Standard

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.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Kostyreva, EA & Sotnich, IS 2017, 'Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise', Russian Geology and Geophysics, Том. 58, № 3-4, стр. 434-442. https://doi.org/10.1016/j.rgg.2016.09.019

APA

Kostyreva, E. A., & Sotnich, I. S. (2017). Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise. Russian Geology and Geophysics, 58(3-4), 434-442. https://doi.org/10.1016/j.rgg.2016.09.019

Vancouver

Kostyreva EA, Sotnich IS. Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise. Russian Geology and Geophysics. 2017 апр. 1;58(3-4):434-442. doi: 10.1016/j.rgg.2016.09.019

Author

Kostyreva, E. A. ; Sotnich, I. S. / Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise. в: Russian Geology and Geophysics. 2017 ; Том 58, № 3-4. стр. 434-442.

BibTeX

@article{680e9bfc35d14acfa562c683d2310ea9,
title = "Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise",
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.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2016.09.019",
language = "English",
volume = "58",
pages = "434--442",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "3-4",

}

RIS

TY - JOUR

T1 - Geochemistry of organic matter of the Bazhenov Formation in the north of the Khantei anteclise

AU - Kostyreva, E. A.

AU - Sotnich, I. S.

PY - 2017/4/1

Y1 - 2017/4/1

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

KW - EVOLUTION

KW - HISTORY

UR - http://www.scopus.com/inward/record.url?scp=85018486394&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.09.019

DO - 10.1016/j.rgg.2016.09.019

M3 - Article

AN - SCOPUS:85018486394

VL - 58

SP - 434

EP - 442

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3-4

ER -

ID: 10040641