TY - JOUR

T1 - Mesozoic-cenozoic climate and the geothermal regime of the oil source kiterbyutskaya suite of the arctic region of western siberia

AU - Isaev, Valery I.

AU - Iskorkina, Albina A.

AU - Lobova, Galina A.

AU - Luneva, Tatyana E.

AU - Osipova, Elizaveta N.

AU - Ayupov, Roman Sh

AU - Igenbaeva, Natalya O.

AU - Fomin, Alexander N.

N1 - Исаев В.И., Искоркина А.А., Лобова Г.А., Лунёва Т.Е., Осипова Е.Н., Аюпов Р.Ш., Игенбаева Н.О., Фомин А.Н. Мезозойско-кайнозойский климат и геотермический режим нефтематеринской китербютской свиты арктического региона Западной Сибири // Георесурсы. - 2018. - Т. 20. - № 4, Ч. 2. - С. 386-395.

PY - 2018

Y1 - 2018

N2 - Using the example of paleotemperature modeling of the Kiterbyutskaya suite of the Mesozoic-Cenozoic section, opened by a deep well at the Bovanenkovskoye oil – gas condensate field (Yamal Peninsula), the influence of paleoclimate factors on the thermal history of the Lower Jurassic oil source deposits, the duration of the main phase of petroleum formation and the value of the paleothermometric maximum and oil generation density. The original computer methodology is described, which takes into account the parameters of the tectonic and sedimentation history, as well as the history of the thermophysical properties of the sedimentary formation, including permafrost and glaciers, and not requiring a priori information about the values and nature of the deep heat flow is given. The features of the model parametrization are shown. The reliability of the results is confidently controlled by the geophysical criterion of the “discrepancy”, comparison with experimental data on the heat flow, and consistency with the drilling data. The presentation is based on the works of the Tomsk School of Geothermics, carried out as part of the development of a methodological base of geothermics as a geophysical oil prospecting method.

AB - Using the example of paleotemperature modeling of the Kiterbyutskaya suite of the Mesozoic-Cenozoic section, opened by a deep well at the Bovanenkovskoye oil – gas condensate field (Yamal Peninsula), the influence of paleoclimate factors on the thermal history of the Lower Jurassic oil source deposits, the duration of the main phase of petroleum formation and the value of the paleothermometric maximum and oil generation density. The original computer methodology is described, which takes into account the parameters of the tectonic and sedimentation history, as well as the history of the thermophysical properties of the sedimentary formation, including permafrost and glaciers, and not requiring a priori information about the values and nature of the deep heat flow is given. The features of the model parametrization are shown. The reliability of the results is confidently controlled by the geophysical criterion of the “discrepancy”, comparison with experimental data on the heat flow, and consistency with the drilling data. The presentation is based on the works of the Tomsk School of Geothermics, carried out as part of the development of a methodological base of geothermics as a geophysical oil prospecting method.

KW - Hydrocarbon resources

KW - Kiterbyutskaya suite

KW - Modelling of geothermal regime

KW - Paleoclimate

KW - Works of the Tomsk School of Geothermics

KW - Yamal Peninsula

KW - PETROLEUM

KW - modelling of geothermal regime

KW - works of the Tomsk School of Geothermics

KW - paleoclimate

KW - hydrocarbon resources

UR - http://www.scopus.com/inward/record.url?scp=85081215127&partnerID=8YFLogxK

UR - https://www.elibrary.ru/item.asp?id=36736142

U2 - 10.18599/grs.2018.4.386-395

DO - 10.18599/grs.2018.4.386-395

M3 - Review article

AN - SCOPUS:85081215127

VL - 20

SP - 386

EP - 395

JO - Георесурсы

JF - Георесурсы

SN - 1608-5043

IS - 4

M1 - 13

ER -