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Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise). / Parfenova, T. M.; Korovnikov, I. V.; Eder, V. G. et al.

In: Russian Geology and Geophysics, Vol. 58, No. 5, 01.05.2017, p. 586-599.

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

Harvard

Parfenova, TM, Korovnikov, IV, Eder, VG & Melenevskii, VN 2017, 'Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise)', Russian Geology and Geophysics, vol. 58, no. 5, pp. 586-599. https://doi.org/10.1016/j.rgg.2017.04.001

APA

Parfenova, T. M., Korovnikov, I. V., Eder, V. G., & Melenevskii, V. N. (2017). Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise). Russian Geology and Geophysics, 58(5), 586-599. https://doi.org/10.1016/j.rgg.2017.04.001

Vancouver

Parfenova TM, Korovnikov IV, Eder VG, Melenevskii VN. Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise). Russian Geology and Geophysics. 2017 May 1;58(5):586-599. doi: 10.1016/j.rgg.2017.04.001

Author

Parfenova, T. M. ; Korovnikov, I. V. ; Eder, V. G. et al. / Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise). In: Russian Geology and Geophysics. 2017 ; Vol. 58, No. 5. pp. 586-599.

BibTeX

@article{42110195df03444eb89b8c89a63cd40a,
title = "Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise)",
abstract = "We investigated organic matter (OM) of the Lower Cambrian Sinyaya Formation in the southeast of the Siberian Platform. The studied collection of rocks was divided into groups according to the contents of organic carbon, bitumens, and sulfur and lithologic characteristics. The content and distribution of saturated biomarkers were examined. Lanostanes C30, norlanostanes C29, 28,30-bisnorhopanes, and 2α- and 3β-methylhopanes have been identified in the bitumens. Relationships between the content of organic carbon and the distribution of hopanes, hopane ratios, and 2α-methylhopane index have been established. The conditions of sedimentation, diagenesis, and catagenesis of OM and the generation potential of the rocks have been estimated. It is shown that lanostanes, 28,30-bisnorhopanes, and methylhopanes can be used as biomarkers of the source rocks of the Sinyaya Formation and thus can help to determine the source of bitumens on the northern slope of the Aldan anteclise of the Siberian Platform.",
keywords = "biomarkers, bitumens, Lower Cambrian, organic geochemistry, Siberian Platform, source rocks, BIOMARKERS, MATTER, SIBERIAN-PLATFORM, PETROLEUM, HYDROCARBONS, SEDIMENTS",
author = "Parfenova, {T. M.} and Korovnikov, {I. V.} and Eder, {V. G.} and Melenevskii, {V. N.}",
year = "2017",
month = may,
day = "1",
doi = "10.1016/j.rgg.2017.04.001",
language = "English",
volume = "58",
pages = "586--599",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "5",

}

RIS

TY - JOUR

T1 - Organic geochemistry of the Lower Cambrian Sinyaya Formation (northern slope of the Aldan anteclise)

AU - Parfenova, T. M.

AU - Korovnikov, I. V.

AU - Eder, V. G.

AU - Melenevskii, V. N.

PY - 2017/5/1

Y1 - 2017/5/1

N2 - We investigated organic matter (OM) of the Lower Cambrian Sinyaya Formation in the southeast of the Siberian Platform. The studied collection of rocks was divided into groups according to the contents of organic carbon, bitumens, and sulfur and lithologic characteristics. The content and distribution of saturated biomarkers were examined. Lanostanes C30, norlanostanes C29, 28,30-bisnorhopanes, and 2α- and 3β-methylhopanes have been identified in the bitumens. Relationships between the content of organic carbon and the distribution of hopanes, hopane ratios, and 2α-methylhopane index have been established. The conditions of sedimentation, diagenesis, and catagenesis of OM and the generation potential of the rocks have been estimated. It is shown that lanostanes, 28,30-bisnorhopanes, and methylhopanes can be used as biomarkers of the source rocks of the Sinyaya Formation and thus can help to determine the source of bitumens on the northern slope of the Aldan anteclise of the Siberian Platform.

AB - We investigated organic matter (OM) of the Lower Cambrian Sinyaya Formation in the southeast of the Siberian Platform. The studied collection of rocks was divided into groups according to the contents of organic carbon, bitumens, and sulfur and lithologic characteristics. The content and distribution of saturated biomarkers were examined. Lanostanes C30, norlanostanes C29, 28,30-bisnorhopanes, and 2α- and 3β-methylhopanes have been identified in the bitumens. Relationships between the content of organic carbon and the distribution of hopanes, hopane ratios, and 2α-methylhopane index have been established. The conditions of sedimentation, diagenesis, and catagenesis of OM and the generation potential of the rocks have been estimated. It is shown that lanostanes, 28,30-bisnorhopanes, and methylhopanes can be used as biomarkers of the source rocks of the Sinyaya Formation and thus can help to determine the source of bitumens on the northern slope of the Aldan anteclise of the Siberian Platform.

KW - biomarkers

KW - bitumens

KW - Lower Cambrian

KW - organic geochemistry

KW - Siberian Platform

KW - source rocks

KW - BIOMARKERS

KW - MATTER

KW - SIBERIAN-PLATFORM

KW - PETROLEUM

KW - HYDROCARBONS

KW - SEDIMENTS

UR - http://www.scopus.com/inward/record.url?scp=85019231669&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2017.04.001

DO - 10.1016/j.rgg.2017.04.001

M3 - Article

AN - SCOPUS:85019231669

VL - 58

SP - 586

EP - 599

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 5

ER -

ID: 10191941