| 000 | 04482nlm0a2200505 4500 | ||
|---|---|---|---|
| 001 | 656615 | ||
| 005 | 20231030041436.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\23056 | ||
| 090 | _a656615 | ||
| 100 | _a20171123d2017 k y0engy50 ca | ||
| 101 | 0 | _aeng | |
| 102 | _aBG | ||
| 105 | _ay z 100zy | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aShale Oil of South Segment of Koltogor-Upaleorift _fG. A. Lobova [et al.] |
|
| 203 |
_aText _celectronic |
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| 300 | _aTitle screen | ||
| 330 | _aThe exploration of shale oil is still the actual problem in the Western Siberia. The Upper Jurassic Bazhenov bituminous strata are widespread here. The Bazhenov strata is perspective shale formation because it has the high quantity of organic carbon and considerable thickness. This region is the most interesting for exploration of shale oil. The object of research are located within the Koltogor-Urengoy paleorift and its fraiming structure. The reconstruction of the tectonic and thermal history of Bazhenov formation was done using a software suite for paleotemperature modeling. The key factor in the realization of oil generation potential of a source rock is its thermal history defining the starting time and the intensity of oil generation. The locations of Bazhenov oil generation are marked by geotemperature criteria. The conditional integral index R was calculated for assessing the density value of the generated Bazhenov oil which allows for cumulatively taking into account the geotemperature dynamics of the main oil generation zone of the source rocks. The high-prospects zones were allocated for exploration of shale oil. Koltogor-Urengoy paleorift zone which was completed activization 160-170 mln. years ago is not different by the reconstructed heat flow density and resource distribution density of Upper Jurassic shale oil. The comparison of highly prospective territories with actually established direct signs of oil-bearing Upper Jurassic source rocks are showed high reliability for zoning. Conditional settlement confidence level is 80%. | ||
| 333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
| 461 |
_tSGEM. 17th International Multidisciplinary Scientific GeoConference _oconference proceedings, Albena, Bulgariaм, 29 June - 5 July, 2017 _d2017 |
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| 463 |
_tVol. 17, iss. 14 _v[P. 867-874] _d2017 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aсланцевая нефть | |
| 610 | 1 | _aпалеотемпературное моделирование | |
| 610 | 1 | _aплотность | |
| 610 | 1 | _aбаженовские отложения | |
| 610 | 1 | _ashale oil | |
| 610 | 1 | _aBazhenov formation | |
| 610 | 1 | _apaleotemperature modeling | |
| 610 | 1 | _aresource density distribution | |
| 610 | 1 | _aKoltogor-Urengoy paleorift | |
| 610 | 1 | _aКолтогор-Уренгойский палеорифт | |
| 701 | 1 |
_aLobova _bG. A. _cgeophysicist _cAssociate Professor of Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences _f1952- _gGalina Anatolyevna _2stltpush _3(RuTPU)RU\TPU\pers\33915 |
|
| 701 | 1 |
_aStotsky _bV. V. _cgeologist _cassistant Professor of Tomsk Polytechnic University _f1992- _gVitaly Valerjevich _2stltpush _3(RuTPU)RU\TPU\pers\39850 |
|
| 701 | 1 |
_aIsaev _bV. I. _cgeologist _cProfessor of Tomsk Polytechnic University, doctor of geological-mineralogical Sciences _f1952- _gValery Ivanovich _2stltpush _3(RuTPU)RU\TPU\pers\32557 |
|
| 701 | 1 |
_aStarostenko _bV. I. _gVitaly Ivanovich |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра транспорта и хранения нефти и газа (ТХНГ) _h257 _2stltpush _3(RuTPU)RU\TPU\col\18661 |
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра физической и аналитической химии (ФАХ) _h94 _2stltpush _3(RuTPU)RU\TPU\col\18656 |
| 801 | 2 |
_aRU _b63413507 _c20180213 _gRCR |
|
| 856 | 4 | _uhttps://doi.org/10.5593/SGEM2017/14/S06.108 | |
| 856 | 4 | _uhttps://sgemworld.at/sgemlib/spip.php?article9384 | |
| 942 | _cCF | ||