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Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea : the influence of tectonic and magmatic processes. / Petrova, V. I.; Batova, G. I.; Kursheva, A. V.; Litvinenko, I. V.; Morgunova, I. P.

в: Russian Geology and Geophysics, Том 58, № 3-4, 01.04.2017, стр. 322-331.

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

Harvard

Petrova, VI, Batova, GI, Kursheva, AV, Litvinenko, IV & Morgunova, IP 2017, 'Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea: the influence of tectonic and magmatic processes', Russian Geology and Geophysics, Том. 58, № 3-4, стр. 322-331. https://doi.org/10.1016/j.rgg.2016.09.008

APA

Petrova, V. I., Batova, G. I., Kursheva, A. V., Litvinenko, I. V., & Morgunova, I. P. (2017). Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea: the influence of tectonic and magmatic processes. Russian Geology and Geophysics, 58(3-4), 322-331. https://doi.org/10.1016/j.rgg.2016.09.008

Vancouver

Petrova VI, Batova GI, Kursheva AV, Litvinenko IV, Morgunova IP. Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea: the influence of tectonic and magmatic processes. Russian Geology and Geophysics. 2017 Апр. 1;58(3-4):322-331. https://doi.org/10.1016/j.rgg.2016.09.008

Author

Petrova, V. I. ; Batova, G. I. ; Kursheva, A. V. ; Litvinenko, I. V. ; Morgunova, I. P. / Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea : the influence of tectonic and magmatic processes. в: Russian Geology and Geophysics. 2017 ; Том 58, № 3-4. стр. 322-331.

BibTeX

@article{74cd73eb4d5c4b4599f50c5dff28a92d,
title = "Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea: the influence of tectonic and magmatic processes",
abstract = "Samples of Triassic sediments were collected from cores of parametric boreholes drilled on the Admiralteiskii Rise, Franz Josef Land Archipelago, and Fersman structure in the northeastern part of the Barents Sea sedimentary basin. The composition and distribution of hydrocarbon biomarkers (n-alkanes, isoprenoids, cyclic alkanes, and polyaromatic hydrocarbons) were studied using the GC-MS method and provided information about the genesis, facies conditions of sedimentation, and catagenetic maturity stage of dispersed organic matter (DOM). The Late Mesozoic-Cenozoic uplifting of the region and active magmatic processes significantly influenced the thermal transformation of sediments. The revealed trend is best observed in the sediment section of the Franz Josef Land Archipelago, where the thermal effects led to a radical increase in DOM transformation, up to the AC1 stage.",
keywords = "Arctic, Barents Sea, catagenesis, dispersed organic matter, hydrocarbon biomarkers, Triassic deposits",
author = "Petrova, {V. I.} and Batova, {G. I.} and Kursheva, {A. V.} and Litvinenko, {I. V.} and Morgunova, {I. P.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2016.09.008",
language = "English",
volume = "58",
pages = "322--331",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier",
number = "3-4",

}

RIS

TY - JOUR

T1 - Molecular geochemistry of organic matter of Triassic rocks in the northeastern part of the Barents Sea

T2 - the influence of tectonic and magmatic processes

AU - Petrova, V. I.

AU - Batova, G. I.

AU - Kursheva, A. V.

AU - Litvinenko, I. V.

AU - Morgunova, I. P.

PY - 2017/4/1

Y1 - 2017/4/1

N2 - Samples of Triassic sediments were collected from cores of parametric boreholes drilled on the Admiralteiskii Rise, Franz Josef Land Archipelago, and Fersman structure in the northeastern part of the Barents Sea sedimentary basin. The composition and distribution of hydrocarbon biomarkers (n-alkanes, isoprenoids, cyclic alkanes, and polyaromatic hydrocarbons) were studied using the GC-MS method and provided information about the genesis, facies conditions of sedimentation, and catagenetic maturity stage of dispersed organic matter (DOM). The Late Mesozoic-Cenozoic uplifting of the region and active magmatic processes significantly influenced the thermal transformation of sediments. The revealed trend is best observed in the sediment section of the Franz Josef Land Archipelago, where the thermal effects led to a radical increase in DOM transformation, up to the AC1 stage.

AB - Samples of Triassic sediments were collected from cores of parametric boreholes drilled on the Admiralteiskii Rise, Franz Josef Land Archipelago, and Fersman structure in the northeastern part of the Barents Sea sedimentary basin. The composition and distribution of hydrocarbon biomarkers (n-alkanes, isoprenoids, cyclic alkanes, and polyaromatic hydrocarbons) were studied using the GC-MS method and provided information about the genesis, facies conditions of sedimentation, and catagenetic maturity stage of dispersed organic matter (DOM). The Late Mesozoic-Cenozoic uplifting of the region and active magmatic processes significantly influenced the thermal transformation of sediments. The revealed trend is best observed in the sediment section of the Franz Josef Land Archipelago, where the thermal effects led to a radical increase in DOM transformation, up to the AC1 stage.

KW - Arctic

KW - Barents Sea

KW - catagenesis

KW - dispersed organic matter

KW - hydrocarbon biomarkers

KW - Triassic deposits

UR - http://www.scopus.com/inward/record.url?scp=85018525332&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.09.008

DO - 10.1016/j.rgg.2016.09.008

M3 - Article

AN - SCOPUS:85018525332

VL - 58

SP - 322

EP - 331

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3-4

ER -

ID: 9362222