Tectonic map of the Vendian-Lower Paleozoic structural stage of the Lena-Tunguska petroleum province, Siberian Platform
A.E. Kontorovich a , S.Yu. Belyaeva, A.A. Kontorovich b , V.S. Starosel'tsev c , M.M. Mandel'baum d , A.V. Migurskii c , S.A. Moiseev a , A.F. Safronov e , V.S. Sitnikov f , Yu.A. Filiptsov g , A.V. Khomenko a , Yu.G. Eremin a , O.V. Bykova a
a Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the RAS, 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia
b Krasnoyarskgeofizika, 24v ul. Partizana Zheleznyaka, Krasnoyarsk, 660022, Russia
c Siberian Research Institute of Geology, Geophysics and Mineral Resources, 67 Krasnyi prosp., Novosibirsk, 630091, Russia
d Irkutskgeofizika, 8 ul. Gor'kogo, Irkutsk, 664025, Russia
e Institute of Oil and Gas Problems, Siberian Branch of the RAS, 1 ul. Oktyabrskaya, Yakutsk, 677891, Russia
f State Committee of the Sakha Republic (Yakutia) for Geology and Subsoil Resource Management, 13 ul. Kirova, Yakutsk, 677892, Russia
g Mineral Resources Management of Krasnoyarsk Territory, 62 ul. Marksa, Krasnoyarsk, 660049, Russia
Keywords: sedimentary cover; petroleum complex; structure map; classification; tectonic map; Siberian Platform
Pages: 649-659
Abstract
A new version of the tectonic map for the Vendian-Lower Paleozoic structural stage of the Lena-Tunguska petroleum province is presented. The map is based on the electronic structure map at a scale of 1:1,000,000, which was the first to be compiled for the uppermost Vendian within the study area. However, no tectonic zonation was made for the deep-buried Meso-Cenozoic Yenisei-Khatanga and Vilyui depressions. The principles and methodology of mapping are given. The study presents spatial, morphological, and quantitative characteristics of the major and large structures.
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