperitat hubs in several layers, which are maintained by strike at a considerable distance. Very numerous and varied forms are found here - like water (larvae of the pivot, water beetles Temptus, dragonflies, swirls, spring, nettoby), and ground (semi-rigid, cockroaches, beetles).

The capacity of the Nizhneitat system to 150 m, the Midnesian - up to 250 m, Verkhneitataya - up to 200 m. The total power of the Itatian suite is up to 600 m.

Cenozoic Erathema (KZ)

Quaternary system (Q)

The sediments of the Quaternary system enjoy in the vicinity of Krasnoyarsk with almost widespread development. It is widely represented by natural deposits of various genetic types: alluvia, prolyuvius, eluveli, collumba, delueli, dessertations, deflucts, limony, lindsublines, defaults, as well as technogenic education. Their age fluctuates in the range from Eopleistocene to Holocene (modern). The basis for the age-related dismemberment of quaternary deposits of the area is the chronological sequence of formation of the terrace complex of the Yenisei. Therefore, alluvial sediments are most reliably disseminated, the levels of different-age terraces. The age of terrace alluvia is defined by sprinkled complexes, bone residues of mammals, and for the youngest - and in Paleolithic tools. The deposits of other genetic types are compared with different levels of the terrace complex on geomorphological features. Those that are superimposed on the surfaces of the terraces or are confined to embedded form embedded in them are treated as younger.

In total, there are nine terraces of various plaster levels in the area of \u200b\u200bKrasnoyarsk in the Yenisei Valley and, respectively, age. All of them, with the exception of the first, have their names. The first terrace is up to 9 m above the modern cutout of the water, the second (loan) - up to 15 m, the third (Krasnoyarsk) - up to 25 m, the fourth (Berezovskaya) - up to 35 m, the fifth (camp) - up to 60 m, sixth (Dogsky ) - up to 80 m, the seventh (Torgashinskaya) - up to 110 m, the eighth (thin-talk) - up to 140 m, the ninth (Badalykskaya) - up to 220 m. The valleys of the main tributaries of Yenisei (Bazai rivers, kachi, guard, etc.) are weakly terrible . Only in some sections of their flow there are single remains of the terraces, and the full terrace complex, similar to the Yenisei, is not developed anywhere. On extensive water-seated spaces, where there is no possibility of geomorphological comparison with a terrace complex, quaternary deposits of all genetic types are considered as belonging to the quarterly unexplored system.

The description of quaternary deposits is provided by genetic types.

Alluvial deposits were formed throughout the eoplestocene to the present. Alluviy IX (Badalykskaya) and VIII (thin-talk) terrace belong to Eopleistocene. In the area of \u200b\u200bKrasnoyarsk, the 9th terrace was preserved on the left side of the Yenisei Valley at the village of Badalyk, on the right - on the mountain, a pine cape, where the lower part of the allyuvia is opened by a quarry. Here, horizontal sand horizontal sands, pebbles of polyminic composition, saccinated with cochings of the polyminal, saccinous sand, are blurred here on the queen-colored clay of weathered cortex. The upper part of the stratum at the village of Badalyk consists of a pebble, which includes a lot of weathered rocks, saccinated by the roened kaolinized sand, and a sulfing of gray-brown with sand lenses (Berbon et al., 2001). The total capacity of up to 9 m. VIII The above-handing terrace is most pronounced on the left bank, in the state of state university and biathlon shooting at the western outskirts of the city. Here, in the logs of logs, you can observe the outputs of brown lime sacks that meet the upper part of the cut. The lower parts of the section of Alluvia VIII were observed by E.I. Berzon et al. (2001) at the top of the Pokrovka microdistrict, which are represented by oily-brown sand with peaks of siliceous rocks, sandstone, granite, as well as sandstone and sublinks. The total capacity of alluvia VIII terrace to 25 m.

The lower link and the lowest part of the middle links of Nelevocene include alluvius VII (Torgashinskaya) terrace, 80-110 m. This terrace is one of the most pronounced Yenisei terraces in the Krasnoyarsk area. On its surface on the left bank, Akademgorodok and the student town are located, and on the right bank, it is stretched along a significant part of the northern slope of the Torgashinsky ridge from the Bazaja River to the village of Torgashino (Cemzavod). The tops of the terrace of the terrace are well naked in the roads from the pond in the area of \u200b\u200bthe subsidiary economy, the sanatorium "Yenisei", west of Akademgorodok. There are dense loams, grayish-brown color, with a thin parallel lamination (with unbearable sand-gray interleavers), limestone; Movement with sand and overlapping them. The lower parts of the cut are not naked, but on the sides of the logs embedded in the terrace, there is a numerous well-rolled fine pebble of a variety of composition, obviously washed out of the terrace aluminum. The total power of Torgashinsky alluvia is up to 40 m. Age is determined by the finds of the fauna of the mammoth, woolly rhino, bison, mollusks, data of dispute and pollen and paleomagnetic analyzes directly in the city of Krasnoyarsk (rattling log).

Allyvial sediments of the VI and V terrace of the Yenisei include the middle link of Nelependocene. VI (Dogian) terrace is best developed on the left bank of the Yenisei, the western outskirts of Krasnoyarsk have. Here it is stretched from the area of \u200b\u200bthe mouth of the Karaul River, through the assistant part of the dog's river at the village of Successful to the Log of Cave from the western outskirts of Akademgorodok. The lower parts of the cut of the Dog's Alluvia are opened with a small quarry located on the surface of the terrace opposite the governor's residence "Pine". Here are the mostly small-grinding pebbles, as part of which volcanic and siliceous rocks are presented, residential quartz; There are poorly returned fragments of vendors of sandstones, aligning terraces base. The overlying part of the Alluvia is opened by shurts and is composed of light loams and sacheses, often limestically. The total power of the allyuvia Vi of the terraces is up to 10 m. V terrace (camp) is widely represented in the left bank, from the mouth of Kachi to the aluminum plant. To the depth of 1.5-2 m, the terrace is composed of forest loads. Below are leather, finely, medium sandy sands are rare pebbles. At the base, there are pebbles. The power of allyuvia IV terrace reaches 35 m. The lower part of the alluvial thickness is dated by the second medium-recycling interglamp on the basis of the findings of the remnants of the mammoth fauna and the spray complex (Berbon et al., 2001)

Allyuviy Upper Neleople's Alloy presented deposits of IV (Berezovskaya), III (Krasnoyarsk) and II (Lade) terraces of Yenisei. The highest development is used by the III terrace, which is located the city center of Krasnoyarsk. The terrace is accumulated, composed of pebbles with sand lenses. In places, the pebble is covered by Lesisoid Suglinkami and Wagrams of the outstanding sands. The capacity of precipitation is 20 meters. The bottoms of alluvia with the remains of woolly rhino and mammoth, according to the composition of the sprinkle complex and the features of precipitation are responsible to the glacial. The tops of the cut contain the South Taiga SPK with an admixture of a glitstic, responding internally. The bottom cultural layer of the Upper Paleolithic parking lot "Afontov Mount II" at the railway bridge is timed to the covering formations of the terrace. From it received a radiocarbon dating of 20900 ± 300 years (Berbon et al., 2001). The II terrace is widespread on the right bank. The whole terrain along the Avenue "Krasnoyarsk Worker" is confined to its surface. Alluvius terrace is represented by peccles, layered with sandy clay, gray sublinks. Power 14 - 20 m.

Border Late Pleisoistocene-Holocene Age have the deployment of the first episode terrace. They are presented with sands with the assesses of clays and clans, sands, peccles. Power of deposits up to 9 m.

Modern Alluvius is represented by the channels and floodplain sediments of the Yenisei and its tributaries - Bazaoi, Berezovka, Kachi, Kasual, etc. Composition of its most part pebble or sandy, with lenses of precipitation alaith-clay composition. In areas with a rapid flow, there are currency sediments observed, in particular, in the assistive part of the Caltat stream and some segments of p. Basai.

Oilly-alluvial deposits compared with the level of VIII of the terrace of Yenisei (Eopleestocene), lay the plain on the left bank. Kacha, being the facies of the periglacial pool in the valley of the river. Yenisei. They are represented by brown clay, gray, greenish-gray with sludge, at the base of which are observed with sandy, clay sands with gravel. Power 5-15 m (Berbon et al., 2001).

Large deposits (Limnia) accumulate in modern ponds, in a large number of Krasnoyarsk arranged in the suburban zone. They are represented by sapropel ally with fine horizontal lamination and admixture of sandy material. You can watch them in arid seasons at a low level of water in the ponds. Age Holocene.

Swamp deposits (lumpy) are developed locally on highly moistened areas in the floodplains of streams and small rivers. Their observation is possible only when driving small shurts in the late autumn, when the swamps begin to freeze. Premises are presented with alcohologenic sediments of dark gray color, with a large amount of indecomposed vegetable material. The age of marshcene sediments installed in the vicinity of Krasnoyarsk.

Elvius is the products of destruction of indigenous rocks that occur in the place of education. It covers the sprinkle and watersheds. It is presented by dressing and rubble, the composition of which corresponds to underlying indigenous rocks. Slit usually directly under the floor layer. Power - to the first tens of centimeters. Age is determined in the range from the eopleistocene and even lategenegular to modern.

Prolutions is the deposit of time aqueous streams. It is based on numerous removal cones imposed in the mouths of dry logs on the surface of various terraces and modern will understand, and also often widespread the bottoms of dry logs. It is complicated by unsorted sublinks and suica usually brown, with rubble, sometimes with boulders. The chip material is always represented by rocks developed above on the slope. In areas where the blurred substrate is represented by carbonate rocks, lime deposits, have a white color. In some cases, when the alluvia is a high terrace, a well-retaent pebble is present in the composition of the Proluvia. In the cones of the removal, the coarse illegal lamination is manifested, expressed in alternating in the power of the layers and lenses, differing in the proportion of the threshold material in the composition. In the context of some taking cones there are horizons of buried soils. This indicates interruptions in the accumulation of the Proluvia, during which the formation of soil cover began, after which the debris of the debris material was resumed by temporary streams. Numerous removal cones can be observed along the entire automotive road from the village. Country on the left bank Yenisei (near Akademgorodsky) before the village. Successful (where they are often opened by roadside recesses), as well as along the foot of the Torgashinsky ridge on the right bank of the Bazai River. The power of the provision in the removal cones can reach 10 or more meters.

The age of prolution and all the inclined deposits described below are determined on each section of geomorphologically according to the ratios with terrace surfaces. In general, their accumulation proceeded in the range from Eopplayian to Golochene and continues at present.

Collumba - Obivanny and Outlinary sediments - represented by rubble and boulders. It is developed mainly on steep and dry slopes of the southern exposition, where physical weathering processes and their products cannot be kept too rare floral cover. Collible deposits by a low-power cover cover the slopes and form, often together with the proliable cones of the removal, the loops along their foot, with a power up to several meters. These sediments get the greatest development there, where the slopes are complicated by unstable, strongly fascinated indigenous rocks. It can be observed across the high terrace of Yenisei along the road from the Academgorodok on the village. Successful, where the base is almost entirely complicated by sandstones and the aleurolites of tubing suite, while weathered easily scattering in Sheblen.

Desserts - unsorted crushes material, developed on the slopes of the average steepness (most of the southern exposure), and slowly sliding under the action of temperature fluctuations. Typical dessert education can be observed on the housing of the mountain Nikolaev Nikolaev Nikola, in the roadside excavation, where they overlap the root yields of shenit-porphyres and microgabbro and themselves are folded by their destruction products. Power dessert up to 1 - 2 m.

Delueli - product washed with rain and thawed waters. It is represented in the vicinity of Krasnoyarsk with thin substantially clay sediments found in the lower parts of the gentle slopes. IN modern conditions The formation of dellowing practically does not occur, since the slopes are almost universally covered with a sufficiently dense layer of the rod, which protects it from erosion. The main volume of deluel was formed in cold epochs in the forwarding atmosphere, with a buccated vegetable cover. Education processes of dellowing and desserts are often manifested on the same sites of the slopes, but at different times and probably with different climates, due to changes in the nature of vegetation

Defluccia is another type of slope deposits, the formation of which is the result of a plastic foaming of a strongly moistened substantially clay soils. Composition - Suglinka, often with rubble of underlying rocks. It is formed mainly on the slopes of the northern exposition, as well as on the shaded and wet slopes deeply embedded logs. Here, deflutation sediments are also often alternate with deluvial, accumulated in colder epochs at cutting vegetable cover. In the modern setting, the deflutation processes are most activated after the melting of the snow, when the topmost, highly moistened by the waters, the soil layer slowly slides on a deeper not flawed and therefore imbusizing underground drains mavel Water. Such phenomena can often be observed in early spring in roadside excavations that cut the moistened slopes.

Deleapps - deposits of landslide origin - developed locally on steep slopes, folded by loose unstable soils, subject to their feeding of groundwater. It is the jams of whole formations or loose sediment blocks, without disturbing the integrity of the slope-fitting slope. Sometimes landslide processes are activated as a result of technogenic intervention, leading to an increase in the level of groundwater (construction of dams, dams).

Landslide on the western slope of the Pokrovskaya Mountain

Technogenic deposits within Krasnoyarsk and its surroundings are very diverse. Among them are shut-down and crushed-lumpy deposits of career dumps, varied by granulometry of the formation of dams and embankments, bottom sediments of industrial septicles. The latter, in particular, includes technogenic ils of the height of the CHP-2, arranged in the abandoned career of the cemyzavod.

The photo is visible to the Tartashinsky ridge, Capera CHP-2 and Cemesavoda.

View from the Pokrovskaya Mountain

They are thin sediments ash-gray with thin parallel lamination and elevated heavy metal contents. As the sump is filling, they are extracted and exported for burial in the nearby quarry "Blooming Log". A special kind of technogenic deposits is the accumulations of household, construction and industrial garbage on numerous landfills - both legal and unauthorized. Age Holocene.

5.2. Intrusive magmatism

Magmatic education in the vicinity of the city of Krasnoyarsk is represented by a variety of petrographic composition by rocks formed in the age range from the late Rifey to early Devon.

Late Frifs and Protrusia

Akhepsky complex of alpinotype hyperbasites (SRF3A). The complexes are sharply dominated by serpentines, often intensively matched. In the Krasnoyarsk zone of his body, two closest "belts" are formed: Akshepsky and Sliznevsky. Previously, they united G.V. Pinus in the "Krasnoyarsk belt". The "Slyznenevskaya belt" is located in the zone of large deep-to-10 km breakdown with a width of up to 10 km (from the mouth of the Bazai River to the mouth of the mysterious river) and a length of more than 35 km. The ultrasound of the complex is naked in the rivers of the rivers of large and small mucillars, the rivers of a dog, on the left bank of the River Yenisei, the above village is successful, as well as in the lower flow of the Bazai River (blue slide and mountain tower).

Rock exposure of serpentines on the left bank of the River Yenisei. Sliznenev Protrusion

Serpentinite with sliding mirror (1 side)

Serpentinite with sliding mirrors (2 side)

Small bodies of hyperbases are brought together with each other, forming chains consisting of two, less often - three-four lenzide bodies of linear-elongated protrusions, with a capacity of 100 - 200 m. The largest of them are Baza - Said (5 km2) and Sliznevsky "arrays" (about 12 km2). All protrusions are stacked by matched, less frequently massive, serpentinites, green and dark green (to black) color, sometimes containing the few Relicates of Olivine (partially substituted by iddingsitis) and Rhombic Pyroxen (Enstatat). Among the accessor minerals are dominated by magnetite and chrome. In relative large bodies Hyperbasites are observed with various ultrasound and main rocks, to one degree or another subjected to serpeninization processes. Thus, on the left bank of the Yenisei, below the mouth of the river Kutenka and the dog's river there are intensively catatlazed greenish-black pyroxyenites of the panidomorphic structure, consisting of Avgita, Hyperstand (about 15%), strongly serucyted plagioclase (up to 10%), Ilmenite and secondary: chlorite , renith, antigorirt, biotitis, brownish horn and carbonates. On the right bank of the Yenisei, opposite the Dunchet's Dunkinsky Island, 1 km above the mouth of the Kovkov's river, a dark-green strongly serpentinized Olivine breed with the relics of Dialland, penetrated by the streaks of chrysotile asbestos and carbonates. Serpentinites of the described area occurred due to pyroxenites, peridotite, dunits and other rocks of a close petrographic composition. The complex is not studied enough, there are no reliable data on the rationale for age. The late fiction age is adopted conditionally.

Bakhtinsky volcanic complex. Subvocanications (NRF3BH) are represented by sizlium by sizes up to 3.5x0.8 km and dikes up to 0.2x0.02 km, intensely green-changing finely and medium-trimmed microgabbro with a gabboophyte structure. CONTACTS OF DEKHES A sharp, swirling, Sillov - consonants with accommodating sediments.

The crushing zone of fine-grained Gabbro Bakhtinsky complex.

Indigenous exits on the right bank of the Bazaja River, in the target of the moss stream

Calcite lived in the crushing area of \u200b\u200bfine-grained gabbro

According to petrochemical and petrographic characteristics, we are identical to the volcanics of the coating facies in the composition of the Bakhtinsky suite and are often the supply channels of these effusives. Late Fifty Age is adopted conditionally.

Medium-Lategoroviki intrusion

Genetically and spatially are associated with the volcanites of the Iramskaya Sweet, the figurative points of the compositions of both volcanic and intrusive rocks form uniform differentiation trends on most petrochemical diagrams, which makes it possible to consider them as members of unified volcano-plutonic associations. The magmatism of the Ordovician stage is characterized by increased alkalinity, with a predominance of Na over to, an increased content of volatile components in the source melts. Comagmaticity of the Association breeds is emphasized by the general geochemical specificity for them - the reduced content of RB and elevated contents of SR, BA, TH, MO and V.

Iramsky volcanic complex. Pole and submulcanic educational part of Iramsky Basalt-Trachyandeze-Trachryolyte Volcanic Complex. Sktoky, etgolites, akmolita, some of the area of \u200b\u200bup to 3 km2 in the field of development of volcanogenic formations of the Iramskaya Sweaters are found.

The headings of the Iramsky volcanic complex are represented by small (diameter up to 200 m) with some kind of messenger on the southern foot of the ridge and on the left bank of the Yenisei river 2.5 km west of the village of successful, as well as on the river arrow smooth and steep kaches. Made with eruptive breccias predominantly basaltometh composition, in which single fragments of pink fools and microsenites are found.

Subvocanic formations are represented by laccolite-shaped intrusions of quartz shenit-porphyres and microsyenites in the area of \u200b\u200bthe ridge, the long mane and stations are minino, as well as numerous dikes of moderately alkaline fine-grained gabbro and microgabbro, trachibasant, trachidolerite, fuchistra. Microsenites, microrenostites, coagmatic rocks of the Iramskaya Sweet. Basalts, funites and trachidelets are often found in the form of a capacity of 0.5 - 0.6 m, traceable on the area of \u200b\u200b500 - 800 m, sometimes more than 1000 m. Usually submulcanic intrusion complex are quite well released in the relief in the form of the grivot, a variety and isometric vertices .

The intrusion of quartz shenit-porphyres (in the area of \u200b\u200bthe first and the second hill) is a laccolite, the roof of which is well cleaned in modern relief. The intrusion has a zonal structure. In its center, quartz weakly burf-like shenites of pink color with fine-grained basic mass are developed, and the peripheral zone of the intrusual body is composed of microsensites and shenita porphyres with a fine-grained majority. According to petrochemical characteristics close to the corresponding effusions of the Iramskaya Sweet.

Geological map of the Range "Long Mane" (Perfilova, Makhlayev, 2010):

1 - quaternary education; 2 - IMIR-volcanic complex, subvulcanic education: 2 A - Shenit-porphira, 2 b - fine-grained weaklyorfire-shaped syenites; 3 - microgabbro; 4 - EUROPETIVE BRACKIES (PERSONAL EDUCATIONS); IMIR SWITE: 5 - Foils (sixth bundle); 6 - basalt buildings and melkoporphic (fifth bundle); 7 - Freshites (fourth pack); 8 - foolet tuffs (third bundle); 9 - basalt buildings and melkoporphic (second tutu); 10 - Basalts Large Prapping (first pack); 11 - UNNWORD SWITE - Limestone and Dolomites; 12 - Tubil Sweet, Upperbilskaya Site - Limestone Sandy and clay bituminous; 13 - Tubil Sweet, Labylovenskaya Sliced \u200b\u200b- Sands, Alevurolites Rhythmichloin, limestone; 14 - Akhepsky complex of alpinotype hyperbastes: serpentines, peridotites, pyroxenites; 15 A - geological boundaries, 15 b - facial boundaries, 15 V - elements of the occurrence; 16 - 18 - discontinuous disorders: 16 - reliable; 17 - alleged; 18 - blocked by quaternary sediments

Senit Porphira. Nikolaev Nikola

Shenit Porphyr with dendrites of manganese hydroxide

Shenit-Porphyr with Squitz Square and Dendrites of Manganese Hydroxide

The age of subvulcanic intrusions (district of Divnogorsk and Art. Minino), determined by U-PB by the method, was 447 ± 10 million years.

Stolpovsky Senit Gosienite complex (XO3ST) was first highlighted by Yu.A. Kuznetsov in 1932. In the future, this association is more often described in the literature as the Shumihinsky complex. But since the latter name was used in the region in relation to several associations of intrusive rocks of various composition and age, then in the development of the latest serial legends for Gosgeagart, it was decided to exclude homonymy and taking into account the priority, return to the title, under which the complex was described initially.

Complex two-phase. The first, main, phase - shenietites, quartz shenites and grazienits, subordinate importance have hybrid endocontact monzonites and monkeidioretions. The second phase is small rods and dyes of moderately alkaline granites, leukogrants, grainienitis, quartz syenitis, their porphyry differences and aplites. The structures of fine and medium-trimmed, often porphyrene. Microstructure hypidomorphscency, micrographic sections. The composition of the Senitites: Anorclase - 75 - 80%, oligoclases (AN9-12) - 0 - 10%, quartz - 5 - 10%. In grazenites and moderately alkaline granites, the content of quartz increases to 15 - 30%. Dark color minerals - biotitis (usually highly decomposed), green egirine-agite and augit, horn cheating. Accessor minerals: magnetite, apatite, zircon, rutile, sfen. It is characterized by an increased alkalinity of potassium-sodium, less often sodium type, high concentrations of ref area, th - up to 30 g / t.

Petrootype of the complex is the column array. In a modern erosion cut, it is an oval body in terms of form, an area of \u200b\u200babout 40 km2. Previously, he was considered the subvertictory rod. But the analysis of the petrostructural zonality of the intrusion, we fulfilled the analysis allows it to be considered as a laccolite, hollowly immersed to the northeast, under the Valley of the Bazai River, which is confirmed by the latest geophysical data. In the composition of the intrusion, the formations of two phases of crystallization are distinguished. Almost the entire volume belongs to the main phase, composed of relatively coarse breeds, the composition of which smoothly varies in the range of syenites and quartz shenites to grazenites. The phase of crystallization of the residual melt is represented by low-power (the first centimeters, rarely up to 10 - 15 cm) by the veins of quartz microsenate - moderately alkaline leukogrants. The body folded by the rocks of the main phase has a zonal structure. Large, the inner part of the intrusion is composed of biotite-corrosion-rogue quartz shenites, porphyrene, with a medium-hearted (dimension of up to 5 mm) by the bulk. The apical zone, the rocks of which in a modern erosion slice are observed in the highest part of the watershed, are complex, composed by grazenites, characterized by a smaller dimension of the grain mass (1 - 3 mm). Dark color minerals are represented by green augite and horny decendment, less often unfolded biotitis. Magnetite, apatite, zircon, sfen and rutral occurred from accessor minerals. Sometimes fluorite and sulphides are noted (pyrite, chalcopyrite and molybdenite). The edge zone, timed to the side contacts of the array, is mostly different from the inner mineral composition. But in some sections, it marks the grain of alkaline dark flowers, replacing the primary horny decendment. This, apparently, is associated with the processes of endocontact metasomatosis at the boundaries of the intrusion with limestone rocks, which is characterized by the metasomatic removal of silica, as a result of which the total cloth increases.

Exokontact changes of the accommodating rocks manifested themselves in their oroging, argillization, marble, berezitization, feeding, sometimes facaticization at a significant (up to 1.5 km) distance.

The breed of the Pillars Shenit-Granosienite complex belongs to the moderately alkaline suburior of the potassium-sodium series (with the predominance of Na).

The Late Kordovik age of the pillars complex is defined both by the breakthrough of the Komagmatic Effusion of the Iramskaya Sweet and on the basis of the available radioisotope dates: for the column massif - U-PB 449 ± 3 and 451 million years, K-AR 469 million years (ruble, etc., 1995).

In the Stolbovoi massif, the manifestations of fluorite and molybdenite are established. Shenites of the Stolpian intrusion (Mokhovskoye deposit) are widely used as a facing stone for the external and interior decoration of buildings in the city of Krasnoyarsk, the manufacture of monuments, road borders, stairs.

Shenites of the column complex. Mokhovskoye deposit

Rannedevon intrusion

Rannedevon intrusion is very diverse in composition and not fully studied. Daishes of a variety of composition - from rollys and rhyolitis grazenitis and rhyoliths are widely distributed among the deposits of the lower and medium-sized Paleozoic.

Chernosopekkin complex (D1ČR). Includes the rocks of the Petrohythip Mountain Mountain Black Nights and numerous dikes of trachidolerite and rover among the formations of the Karamov Sweets of the Early Devon. Mountain Black Sotka is perfectly visible from many areas of Krasnoyarsk, being one of the highest peaks in the vicinity of Krasnoyarsk. The absolute height of the mountain is 691 m. It is 8 km south-east of Krasnoyarsk city in Berezovsky administrative district, in the field of the articulation of the North-Western tip of Eastern Sayan with Rybinsk Vpadina

For the first time, an array of mountain black hill is described by Yu.A. Kuznetsov in 1932. He highlighted the genetic series of the methods of its breeds from the trachidolerite to Tinguites, considering their differentiation of a single magmatic focus and identifying them with those developed in the Kuzbass area, whose age is considered permot carbon. The same point of view was adhered to S.I. Makarov (1968). Rannedyevonian age of intrusion (parnachev et al., 2002) was established later.

The blackstall is a substantial intrusion well swept in the relief. In shape it is a rod with a diameter of 1.2 - 1.5 km, having an annular structure. Its central part is composed of alkaline olivine cases and easexites, and the periphery - tinguitis; Moreover, the latter perform the annular spill resulting from the formation of the trouting intrusion. This is evidenced by the results of observation of the fractured tectonics, the presence of alkaline shenit-porphyirov in case and involuntary changes in the latter.

Kuruma on the slope of the mountain Black

Stow of alkaline cases and easexites are tilted to the north, confirming what is the orientation of the plagioclase in the porphic differences of these breeds. This also says the asymmetric location of alkaline cases and easesites relative to the top of the Black Nat's mountain. If in the south, their distribution is limited to a horizontal conducted in 680 m above sea level, then in the north - horizontal, conducted in 550 m. Nethelinic shenits that occur among the gravel sandstones in Tubil's sweatsets, are known only in one exit - 3.5 km west of Mountains black hill.

The structures of alkaline cases and easexites are porphyrene fine, fine-and medium-trimmed. The main mass microstructure is a gabbro-official. Textures are massive, and in the edge parts of the intrusion - fiber-like, subathoral contacts. The composition of alkaline functions: Plagioclase (Andesin-Labrador) - 58 - 66%; Pyroxen - 11 - 15%; olivine (htontolite f \u003d 0.6 - 0.66) - 4 - 10%; Analcim - 8 - 13%, biotit (red-brown, f \u003d 0.4 - 0.5) - 1 - 4%; Sometimes in interstics there are separate grains of micropertitis (anorertoklas).

The color of Tinguitis is greenish-gray, reddish-brown, pinkish-gray, is characteristic of a tile separately. The structure of the porphyrene, enclosures are represented by long-crystal crystals of albit oligoclase and nephower. Microstructure hypidomorphsorous and upcoming (eyeball), due to the formation of a "protective shirt" around nefeline grains made of small needle crystals of Egina and Arpvedzonite.

Mineral composition of alkaline shenit-porphyirov 2 phases: Porphy and 8 mm porphyry (up to 30%) are presented with tablet phenocrystals K-Na field spat, less often - dark green egin-avgita (3-4 mm) and isometric discharge of nebelina ( 2 - 3 mm). The bulk consists of arcuate subparallel microliths of intensely pelitized and limonitized alkaline fieldspap, between which the small xenomorphic grains of egin-avgita are "clamping". Plots are composed by the aggregate of fresh leastoid albite. Nefteline-containing and fagpatoo-containing shenit-porphyry: Albit, Kalischpat, Sprouustensified nefeline (or analtsim) - up to 10 - 15%, Eginrian and Arphvedazonite - up to 10 - 15%, zeolites. Often, nefeline grains are booked by prismatic grains of alkaline amphibole and needle-tunic-fibrous aggregates of egirin. Accessor minerals: Titanoagnetitis, fluoropatite, pyrite, pyrrhotite. Sometimes in the rocks of the array observed streaks of fluorite.

Nethelin-field-sighted rocks can be promising as decorative facing material. The age of the Mountain Mountain Copka is Rannedevon, which is confirmed as its committees of the trachidoleritis of the Karymovskaya Sweets of the Early Devon, and the definitions of radioisotope-age rocks AR-AR method - 402 - 406 million years.

The dikes of the main composition (case, trachidolerites), also attributable to the Chernoshopkinsky company, apparently, are derivatives of the Rannedevon magmatism of increased alkalinity, which manifested within the Rybinsk, and the Commasts of Effusion Karymovskaya Sweet.

These dikes are predominantly developed in the southeastern part of the square. Moreover, the dikes of the trachidoleritis are often found directly among the formations of Karymovskaya suite. Their morphology is diverse. Duration - from 200 - 250 to 2500 m. The prevailing stretch of the North-West, less often - northeast. Dutcherites and trachidolerites, the laying dikes, are distinguished by fresh appearance, have a dark gray and black color, most often have a porphy-colored structure with a fine-grained majority. The main plagioclase (Labrador), Olivine and Klinopyroxen prevail in the composition of porphy-level engines. As part of the main mass present the main plagioclases, pyroxes, olivine, sometimes biotit, magnetite and apatite. Often the components of the complex are enriched with fine-dispersed magnetite and therefore differ in high magnitude.

5.3 .. tectonics

Through the addition of the geological structure of the district of Krasnoyarsk, three structural floors are clearly distinguished. The lower, the folded structural floor is complicated by the formations of the late Precambria and the Lower Middle Cambrian. The medium, transitional structural, forming superimposed depressions, is made by volcanogenic and sedimentary rocks of the Middle-upper Ordovic, Devon and Lower Carbon. Finally, the top, platform structural floor is represented by the hollow with the deposits of the Mesozoic.

Lower Structural Floor (RF3 - € 2) is characterized by a complex deployment of its rocks. The formation of them occurred in the conditions of the open ocean basin and the active continental outskirts of the Pacific type (the situation of the inhabited sea). They are mostly crushed into the stressful folds, mainly linear, and are broken with numerous faults. As part of the floor, two structural tiers are represented - Upperrithic and Vend-Midkumbrian.

The Upper Apronity Structural Tier is represented by the formations of alpine-type hyperbasites (Akhepsky complex), metapsamimmoto-silicon-carbon monogram with elements of carbonate (urmanskaya retinue), metacarbonate with elements of carbon-silicon (manal retinue) and metapic domestic metabasalt metaturashibazalt (Bakhtinsky retinue).

In this area, the formation of this structural tier is mainly developed in the form of tectonic wedges within the Lahetyan-Ustbazaykh zone of faults. The formation of the formation of alpinotype hyperbasites, besides, there are found along other subvertictive faults of the northeast stretch, forming lenzide protrusions. The relationships of the rocks, the stories of this structural tier, with the formations of the Vendous Mediterranean structural tier in the vicinity of the city of Krasnoyarsk are exceptionally tectonic. The occurrence of vendors in the rocks of the cluster series of upper reefs with erosion and angular disagreement, on which it is based on the assignment of these formations to different structural tiers, is established far beyond the territory under consideration.

Tectonic scheme of the surroundings of Krasnoyarsk. Amounted to GV Mironyuk based on E.I. Berzon et al. (2001) and L.K. Kachevsky et al. (2009):

Altai-Sayansky Folded Region: I - Krasnoyarsk Raising: 1 - Kaczynsko-Lithuanian Volcanogenic Depression: 1 A - Maltic Synclinal; 1 b - Karaulninskaya Synclinal; 1 V - Shubbzavodskaya Syncline; 1 g - Kaczynsky Horst. 2 - Derbinsky Anticlinorial (Kulyuksky Block): 2 A - Sliznevsky Brachisinclinal; 2 b - Malosliznev Synclinal; 2 V - Namurt Synclinal; 2G - Namurt anticline. II - Rybinskaya Vpadina: 3 - Krasnoyarsk monoclinary; 4 - Balay Synclinal Zone: 4 A - Zhernovskaya Syncline; 4 b - Sorokinsky anticline.

West Siberian Plate: III - Chulymo-Yenisei deflection. Princesssee Vpadina: 5 A - Arena-Shilinsky shaft; 5 b - Badalik Multi; 5 V - Esaulovsky Multi.

Intrusive and protezy arrays: M1 - lepty; M2 - Shumykhinsky; M3 - Kulyuksky; M4 - Stolbovsky; M5 -Abakatsky; M6 - Sliznenevsky. Carbonate arrays: K1 - Torgashinsky rhygenic.

Fault and their numbers: P1 - Canco-Agulsky (Iysko-Kansky); P2 - Bathaysky; P3 - Kolsky; P4 - Sliznenevsky; P5 - Sosnovsky

As a specific feature of the breeds of the Upperrithic structural tier, it should be noted that they, in their main part, were subjected to a weak regional metamorphism, the level of which corresponds to the most nose of the green-plants,

The Wend-Mediterranean structural tier is complicated exclusively by sedimentary rocks, the accumulation of which is generally characteristic of the situation in the seasons. Carbonate formations are dominated here (limestone-dolomitic, alasrito-limestone, limestone reef); There is also deposits of fluchery formation (tubilic retinue).

The formations of this tier is complicated by the main volume of formations of the lower structural floor in the nearest surroundings of the city of Krasnoyarsk. The sedimentary breeds of the tier on extensive spaces are crumpled into stress linear folds, often overturned, are broken down by numerous discrepancies of the scope of scattering. As a result, cases of repeated summation of the same fragments of the incision are numerous. The immersion of the axes of overturned folds and movers of faults under the average (30-50 °) corners in the zois in the area, which is most typically observed in many sections of the axes under average (30-50 °) corners in the area, which corresponds to the overall movements from the SM in St. Watch the folds and discontinuous disorders of such orientation can be south-west of Akademgorodok, on the descent along the monastery road, and in the assistive part of the Kaltat river. The largest folded structure, folded by the formations of the subjarus under consideration, is located on the Right Bank of Yenisei, the Grassalyznevskaya Synclinal. The axis of this syncline is oriented submeridionially. Its kernel is made by carbonate rocks of Ovsynkovskaya suite, and wings - terrific deposits of tubing suite.

Especially in the nature of the occurrence of Cambrian deposits, a Torgashinsky structural unit is allocated on the right bank of the Bazaja River. There are not characterized by stress linear folds and manifestations of passion tectonics. Here the rocks are assembled into a series of gentle-restrained folds, with angle of fall 25 - 60 o. Often this is a monoclinary falling undermining layers complicated by flexo-shaped beggars. It can be assumed that this block in the era of folding played the role of auththon, in relation to which the remaining blocks of the lower structural floor were subjected to passing movements.

The average structural floor (O2-3 - C1) is represented by sedimentary and volcanogenic formations of the Ordovic and the average Paleozoic, performing individual depressions, with a sharply pronounced structural disagreement superimposed on the complex formalized folding complex of the lower structural floor. The formation of these depadies proceeded on the young cortex of continental type in the setting of the rear part of the active continental outskirts. In its framework, two sub-stores that are characterized by the similarity of tectonic structures and, partly, geological formations, but in two different stages of tectonic activation - medium-Upperordovik and Devonian-ninecalented are available.

Middle-Upperordovik LED (O2-3). The formation of this otignation is presented exclusively by the magmatic rocks - volcanics of the trachibasant-fuchit-trachryrylitic formations (relative to the Imyar Speat or to the Divnogorsk thicker (O2-3). They perform Kaczynsko-Shumykhinsky volkano-tectonic depression, located mainly on the left bank of the Yenisei of the west of the city of Krasnoyarsk. This is Colorful collar, in a modern cut, stretching about 50 km in the latitudinal direction (from the city of Krasnoyarsk to the city of Divnogorsk and west), up to 30 km wide. Performing depression Lava streams and pouring tuffs (at angles up to 30 - 35 °) are immersed from edges Depressed in the northern direction, where they disagree with more young sediments (Devonian or Jurassic). With the same stage of tectonic development, the formation of large laccolite-like introsions of the Shenit-Granosienite formation (Pillars complex) developed by a part within the Kaczynsko-Shumykhin depression is part of - in the structures of its folds Self framing (among the formations of the lower structural floor).

Devonian-ninecalented landing (D1 - C1). Its breeds performed the Rybinskaya Vadina, opening from the city of Krasnoyarsk in the eastern and southeast directions. Nizhnedyevonian education of this sub-storey is represented by a combination of MOLASSOVO and trachibasant-fuchit-trachryiroly formations that shapely form a Karymovsky retinue. The overlying deposits are predominantly predominantly by the formations of continental terrigenous red-color formation with elements of carbonate, as well as the terrigenous-telecoclastic formation (Krasnogoryevskaya Sweet of the lower carbon). In the structure of the sub-storey, several structural tiers are distinguished: Nizhnevonsky (Karymovskaya Sweet), Middle-Verkhnedyevonsky (Pavlovskaya and Kungus Sweets) and Nizhnekamenegonal (Chargin and Krasnogoryevskaya Sweets). The boundaries between structural tiers are well-pronounced surfaces of the erosion, which are also timed angular disagreement.

The main structural elements of this sub-storey in the neighborhood of the city of Krasnoyarsk are Krasnoyarsk Monocline and the Zherern Synclinal. Krasnoyarsk Monocline is stretched from the northwestern suburb of the city in the south-east direction. Within its limits, there is a steady monoclinal drop in Devonian and coal deposits in the northeast direction at an angles to 20 °. Zhernovskaya (Berezovskaya Syncline) replaces the Krasnoyarsk Monocline in the Southern direction. This is a brachiform fold located in the valley of the Berezovsky River in the area of \u200b\u200bZykovo Station and Paryshino platforms. It is folded by rocks of various packs of Karymovskaya suite. The fold axis is oriented submeridian; Hollow hinge immersed in a yuvan direction. Flops in the southwespal wing - 15 - 30 °, and 30 - 55 ° - in northeast.

The upper structural floor (j) in the territory under consideration is entirely formed by the deposits of the Jurassic system. They belong to the coal-like limn formation and perform the system of depression of the Canco-Achinsky bromade basin, stretching the sub-liablon along the northern periphery of the Altai-Sayan folded area. The formation of this floor is listed with a sharp structural disagreement on all underlying sediments. In the edge parts of the depression, there are sometimes their adjacent to more ancient formations. Characteristic of the very hollow lowering - the angles of the fall usually do not exceed 5 °. Only in the edge parts, near the faults and in rare flexures, they may increase to the first dozen degrees.

The Jurassic deposits of the district of Krasnoyarsk belong to one of the Vpadin of the Canadian-Achinsky Basin - Chulymo-Yenisei. Within its limits on the territory of the city and its surroundings, two gentlemen of Multi - Badalik and Esaulovskaya are allocated, as well as a meridional oriented Azeri-Shilinsky shaft, which limits the Badalyk Mount from the West.