Influences of Neo-Pleistocene permafrost on thermal history of petromaternal Lower Jurassic Togur suite (Tomsk region); IOP Conference Series: Earth and Environmental Science; Vol. 43 : Problems of Geology and Subsurface Development

গ্রন্থ-পঞ্জীর বিবরন
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012009, 6 p.]
প্রধান লেখক: Iskorkina A. A. Albina Albertovna
সংস্থা লেখক: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геофизики (ГЕОФ)
অন্যান্য লেখক: Isaev V. I. Valery Ivanovich, Fomin A. N.
সংক্ষিপ্ত: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.
ভাষা:ইংরেজি
প্রকাশিত: 2016
মালা:Mineralogy, Geochemistry and Petrography
বিষয়গুলি:
অনলাইন ব্যবহার করুন:http://dx.doi.org/10.1088/1755-1315/43/1/012009
http://earchive.tpu.ru/handle/11683/35196
বিন্যাস: বৈদ্যুতিক গ্রন্থের অধ্যায়
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650804

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