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

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

Bibliographic Details
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 27 : Problems of Geology and Subsurface Development.— 2015.— [012023, 6 p.]
Main Author: Iskorkina A. A. Albina Albertovna
Corporate Authors: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра иностранных языков (ИЯПР), Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геофизики (ГЕОФ)
Other Authors: Isaev V. I. Valery Ivanovich, Terre D. A. Dina Anatolievna
Summary: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
Language:English
Published: 2015
Series:Geophysical Surveying Methods for Ore Deposit Prospecting. Geoinformation Systems in Geophysical Surveys
Subjects:
электронный ресурс
труды учёных ТПУ
климат
нефти
Западная Сибирь
палеотемпературы
вечная мерзлота
углеводороды
Online Access:http://dx.doi.org/10.1088/1755-1315/27/1/012023
http://earchive.tpu.ru/handle/11683/19922
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645081
Description
Summary: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
DOI:10.1088/1755-1315/27/1/012023

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