Classification of rocks of the Bazhenov Formation. / Kontorovich, A. E.; Yan, P. A.; Zamirailova, A. G. et al.
In: Russian Geology and Geophysics, Vol. 57, No. 11, 01.11.2016, p. 1606-1612.Research output: Contribution to journal › Article › peer-review
}
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