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Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. / Fomin, A. N.

In: Russian Geology and Geophysics, Vol. 58, No. 3-4, 01.04.2017, p. 443-450.

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

Harvard

Fomin, AN 2017, 'Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin', Russian Geology and Geophysics, vol. 58, no. 3-4, pp. 443-450. https://doi.org/10.1016/j.rgg.2016.09.020

APA

Fomin, A. N. (2017). Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. Russian Geology and Geophysics, 58(3-4), 443-450. https://doi.org/10.1016/j.rgg.2016.09.020

Vancouver

Fomin AN. Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. Russian Geology and Geophysics. 2017 Apr 1;58(3-4):443-450. doi: 10.1016/j.rgg.2016.09.020

Author

Fomin, A. N. / Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. In: Russian Geology and Geophysics. 2017 ; Vol. 58, No. 3-4. pp. 443-450.

BibTeX

@article{d08930be0aa64f9184faf0a04c3f827e,
title = "Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin",
abstract = "More than 1500 measurements of vitrinite reflectance (R°t), along with mathematical modeling and computing, have been used to map the uppermost Middle Jurassic sediments of the West Siberian basin according to thermal maturity (catagenesis). The thermal maturity varies within the grades PC3 to AC2. Sediments are the least mature along the margins of the basin, and the maturity grade increases progressively toward its central and northern parts (grades MC1-MC2). It reaches a maximum in the north (AC2), where the sediments which subsided to large depths became exposed to high temperatures and pressures. The maturity zones of Jurassic sediments in the West Siberian basin form a typical pattern of regional catagenesis.",
keywords = "catagenesis, Jurassic sediments, organic matter, thermal maturity, West Siberian basin, CATAGENESIS",
author = "Fomin, {A. N.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2016.09.020",
language = "English",
volume = "58",
pages = "443--450",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "3-4",

}

RIS

TY - JOUR

T1 - Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin

AU - Fomin, A. N.

PY - 2017/4/1

Y1 - 2017/4/1

N2 - More than 1500 measurements of vitrinite reflectance (R°t), along with mathematical modeling and computing, have been used to map the uppermost Middle Jurassic sediments of the West Siberian basin according to thermal maturity (catagenesis). The thermal maturity varies within the grades PC3 to AC2. Sediments are the least mature along the margins of the basin, and the maturity grade increases progressively toward its central and northern parts (grades MC1-MC2). It reaches a maximum in the north (AC2), where the sediments which subsided to large depths became exposed to high temperatures and pressures. The maturity zones of Jurassic sediments in the West Siberian basin form a typical pattern of regional catagenesis.

AB - More than 1500 measurements of vitrinite reflectance (R°t), along with mathematical modeling and computing, have been used to map the uppermost Middle Jurassic sediments of the West Siberian basin according to thermal maturity (catagenesis). The thermal maturity varies within the grades PC3 to AC2. Sediments are the least mature along the margins of the basin, and the maturity grade increases progressively toward its central and northern parts (grades MC1-MC2). It reaches a maximum in the north (AC2), where the sediments which subsided to large depths became exposed to high temperatures and pressures. The maturity zones of Jurassic sediments in the West Siberian basin form a typical pattern of regional catagenesis.

KW - catagenesis

KW - Jurassic sediments

KW - organic matter

KW - thermal maturity

KW - West Siberian basin

KW - CATAGENESIS

UR - http://www.scopus.com/inward/record.url?scp=85018496672&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.09.020

DO - 10.1016/j.rgg.2016.09.020

M3 - Article

AN - SCOPUS:85018496672

VL - 58

SP - 443

EP - 450

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3-4

ER -

ID: 10036075