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Geochemistry of organic matter of the Neoproterozoic strata within the Berezovka depression (Seralakh Formation,Siberian Platform)
Institution:1. A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia;2. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia;3. M.V. Lomonosov Moscow State University, Leninskiye Gory, Moscow, 119991, Russia;4. Geological Survey of Western Australia, 100 Plain Str., East Perth, WA 6004, Australia;5. A.P. Karpinsky Russian Geological Research Institute, Srednii pr. 74, Saint Petersburg, 199106, Russia;1. I.S. Gramberg All-Russia Scientific Research Institute for Geology and Mineral Resources of the Ocean (VNIIOkeangeologia), Angliiskii pr. 1, St. Petersburg, 190121, Russia;2. Tallinn Teckhnological University, 5, ul. Ehitayaatee, Tallinn, 19086, Estonia;3. M.V. Lomonosov Moscow State University, Leninskie Gory, Moscow, 119991, Russia;4. Earth Cryosphere Institute, Siberian Branch of the Russian Academy of Sciences, ul. Malygina 86, P/O box 1230, Tyumen, 625000, Russia;5. Central Laboratory for Mining and Geology, ul. Markova 35, Syktyvkar, 167004, Russia;6. St. Petersburg State University, Universitetskaya nab. 7/9, St. Petersburg, 199034, Russia;1. Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia;2. Department of Geological Sciences, Stockholm University, Svante Arrhenius vag 8, SE-106 91 Stockholm, Sweden;3. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, ul. Kosygina 19, Moscow, 119991, Russia;1. V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences, ul. Baltiiskaya 43, Vladivostok, 690041, Russia;2. School of Natural Sciences, Far Eastern Federal University, ul. Sukhanova 8, Vladivostok, 690950, Russia;3. Mining Institute, Far Eastern Branch of the Russian Academy of Sciences, ul. Turgeneva 51, Khabarovsk, 680000, Russia;1. VIRG-Rudgeofizika, Petrovskaya Kosa 1, St. Petersburg, 197110, Russia;2. St. Petersburg State University, Universitetskaya naberezhnaya 7/9, St. Petersburg, 199034, Russia
Abstract:The results of study of geochemistry of the Neoproterozoic and Lower Cambrian deposits within the Berezovka depression are presented. A mudstone member of the Seralakh Formation is assumed to be an oil source bed. We compiled a series of geochemical maps for this formation and estimated the hydrocarbon generation potential and the scales of oil and gas formation in its mudstone member, using the volumetric-genetic method. The migrated liquid hydrocarbons amount to about 8 billion tons.
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