Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise

E. A. Kostyreva; I. S. Sotnich

doi:10.1016/j.rgg.2016.09.019

Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise

E. A. Kostyreva, I. S. Sotnich

Геолого-геофизический факультет

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

6 Цитирования (Scopus)

Аннотация

Results of comprehensive geochemical studies of dispersed organic matter of the Bazhenov Formation are presented. The maximum total contents of organic carbon are found in the areas of the Surgut arch and South Nadym megamonoclise. The contents of organic matter are high (up to 24%) at the top of the formation section and gradually decrease to its bottom. By pyrolysis parameters and the composition of hydrocarbon biomarkers, the organic matter is referred to as type II kerogen (sapropelic organic matter) and is localized in the oil window.

Язык оригинала	английский
Страницы (с-по)	434-442
Число страниц	9
Журнал	Russian Geology and Geophysics
Том	58
Номер выпуска	3-4
DOI	https://doi.org/10.1016/j.rgg.2016.09.019
Состояние	Опубликовано - 1 апр. 2017

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10.1016/j.rgg.2016.09.019

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abstract = "Results of comprehensive geochemical studies of dispersed organic matter of the Bazhenov Formation are presented. The maximum total contents of organic carbon are found in the areas of the Surgut arch and South Nadym megamonoclise. The contents of organic matter are high (up to 24%) at the top of the formation section and gradually decrease to its bottom. By pyrolysis parameters and the composition of hydrocarbon biomarkers, the organic matter is referred to as type II kerogen (sapropelic organic matter) and is localized in the oil window.",

keywords = "Bazhenov Formation, biomarker hydrocarbons, chloroform-extracted bitumens, organic matter, pyrolysis, total organic carbon, EVOLUTION, HISTORY",

author = "Kostyreva, {E. A.} and Sotnich, {I. S.}",

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Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise. / Kostyreva, E. A.; Sotnich, I. S.

В: Russian Geology and Geophysics, Том 58, № 3-4, 01.04.2017, стр. 434-442.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

TY - JOUR

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AU - Kostyreva, E. A.

AU - Sotnich, I. S.

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N2 - Results of comprehensive geochemical studies of dispersed organic matter of the Bazhenov Formation are presented. The maximum total contents of organic carbon are found in the areas of the Surgut arch and South Nadym megamonoclise. The contents of organic matter are high (up to 24%) at the top of the formation section and gradually decrease to its bottom. By pyrolysis parameters and the composition of hydrocarbon biomarkers, the organic matter is referred to as type II kerogen (sapropelic organic matter) and is localized in the oil window.

AB - Results of comprehensive geochemical studies of dispersed organic matter of the Bazhenov Formation are presented. The maximum total contents of organic carbon are found in the areas of the Surgut arch and South Nadym megamonoclise. The contents of organic matter are high (up to 24%) at the top of the formation section and gradually decrease to its bottom. By pyrolysis parameters and the composition of hydrocarbon biomarkers, the organic matter is referred to as type II kerogen (sapropelic organic matter) and is localized in the oil window.

KW - Bazhenov Formation

KW - biomarker hydrocarbons

KW - chloroform-extracted bitumens

KW - organic matter

KW - pyrolysis

KW - total organic carbon

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