Results 171 to 180 of about 5,190 (217)
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The Uralides and the Motion of the Russian and Siberian Platforms

Geological Society of America Bulletin, 1970
The Uralides—the late Precambrian and Paleozoic orogenic terrane between the Russian and Siberian Platforms—in part are exposed in the Ural Mountains, in the central Soviet Arctic, along the west edge of the Siberian Platform, and in southern Siberia and Kazakhstan, and in part are buried beneath the fill of the West Siberian Lowlands and other basins.
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The Trappean Complex of the Siberian Platform

2016
This chapter is devoted to a study of thermal effect of numerous dolerite intrusions of the Lower Triassic age presented widely in sedimentary basins of the East Siberia platform. The modeling of thermal regime and maturation history of sedimentary basin of the Siberian Platform is conducted on the examples of two sedimentary sections: the Kuyumba-12 ...
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Cupriferous Sandstones and Shales of the Siberian Platform

1986
The Siberian platform is host to a variety of mineral deposits, including stratiform copper deposits in sandstones and shales. Six major copper provinces are recognized (Prieniseyskaya, Prisajanskaya, Pribaikalskaya, Prialdanskaya, Priverkhojanskaya, Prianabarskaya), and within these at least 15 major zones of deposits and occurrences, including the ...
F. P. Krendelev   +7 more
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Oil and Gas Bearing Complexes of the Sedimentary Cover of the Arctic Zone of the Siberian Platform Marginal Zones of the North of the Siberian Platform?

SPE Russian Petroleum Technology Conference, 2019
Abstract The report discusses issues related to the assessment of the resource base and the development potential of the Arctic zone of the Siberian platform along the Northern sea route, the region of Russia with a high concentration of oil and gas resources.
Anatoly Dmitrievsky   +2 more
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BAUXITES OF PALEOZOIC BASEMENT OF WESTERN-SIBERIAN PLATFORM

Russian Geology and Geophysics, 1991
Bauxites which often occur on the Paleozoic basement surface are of rather a complex mineralogical composition. Diaspore, boehmite, siderite, kaolinite, crandallite and other minerals are identified in them. Their structural and textural characteristic are described. The laterite-sedimentary genesis of the rocks is concluded.
V.A. Bazhenov, I.A. Babanskaya
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Paleomagnetism of Vendian rocks in the southwest of the Siberian Platform

Russian Journal of Earth Sciences, 2006
[1] Presented in this paper are paleomagnetic data for the Vendian sedimentary rocks of the southwestern region of the Siberian Platform, obtained during the study of the reference rock sequences of the Central and Biryusa areas of the Sayan region and of the Yenisei mountain range in the lower reaches of the Angara River and its tributaries.
A. V. Shatsillo   +2 more
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New Material on the Ordovician Ostracodes of the Siberian Platform

Paleontological Journal, 2020
Twelve new species of Ordovician ostracodes are described from the sections on the Moyero, Angara and Nizhnyaya Chunku rivers. They belong to six previously described genera (Laccochilina, Kiesowia, Disulcina, Foramenella, Hallatina, and Pseudulrichia) and four new genera (Direigina, Korolyukina, Angarallina, and Tesakovites).
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Identification of Paleogene deposits in southern Siberian Platform

International Geology Review, 1967
Age of Paleogene deposits of flora and fauna in the southern Siberian Platform (Pg23 - Pg31), determined solely on the basis of palynological data was determined in 1962 in the sporepollen laboratory of the Irkutsk Geologic Board. These data indicate that at the time the sediments were formed the dominant vegetation consisted of typically subtropical ...
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Petroleum Potential of Baikit Anteclise, Siberian Platform

AAPG Bulletin, 1993
The Baikit Anteclise lies east of the Yenisei ridge, and it occupies an area of 155,000 km[sup 2] of the western part of the Siberian platform. The major structure of the anteclise outlined by seismic survey is the Kanovsky arch, complicated by three domal uplifts.
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Place of birth of the Siberian Platform

Doklady Earth Sciences, 2015
V. E. Pavlov, A. V. Shatsillo
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