Influences of Neo-Pleistocene permafrost on thermal history of petromaternal Lower Jurassic Togur suite (Tomsk region)

Influences of Neo-Pleistocene permafrost on thermal history of petromaternal Lower Jurassic Togur suite (Tomsk region)

Bibliographic Details
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012009, 6 p.]
Main Author: Iskorkina A. A. Albina Albertovna
Corporate Author: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геофизики (ГЕОФ)
Other Authors: Isaev V. I. Valery Ivanovich, Fomin A. N.
Summary:Title screen
Based on paleotemperature modeling, evaluation of Neo-Pleistocene permafrost rock thickness impact on geothermal regime of the petromaternal Togur deposits has been performed within the territory of oil fields of the Tomsk region (the southeast of Western Siberia). It has been stated that paleopermafrost with the thickness of about 300 m must be considered for appropriate reconstruction of geothermal history of petromaternal rocks in the south-east areas of West Siberia. This condition is relevant to a consistent consideration of thermal history of maternal deposits in course of assessment of resources by a volumetric- genetic method.
Published: 2016
Series:Mineralogy, Geochemistry and Petrography
Subjects:
электронный ресурс
труды учёных ТПУ
вечная мерзлота
тогурская свита
Томская область
мерзлота
горные породы
нефтяные месторождения
углеводороды
температура
Online Access:http://dx.doi.org/10.1088/1755-1315/43/1/012009
http://earchive.tpu.ru/handle/11683/35196
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650804

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