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Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin. / Ponomareva, E. V.; Burshtein, L. M.; Kontorovich, A. E. et al.

In: Doklady Earth Sciences, Vol. 481, No. 1, 01.07.2018, p. 918-921.

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

Harvard

Ponomareva, EV, Burshtein, LM, Kontorovich, AE & Kostyreva, EA 2018, 'Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin', Doklady Earth Sciences, vol. 481, no. 1, pp. 918-921. https://doi.org/10.1134/S1028334X18070176

APA

Ponomareva, E. V., Burshtein, L. M., Kontorovich, A. E., & Kostyreva, E. A. (2018). Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin. Doklady Earth Sciences, 481(1), 918-921. https://doi.org/10.1134/S1028334X18070176

Vancouver

Ponomareva EV, Burshtein LM, Kontorovich AE, Kostyreva EA. Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin. Doklady Earth Sciences. 2018 Jul 1;481(1):918-921. doi: 10.1134/S1028334X18070176

Author

Ponomareva, E. V. ; Burshtein, L. M. ; Kontorovich, A. E. et al. / Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin. In: Doklady Earth Sciences. 2018 ; Vol. 481, No. 1. pp. 918-921.

BibTeX

@article{1958aa01b5354c3e9dae1060ad7fce6d,
title = "Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin",
abstract = "The distribution of organic carbon in the Bazhenov horizon rocks of the western Siberian sedimentary basin is investigated. The organic carbon concentration in rocks is estimated by the results of core analyses (4094 core analyses) and by the calculations of the core-log data correlations (48 500 measurements) according to the data of radiation and electrical loggings. The average content of organic carbon in the rocks of the Bazhenov and Tutleim (lower subformation) formation is 7.7%. The map of organic carbon concentrations in the sedimentary rocks of the basin is constructed. In the basin, Corg is distributed asymmetrically. The region of maximum Corg concentrations occupies the southwestern part of the internal area of the sedimentary basin. Silicites and biogene silica-enriched mixtites are enriched with organic matter most of all.",
author = "Ponomareva, {E. V.} and Burshtein, {L. M.} and Kontorovich, {A. E.} and Kostyreva, {E. A.}",
year = "2018",
month = jul,
day = "1",
doi = "10.1134/S1028334X18070176",
language = "English",
volume = "481",
pages = "918--921",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Organic Carbon Distribution in the Bazhenov Horizon Rocks of the Western Siberian Megabasin

AU - Ponomareva, E. V.

AU - Burshtein, L. M.

AU - Kontorovich, A. E.

AU - Kostyreva, E. A.

PY - 2018/7/1

Y1 - 2018/7/1

N2 - The distribution of organic carbon in the Bazhenov horizon rocks of the western Siberian sedimentary basin is investigated. The organic carbon concentration in rocks is estimated by the results of core analyses (4094 core analyses) and by the calculations of the core-log data correlations (48 500 measurements) according to the data of radiation and electrical loggings. The average content of organic carbon in the rocks of the Bazhenov and Tutleim (lower subformation) formation is 7.7%. The map of organic carbon concentrations in the sedimentary rocks of the basin is constructed. In the basin, Corg is distributed asymmetrically. The region of maximum Corg concentrations occupies the southwestern part of the internal area of the sedimentary basin. Silicites and biogene silica-enriched mixtites are enriched with organic matter most of all.

AB - The distribution of organic carbon in the Bazhenov horizon rocks of the western Siberian sedimentary basin is investigated. The organic carbon concentration in rocks is estimated by the results of core analyses (4094 core analyses) and by the calculations of the core-log data correlations (48 500 measurements) according to the data of radiation and electrical loggings. The average content of organic carbon in the rocks of the Bazhenov and Tutleim (lower subformation) formation is 7.7%. The map of organic carbon concentrations in the sedimentary rocks of the basin is constructed. In the basin, Corg is distributed asymmetrically. The region of maximum Corg concentrations occupies the southwestern part of the internal area of the sedimentary basin. Silicites and biogene silica-enriched mixtites are enriched with organic matter most of all.

UR - http://www.scopus.com/inward/record.url?scp=85051211529&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18070176

DO - 10.1134/S1028334X18070176

M3 - Article

AN - SCOPUS:85051211529

VL - 481

SP - 918

EP - 921

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25472922