Standard

Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia). / Kontorovich, A. E.; Ponomareva, E. V.; Burshtein, L. M. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 3, 01.03.2018, p. 285-298.

Research output: Contribution to journal › Article › peer-review

Harvard

Kontorovich, AE, Ponomareva, EV, Burshtein, LM, Glinskikh, VN, Kim, NS, Kostyreva, EA, Pavlova, MA, Rodchenko, AP & Yan, PA 2018, 'Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia)', Russian Geology and Geophysics, vol. 59, no. 3, pp. 285-298. https://doi.org/10.1016/j.rgg.2018.03.007

APA

Kontorovich, A. E., Ponomareva, E. V., Burshtein, L. M., Glinskikh, V. N., Kim, N. S., Kostyreva, E. A., Pavlova, M. A., Rodchenko, A. P., & Yan, P. A. (2018). Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia). Russian Geology and Geophysics, 59(3), 285-298. https://doi.org/10.1016/j.rgg.2018.03.007

Vancouver

Kontorovich AE, Ponomareva EV, Burshtein LM, Glinskikh VN, Kim NS, Kostyreva EA et al. Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia). Russian Geology and Geophysics. 2018 Mar 1;59(3):285-298. doi: 10.1016/j.rgg.2018.03.007

Author

Kontorovich, A. E. ; Ponomareva, E. V. ; Burshtein, L. M. et al. / Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia). In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 3. pp. 285-298.

BibTeX

@article{ec015031a538447aa1bf898b2b5326c5,
title = "Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia)",
abstract = "We studied the distribution of organic carbon in rocks of the Bazhenov horizon, a unique object of predominantly biogenic sedimentation in the West Siberian sedimentary basin. The contents of organic carbon in the rocks were determined using the data from 4094 core analyses and core-log relationships derived from 48,500 radioactive- and electrical-log measurements. For the Bazhenov and Tutleima Formations, both approaches gave the same results. The average content of organic carbon in the rocks is 7.7%. These data were used to compile a detailed map of the distribution of organic carbon contents in sedimentary rocks of the basin. It was shown that the average organic carbon content in the rocks increases from 2-4% on the periphery of the basin to 10-12% in its central, deepest part. The distribution of Corg values in the basin is highly asymmetric. The highest Corg values are observed in the southwestern part of the basin interior, where beds with > 10% Corg range in thickness from 5 to 12-15 m. In sections, the highest Corg values are observed in their middle and upper parts, composed predominantly of silicites and mixtites enriched in biogenic silica.",
keywords = "Bazhenov horizon, organic matter, West Siberia",
author = "Kontorovich, {A. E.} and Ponomareva, {E. V.} and Burshtein, {L. M.} and Glinskikh, {V. N.} and Kim, {N. S.} and Kostyreva, {E. A.} and Pavlova, {M. A.} and Rodchenko, {A. P.} and Yan, {P. A.}",
year = "2018",
month = mar,
day = "1",
doi = "10.1016/j.rgg.2018.03.007",
language = "English",
volume = "59",
pages = "285--298",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "3",

}

RIS

TY - JOUR

T1 - Distribution of organic matter in rocks of the Bazhenov horizon (West Siberia)

AU - Kontorovich, A. E.

AU - Ponomareva, E. V.

AU - Burshtein, L. M.

AU - Glinskikh, V. N.

AU - Kim, N. S.

AU - Kostyreva, E. A.

AU - Pavlova, M. A.

AU - Rodchenko, A. P.

AU - Yan, P. A.

PY - 2018/3/1

Y1 - 2018/3/1

N2 - We studied the distribution of organic carbon in rocks of the Bazhenov horizon, a unique object of predominantly biogenic sedimentation in the West Siberian sedimentary basin. The contents of organic carbon in the rocks were determined using the data from 4094 core analyses and core-log relationships derived from 48,500 radioactive- and electrical-log measurements. For the Bazhenov and Tutleima Formations, both approaches gave the same results. The average content of organic carbon in the rocks is 7.7%. These data were used to compile a detailed map of the distribution of organic carbon contents in sedimentary rocks of the basin. It was shown that the average organic carbon content in the rocks increases from 2-4% on the periphery of the basin to 10-12% in its central, deepest part. The distribution of Corg values in the basin is highly asymmetric. The highest Corg values are observed in the southwestern part of the basin interior, where beds with > 10% Corg range in thickness from 5 to 12-15 m. In sections, the highest Corg values are observed in their middle and upper parts, composed predominantly of silicites and mixtites enriched in biogenic silica.

AB - We studied the distribution of organic carbon in rocks of the Bazhenov horizon, a unique object of predominantly biogenic sedimentation in the West Siberian sedimentary basin. The contents of organic carbon in the rocks were determined using the data from 4094 core analyses and core-log relationships derived from 48,500 radioactive- and electrical-log measurements. For the Bazhenov and Tutleima Formations, both approaches gave the same results. The average content of organic carbon in the rocks is 7.7%. These data were used to compile a detailed map of the distribution of organic carbon contents in sedimentary rocks of the basin. It was shown that the average organic carbon content in the rocks increases from 2-4% on the periphery of the basin to 10-12% in its central, deepest part. The distribution of Corg values in the basin is highly asymmetric. The highest Corg values are observed in the southwestern part of the basin interior, where beds with > 10% Corg range in thickness from 5 to 12-15 m. In sections, the highest Corg values are observed in their middle and upper parts, composed predominantly of silicites and mixtites enriched in biogenic silica.

KW - Bazhenov horizon

KW - organic matter

KW - West Siberia

UR - http://www.scopus.com/inward/record.url?scp=85044002138&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.03.007

DO - 10.1016/j.rgg.2018.03.007

M3 - Article

AN - SCOPUS:85044002138

VL - 59

SP - 285

EP - 298

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3

ER -

ID: 12027878