Standard

New monoaromatic steroids in organic matter of the apocatagenesis zone. / Kashirtsev, V. A.; Fomin, A. N.; Shevchenko, N. P. и др.

в: Doklady Earth Sciences, Том 469, № 2, 01.08.2016, стр. 815-818.

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

Harvard

Kashirtsev, VA, Fomin, AN, Shevchenko, NP & Dolzhenko, KV 2016, 'New monoaromatic steroids in organic matter of the apocatagenesis zone', Doklady Earth Sciences, Том. 469, № 2, стр. 815-818. https://doi.org/10.1134/S1028334X16080031

APA

Kashirtsev, V. A., Fomin, A. N., Shevchenko, N. P., & Dolzhenko, K. V. (2016). New monoaromatic steroids in organic matter of the apocatagenesis zone. Doklady Earth Sciences, 469(2), 815-818. https://doi.org/10.1134/S1028334X16080031

Vancouver

Kashirtsev VA, Fomin AN, Shevchenko NP, Dolzhenko KV. New monoaromatic steroids in organic matter of the apocatagenesis zone. Doklady Earth Sciences. 2016 авг. 1;469(2):815-818. doi: 10.1134/S1028334X16080031

Author

Kashirtsev, V. A. ; Fomin, A. N. ; Shevchenko, N. P. и др. / New monoaromatic steroids in organic matter of the apocatagenesis zone. в: Doklady Earth Sciences. 2016 ; Том 469, № 2. стр. 815-818.

BibTeX

@article{abd555ffe5d44b6b8b6d4e37819ffa68,
title = "New monoaromatic steroids in organic matter of the apocatagenesis zone",
abstract = "According to the materials of geochemical study in the core of the ultradeep hole SV-27 of aromatic fractions of bitumoids of the Vilyui syneclise (East Siberia) by the method of chromatography–mass spectrometry, starting from the depth of >5000 m, four diastereomers of previously unknown hydrocarbons, which become predominant in the fraction at a depth of ∼6500 m, were distinguished. Similar hydrocarbons were found in organic matter of Upper Paleozoic rocks of the Kharaulakh anticlinorium in the Verkhoyansk folded area. According to the intense molecular ion m/z 366 and the character of the basic fragmental ions (m/z 238, 309, and 323), the major structure of the compounds studied was determined as 17-desmethyl-23-methylmonoaromatic steroid C27. The absence of such steroids in oil of the Vilyui syneclise shows that deep micro-oils did not participate in the formation of oil fringes of gas condensate deposits of the region.",
author = "Kashirtsev, {V. A.} and Fomin, {A. N.} and Shevchenko, {N. P.} and Dolzhenko, {K. V.}",
year = "2016",
month = aug,
day = "1",
doi = "10.1134/S1028334X16080031",
language = "English",
volume = "469",
pages = "815--818",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - New monoaromatic steroids in organic matter of the apocatagenesis zone

AU - Kashirtsev, V. A.

AU - Fomin, A. N.

AU - Shevchenko, N. P.

AU - Dolzhenko, K. V.

PY - 2016/8/1

Y1 - 2016/8/1

N2 - According to the materials of geochemical study in the core of the ultradeep hole SV-27 of aromatic fractions of bitumoids of the Vilyui syneclise (East Siberia) by the method of chromatography–mass spectrometry, starting from the depth of >5000 m, four diastereomers of previously unknown hydrocarbons, which become predominant in the fraction at a depth of ∼6500 m, were distinguished. Similar hydrocarbons were found in organic matter of Upper Paleozoic rocks of the Kharaulakh anticlinorium in the Verkhoyansk folded area. According to the intense molecular ion m/z 366 and the character of the basic fragmental ions (m/z 238, 309, and 323), the major structure of the compounds studied was determined as 17-desmethyl-23-methylmonoaromatic steroid C27. The absence of such steroids in oil of the Vilyui syneclise shows that deep micro-oils did not participate in the formation of oil fringes of gas condensate deposits of the region.

AB - According to the materials of geochemical study in the core of the ultradeep hole SV-27 of aromatic fractions of bitumoids of the Vilyui syneclise (East Siberia) by the method of chromatography–mass spectrometry, starting from the depth of >5000 m, four diastereomers of previously unknown hydrocarbons, which become predominant in the fraction at a depth of ∼6500 m, were distinguished. Similar hydrocarbons were found in organic matter of Upper Paleozoic rocks of the Kharaulakh anticlinorium in the Verkhoyansk folded area. According to the intense molecular ion m/z 366 and the character of the basic fragmental ions (m/z 238, 309, and 323), the major structure of the compounds studied was determined as 17-desmethyl-23-methylmonoaromatic steroid C27. The absence of such steroids in oil of the Vilyui syneclise shows that deep micro-oils did not participate in the formation of oil fringes of gas condensate deposits of the region.

UR - http://www.scopus.com/inward/record.url?scp=84984918868&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16080031

DO - 10.1134/S1028334X16080031

M3 - Article

AN - SCOPUS:84984918868

VL - 469

SP - 815

EP - 818

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25766355