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; Applied Clay Science; Vol. 136
| Parent link: | Applied Clay Science Vol. 136.— 2017.— [P. 75-89] |
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| 共著者: | , , |
| その他の著者: | , , , , |
| 要約: | 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 |
| 言語: | 英語 |
| 出版事項: |
2017
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| 主題: | |
| オンライン･アクセス: | https://doi.org/10.1016/j.clay.2016.11.009 |
| フォーマット: | MixedMaterials 電子媒体 図書の章 |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656813 |