Standard

Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia). / Fursenko, E. A.; Kim, N. S.

в: Petroleum Chemistry, Том 59, № 10, 01.10.2019, стр. 1138-1146.

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

Harvard

Fursenko, EA & Kim, NS 2019, 'Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)', Petroleum Chemistry, Том. 59, № 10, стр. 1138-1146. https://doi.org/10.1134/S0965544119100049

APA

Fursenko, E. A., & Kim, N. S. (2019). Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia). Petroleum Chemistry, 59(10), 1138-1146. https://doi.org/10.1134/S0965544119100049

Vancouver

Fursenko EA, Kim NS. Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia). Petroleum Chemistry. 2019 окт. 1;59(10):1138-1146. doi: 10.1134/S0965544119100049

Author

Fursenko, E. A. ; Kim, N. S. / Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia). в: Petroleum Chemistry. 2019 ; Том 59, № 10. стр. 1138-1146.

BibTeX

@article{eee8ddde1500446f9e29670293655434,
title = "Geochemistry of Condensates of Maloyamal{\textquoteright}skoe Field (Yamal Peninsula, Western Siberia)",
abstract = "Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal{\textquoteright}skoe field (beds Yu2–3, Yu4 and Yu6, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.",
keywords = "condensates, dispersed organic matter, geochemistry, the Yamal peninsula, PETROLEUM, DEPOSITIONAL ENVIRONMENT, BASIN, MATURITY",
author = "Fursenko, {E. A.} and Kim, {N. S.}",
year = "2019",
month = oct,
day = "1",
doi = "10.1134/S0965544119100049",
language = "English",
volume = "59",
pages = "1138--1146",
journal = "Petroleum Chemistry",
issn = "0965-5441",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "10",

}

RIS

TY - JOUR

T1 - Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)

AU - Fursenko, E. A.

AU - Kim, N. S.

PY - 2019/10/1

Y1 - 2019/10/1

N2 - Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu2–3, Yu4 and Yu6, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.

AB - Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu2–3, Yu4 and Yu6, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.

KW - condensates

KW - dispersed organic matter

KW - geochemistry

KW - the Yamal peninsula

KW - PETROLEUM

KW - DEPOSITIONAL ENVIRONMENT

KW - BASIN

KW - MATURITY

UR - http://www.scopus.com/inward/record.url?scp=85073520042&partnerID=8YFLogxK

U2 - 10.1134/S0965544119100049

DO - 10.1134/S0965544119100049

M3 - Article

AN - SCOPUS:85073520042

VL - 59

SP - 1138

EP - 1146

JO - Petroleum Chemistry

JF - Petroleum Chemistry

SN - 0965-5441

IS - 10

ER -

ID: 21927410