Assessment of Mesozoic-Kainozoic climate impact on oil-source rock potential (West Siberia); IOP Conference Series: Earth and Environmental Science; Vol. 27 : Problems of Geology and Subsurface Development
| Parent link: | IOP Conference Series: Earth and Environmental Science Vol. 27 : Problems of Geology and Subsurface Development.— 2015.— [012023, 6 p.] |
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| Автор: | |
| Співавтори: | , |
| Інші автори: | , |
| Резюме: | Title screen Based on paleotemperature modeling, the evaluation of the effect of Neo-Pleistocene permafrost rock thickness on geothermal regime of the Bazhenov deposits has been performed. It has been stated that permafrost about 300 m in thickness must be considered for appropriate reconstruction of geothermal history of source rocks in the south-east areas of West Siberia. This condition is relevant to a consistent consideration of oil-generation phase history and can prevent underestimation (to 25%) of hydrocarbon-in-place resources. Режим доступа: по договору с организацией-держателем ресурса |
| Мова: | Англійська |
| Опубліковано: |
2015
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| Серія: | Geophysical Surveying Methods for Ore Deposit Prospecting. Geoinformation Systems in Geophysical Surveys |
| Предмети: | |
| Онлайн доступ: | http://dx.doi.org/10.1088/1755-1315/27/1/012023 http://earchive.tpu.ru/handle/11683/19922 |
| Формат: | Електронний ресурс Частина з книги |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645081 |
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| 200 | 1 | |a Assessment of Mesozoic-Kainozoic climate impact on oil-source rock potential (West Siberia) |f А. А. Iskorkina, V. I. Isaev, D. A. Terre | |
| 203 | |a Text |c electronic | ||
| 225 | 1 | |a Geophysical Surveying Methods for Ore Deposit Prospecting. Geoinformation Systems in Geophysical Surveys | |
| 300 | |a Title screen | ||
| 320 | |a [References: 9 tit.] | ||
| 330 | |a Based on paleotemperature modeling, the evaluation of the effect of Neo-Pleistocene permafrost rock thickness on geothermal regime of the Bazhenov deposits has been performed. It has been stated that permafrost about 300 m in thickness must be considered for appropriate reconstruction of geothermal history of source rocks in the south-east areas of West Siberia. This condition is relevant to a consistent consideration of oil-generation phase history and can prevent underestimation (to 25%) of hydrocarbon-in-place resources. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | 0 | |0 (RuTPU)RU\TPU\network\2499 |t IOP Conference Series: Earth and Environmental Science | |
| 463 | 0 | |0 (RuTPU)RU\TPU\network\10088 |t Vol. 27 : Problems of Geology and Subsurface Development |o XIX International Scientific Symposium in honor of Academician M. A. Usov, 6–10 April 2015, Tomsk, Russia |v [012023, 6 p.] |d 2015 | |
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| 701 | 1 | |a Isaev |b V. I. |c geologist |c Professor of Tomsk Polytechnic University, doctor of geological-mineralogical Sciences |f 1952- |g Valery Ivanovich |3 (RuTPU)RU\TPU\pers\32557 | |
| 701 | 1 | |a Terre |b D. A. |c linguist |c Associate Professor of Tomsk Polytechnic University, Candidate of philological science |f 1980- |g Dina Anatolievna |3 (RuTPU)RU\TPU\pers\30937 |9 15175 | |
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