| 000 | 03887nla2a2200481 4500 | ||
|---|---|---|---|
| 001 | 650803 | ||
| 005 | 20231030041005.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\16052 | ||
| 035 | _aRU\TPU\network\16051 | ||
| 090 | _a650803 | ||
| 100 | _a20161021a2016 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 105 | _ay z 100zy | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aFracture system influence on the reservoirs rock formation of Ordovician-Devonian carbonates in West Siberia tectonic depression _fA. E. Koveshnikov, A. C. Nesterova, T. F. Dolgaya |
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| 203 |
_aText _celectronic |
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| 225 | 1 | _aMineralogy, Geochemistry and Petrography | |
| 300 | _aTitle screen | ||
| 320 | _a[References: 10 tit.] | ||
| 330 | _aDuring the Paleozoic period from the beginning of the Cambrian to the end of the Carboniferous in the boundaries of the West Siberia tectonic depression there occurred the sea, where the carbonate platforms were formed by the limestones accumulation. All the area at the end of the Carboniferous period was turned to land. Resulting from Gertsynskaya folding in the times of Permian - Triassic the formed deposits were folded and denudated to a considerable extent. Besides, the reservoir rocks of the crust of weathering including redeposited one, were formed as a result of hypergenesis, during the continental stand of the area in the near-surface zone. A new geological prospecting unit has been suggested which underlies these crusts of weathering and formed during fracture tectonic processes with hydrothermal-metasomatic limestones reworking and the processes of hydrothermal leaching and dolomitization. So, in the carbonate platforms the system of fissure zones related to tectonic disturbance was formed. This has a dendrite profile where the series of tangential, more thinned fractures deviate from the stem and finish in pores and caverns. The carbonate platforms formation in the West Siberia tectonic depression has been analyzed, their dynamics and gradual increasing from the minimal in Ordovician and Silurian to maximal at the end of the Late Devonian has been shown. | ||
| 461 | 0 |
_0(RuTPU)RU\TPU\network\2499 _tIOP Conference Series: Earth and Environmental Science |
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| 463 | 0 |
_0(RuTPU)RU\TPU\network\16030 _tVol. 43 : Problems of Geology and Subsurface Development _oXX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia _v[012008, 7 p.] _d2016 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aводохранилища | |
| 610 | 1 | _aордовик | |
| 610 | 1 | _aкарбонаты | |
| 610 | 1 | _aЗападная Сибирь | |
| 610 | 1 | _aсинеклизы | |
| 610 | 1 | _aгеологоразведка | |
| 610 | 1 | _aпластовые пробы | |
| 610 | 1 | _aкарбонатные породы | |
| 610 | 1 | _aтектонические впадины | |
| 700 | 1 |
_aKoveshnikov _bA. E. _cGeologist _cAssociate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences _f1953- _gAleksandr Evgenievich _2stltpush _3(RuTPU)RU\TPU\pers\32375 |
|
| 701 | 1 |
_aNesterova _bA. C. |
|
| 701 | 1 |
_aDolgaya _bT. F. _clinguist _cSenior Lecturer of Tomsk Polytechnic University _f1952- _gTatiana Fedorovna _2stltpush _3(RuTPU)RU\TPU\pers\30911 |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра геологии и разведки полезных ископаемых (ГРПИ) _h2181 _2stltpush _3(RuTPU)RU\TPU\col\18660 |
| 801 | 2 |
_aRU _b63413507 _c20170120 _gRCR |
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| 856 | 4 | _uhttp://dx.doi.org/10.1088/1755-1315/43/1/012008 | |
| 856 | 4 | _uhttp://earchive.tpu.ru/handle/11683/35185 | |
| 942 | _cCF | ||