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Russian Geology and Geophysics

2017 year, number 3-4

THERMAL MATURITY OF UPPERMOST MIDDLE JURASSIC SEDIMENTS IN THE WEST SIBERIAN BASIN

A.N. Fomin1,2
1A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
Keywords: West Siberian basin, Jurassic sediments, organic matter, thermal maturity, catagenesis

Abstract

More than 1500 measurements of vitrinite reflectance ( R 0Vt), 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 MC21-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.