The mineralogy of the clayey-silty siliceous rocks in the Bazhenov Shale Formation (Upper Jurassic) in the west Siberian Basin, Russia: The role of diagenesis and possible implications for their exploitation as an unconventional hydrocarbon reservoir

The mineralogy of the clayey-silty siliceous rocks in the Bazhenov Shale Formation (Upper Jurassic) in the west Siberian Basin, Russia: The role of diagenesis and possible implications for their exploitation as an unconventional hydrocarbon reservoir

Bibliographic Details
Parent link:Applied Clay Science
Vol. 136.— 2017.— [P. 75-89]
Corporate Authors: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ), Национальный исследовательский Томский политехнический университет (ТПУ) Институт физики высоких технологий (ИФВТ) Лаборатория № 12, Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра проектирования объектов нефтегазового комплекса (ПОНК)
Other Authors: Shaldybin M. V. Mikhail Viktorovich, Lopushnyak Yu. M., Goncharov I. V. Ivan Vasilyevich, Wilson M. J. Michael Jeffrey, Mendis B. G. Budhika
Summary:Title screen
The Bazhenov Shale Formation (BSF) of the west Siberian Basin is considered to be a promising unconventional hydrocarbon reservoir, acting as a source, store and seal of the oil and gas contained therein. It has a high content of organic matter, ranging from 2 to 20% (average 8–12%), and was deposited in a marine environment at an average water depth of 2220 to 2500 m where depositional conditions were of an intensely reducing nature. Deposition took place over a period of 8 to 10 million years mainly during Upper Jurassic times.
Режим доступа: по договору с организацией-держателем ресурса
Published: 2017
Subjects:
электронный ресурс
труды учёных ТПУ
баженовские отложения
сланцы
глинистые минералы
иллиты
альбиты
bazhenov formation
diagenesis
unconventional hydrocarbon reservoirs
shale
clay minerals
illite
albite
Online Access:https://doi.org/10.1016/j.clay.2016.11.009
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656813
Description
Summary:Title screen
The Bazhenov Shale Formation (BSF) of the west Siberian Basin is considered to be a promising unconventional hydrocarbon reservoir, acting as a source, store and seal of the oil and gas contained therein. It has a high content of organic matter, ranging from 2 to 20% (average 8–12%), and was deposited in a marine environment at an average water depth of 2220 to 2500 m where depositional conditions were of an intensely reducing nature. Deposition took place over a period of 8 to 10 million years mainly during Upper Jurassic times.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1016/j.clay.2016.11.009

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