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Hydrocarbons occluded by asphaltenes. / Kashirtsev, V. A.

в: Russian Geology and Geophysics, Том 59, № 8, 01.08.2018, стр. 975-982.

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

Harvard

Kashirtsev, VA 2018, 'Hydrocarbons occluded by asphaltenes', Russian Geology and Geophysics, Том. 59, № 8, стр. 975-982. https://doi.org/10.1016/j.rgg.2018.07.017

APA

Kashirtsev, V. A. (2018). Hydrocarbons occluded by asphaltenes. Russian Geology and Geophysics, 59(8), 975-982. https://doi.org/10.1016/j.rgg.2018.07.017

Vancouver

Kashirtsev VA. Hydrocarbons occluded by asphaltenes. Russian Geology and Geophysics. 2018 авг. 1;59(8):975-982. doi: 10.1016/j.rgg.2018.07.017

Author

Kashirtsev, V. A. / Hydrocarbons occluded by asphaltenes. в: Russian Geology and Geophysics. 2018 ; Том 59, № 8. стр. 975-982.

BibTeX

@article{34da7d99bd8545a286920b86cf1c06de,
title = "Hydrocarbons occluded by asphaltenes",
abstract = "Homologous series of n-alkenes and dimethylalkanes with the odd or even number of carbon atoms in the molecule have been identified in chloroform extracts from the organic matter of Upper Paleozoic deposits of the Vilyui syneclise penetrated by the superdeep well SV-27 at depths below 5 km. It is presumed that these unusual hydrocarbons resulted from the destruction of asphaltene occlusions under severe P-T conditions at great depths and that the hydrocarbon generation began in the zone of postdiagenetic transformations of sediments. This hypothesis was tested in the sections of deposits whose organic matter underwent catagenesis of different grades. On the basis of these results, zones of emergence, transition, and destruction of occlusions have been recognized.",
keywords = "asphaltenes, bitumen, hydrocarbons, occlusion, OILS, PRODUCTS, ORGANIC-MATTER, FEATURES",
author = "Kashirtsev, {V. A.}",
year = "2018",
month = aug,
day = "1",
doi = "10.1016/j.rgg.2018.07.017",
language = "English",
volume = "59",
pages = "975--982",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "8",

}

RIS

TY - JOUR

T1 - Hydrocarbons occluded by asphaltenes

AU - Kashirtsev, V. A.

PY - 2018/8/1

Y1 - 2018/8/1

N2 - Homologous series of n-alkenes and dimethylalkanes with the odd or even number of carbon atoms in the molecule have been identified in chloroform extracts from the organic matter of Upper Paleozoic deposits of the Vilyui syneclise penetrated by the superdeep well SV-27 at depths below 5 km. It is presumed that these unusual hydrocarbons resulted from the destruction of asphaltene occlusions under severe P-T conditions at great depths and that the hydrocarbon generation began in the zone of postdiagenetic transformations of sediments. This hypothesis was tested in the sections of deposits whose organic matter underwent catagenesis of different grades. On the basis of these results, zones of emergence, transition, and destruction of occlusions have been recognized.

AB - Homologous series of n-alkenes and dimethylalkanes with the odd or even number of carbon atoms in the molecule have been identified in chloroform extracts from the organic matter of Upper Paleozoic deposits of the Vilyui syneclise penetrated by the superdeep well SV-27 at depths below 5 km. It is presumed that these unusual hydrocarbons resulted from the destruction of asphaltene occlusions under severe P-T conditions at great depths and that the hydrocarbon generation began in the zone of postdiagenetic transformations of sediments. This hypothesis was tested in the sections of deposits whose organic matter underwent catagenesis of different grades. On the basis of these results, zones of emergence, transition, and destruction of occlusions have been recognized.

KW - asphaltenes

KW - bitumen

KW - hydrocarbons

KW - occlusion

KW - OILS

KW - PRODUCTS

KW - ORGANIC-MATTER

KW - FEATURES

UR - http://www.scopus.com/inward/record.url?scp=85051086454&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.07.017

DO - 10.1016/j.rgg.2018.07.017

M3 - Article

AN - SCOPUS:85051086454

VL - 59

SP - 975

EP - 982

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 8

ER -

ID: 16112157