Standard

Classification of rocks of the Bazhenov Formation. / Kontorovich, A. E.; Yan, P. A.; Zamirailova, A. G. и др.

в: Russian Geology and Geophysics, Том 57, № 11, 01.11.2016, стр. 1606-1612.

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

Harvard

Kontorovich, AE, Yan, PA, Zamirailova, AG, Kostyreva, EA & Eder, VG 2016, 'Classification of rocks of the Bazhenov Formation', Russian Geology and Geophysics, Том. 57, № 11, стр. 1606-1612. https://doi.org/10.1016/j.rgg.2016.10.006

APA

Kontorovich, A. E., Yan, P. A., Zamirailova, A. G., Kostyreva, E. A., & Eder, V. G. (2016). Classification of rocks of the Bazhenov Formation. Russian Geology and Geophysics, 57(11), 1606-1612. https://doi.org/10.1016/j.rgg.2016.10.006

Vancouver

Kontorovich AE, Yan PA, Zamirailova AG, Kostyreva EA, Eder VG. Classification of rocks of the Bazhenov Formation. Russian Geology and Geophysics. 2016 нояб. 1;57(11):1606-1612. doi: 10.1016/j.rgg.2016.10.006

Author

Kontorovich, A. E. ; Yan, P. A. ; Zamirailova, A. G. и др. / Classification of rocks of the Bazhenov Formation. в: Russian Geology and Geophysics. 2016 ; Том 57, № 11. стр. 1606-1612.

BibTeX

@article{72f566a5a35a454691512bb79d146b93,
title = "Classification of rocks of the Bazhenov Formation",
abstract = "In this study, we propose a new classification of rocks of the Bazhenov Formation based on the proportions of four principal components (siliceous, clay, and carbonate minerals and organic matter (kerogen)) of mostly biochemogenic and, to a lesser extent, allothigenic origin. The classification is based on the results of mineralogical and chemical analyses of more than 400 core samples from 15 wells drilled within the Bazhenov Formation, West Siberian petroleum basin. Four major classes of rocks, divided into 16 subclasses, have been recognized. The terms mixtite and kerogen-rich rock are introduced. Mixtites (biochemogenic mixtites) are defined as a class of rocks containing less than 50% of each component, including kerogen. It was shown that the most common rocks of the Bazhenov Formation are siliceous-argillaceous, kerogen-siliceous, and kerogen-argillaceous-siliceous mixtites and kerogen silicites, which together account for ~ 65% of all samples analyzed. The proposed approach can be used to study organic-rich black shales in different sedimentary basins worldwide.",
keywords = "Bazhenov Formation, petroleum source rocks, rock classification, West Siberia",
author = "Kontorovich, {A. E.} and Yan, {P. A.} and Zamirailova, {A. G.} and Kostyreva, {E. A.} and Eder, {V. G.}",
year = "2016",
month = nov,
day = "1",
doi = "10.1016/j.rgg.2016.10.006",
language = "English",
volume = "57",
pages = "1606--1612",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "11",

}

RIS

TY - JOUR

T1 - Classification of rocks of the Bazhenov Formation

AU - Kontorovich, A. E.

AU - Yan, P. A.

AU - Zamirailova, A. G.

AU - Kostyreva, E. A.

AU - Eder, V. G.

PY - 2016/11/1

Y1 - 2016/11/1

N2 - In this study, we propose a new classification of rocks of the Bazhenov Formation based on the proportions of four principal components (siliceous, clay, and carbonate minerals and organic matter (kerogen)) of mostly biochemogenic and, to a lesser extent, allothigenic origin. The classification is based on the results of mineralogical and chemical analyses of more than 400 core samples from 15 wells drilled within the Bazhenov Formation, West Siberian petroleum basin. Four major classes of rocks, divided into 16 subclasses, have been recognized. The terms mixtite and kerogen-rich rock are introduced. Mixtites (biochemogenic mixtites) are defined as a class of rocks containing less than 50% of each component, including kerogen. It was shown that the most common rocks of the Bazhenov Formation are siliceous-argillaceous, kerogen-siliceous, and kerogen-argillaceous-siliceous mixtites and kerogen silicites, which together account for ~ 65% of all samples analyzed. The proposed approach can be used to study organic-rich black shales in different sedimentary basins worldwide.

AB - In this study, we propose a new classification of rocks of the Bazhenov Formation based on the proportions of four principal components (siliceous, clay, and carbonate minerals and organic matter (kerogen)) of mostly biochemogenic and, to a lesser extent, allothigenic origin. The classification is based on the results of mineralogical and chemical analyses of more than 400 core samples from 15 wells drilled within the Bazhenov Formation, West Siberian petroleum basin. Four major classes of rocks, divided into 16 subclasses, have been recognized. The terms mixtite and kerogen-rich rock are introduced. Mixtites (biochemogenic mixtites) are defined as a class of rocks containing less than 50% of each component, including kerogen. It was shown that the most common rocks of the Bazhenov Formation are siliceous-argillaceous, kerogen-siliceous, and kerogen-argillaceous-siliceous mixtites and kerogen silicites, which together account for ~ 65% of all samples analyzed. The proposed approach can be used to study organic-rich black shales in different sedimentary basins worldwide.

KW - Bazhenov Formation

KW - petroleum source rocks

KW - rock classification

KW - West Siberia

UR - http://www.scopus.com/inward/record.url?scp=84995747450&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.10.006

DO - 10.1016/j.rgg.2016.10.006

M3 - Article

AN - SCOPUS:84995747450

VL - 57

SP - 1606

EP - 1612

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -

ID: 25503997