Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin
A. N. Fomin
Кафедра геологии месторождений нефти и газа ГГФ
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.
Russian Geology and Geophysics
https://doi.org/10.1016/j.rgg.2016.09.020
Опубликовано - 1 апр 2017
10.1016/j.rgg.2016.09.020
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thermal maturity Науки об окружающей среде
sediments Физика и астрономия
Jurassic Науки об окружающей среде
catagenesis Науки об окружающей среде
grade Физика и астрономия
basin Науки об окружающей среде
sediment Науки об окружающей среде
vitrinite reflectance Науки об окружающей среде
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
Fomin, A. N. / Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. В: Russian Geology and Geophysics. 2017 ; Том 58, № 3-4. стр. 443-450.
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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.}",
doi = "10.1016/j.rgg.2016.09.020",
journal = "Russian Geology and Geophysics",
Fomin, AN 2017, 'Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin', Russian Geology and Geophysics, том. 58, № 3-4, стр. 443-450. https://doi.org/10.1016/j.rgg.2016.09.020
Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. / Fomin, A. N.
В: Russian Geology and Geophysics, Том 58, № 3-4, 01.04.2017, стр. 443-450.
T1 - Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin
AU - Fomin, A. N.
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
U2 - 10.1016/j.rgg.2016.09.020
DO - 10.1016/j.rgg.2016.09.020
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
Fomin AN. Thermal maturity of uppermost Middle Jurassic sediments in the West Siberian basin. Russian Geology and Geophysics. 2017 Апр. 1;58(3-4):443-450. https://doi.org/10.1016/j.rgg.2016.09.020