Results 241 to 250 of about 8,518,257 (285)
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Permian nonmarine bivalve zonation of the East European platform
Stratigraphy and Geological Correlation, 2014New finds and revision of available collections of nonmarine bivalves provided grounds for development of a zonal scale for terrestrial sequences of the Permian System based on species belonging to the genus Palaeomutela Amalitzky, 1891, which are characterized by regular changes in the structure of the shell hinge.
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The study of the asthenosphere of the East European platform by electromagnetic sounding
Physics of the Earth and Planetary Interiors, 1977Abstract A generalized curve of the apparent resistivity constructed from global and regional data leads us to suggest that the ancient shields of the East European Platform have no well-developed ...
L.L. Vanyan +3 more
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Deep structure of the southeastern part of the East European Platform
Geotectonics, 2014The results of CMP seismic data acquisition along regional deep profiles that cross large tectonic elements in the east of the East European Platform are considered. It has been established that the Zhiguli-Pugachev Arch and the Stavropol Depression (southern part of the Melekess Basin), as well as the Volga-Kama Anteclise and Pericaspian Syneclise ...
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Kimberlites and lamproites of the East European Platform: Petrology and geochemistry
Petrology, 2007Several episodes of kimberlite magmatism occurred in the East European Province (EEP) during a long (about 1.5 Gyr) time period, from the Late Paleoproterozoic (ca. 1.8 Ga) in the Archean Ukrainian and Baltic shields to the Middle Paleozoic (ca. 0.36 Ga) mainly in the Arkhangelsk, Timan, and adjacent regions.
O. A. Bogatikov +3 more
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The Influence of the Basement on the Formation of the Recent Structure of the East European Platform
Moscow University Geology Bulletin, 2019Structural–geomorphological studies of most of the territory of the East European Platform revealed an arch-block style of the recent dislocations. The 3D geodynamic modeling showed a direct correlation (K = 0.26) between the basement structures and the surface topography, indicating a direct geodynamic influence of the basement on the structure of the
L. V. Panina, V. A. Zaitsev
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Regional belts of uplifts and downwarpings on the East European Platform
International Geology Review, 1979(1979). Regional belts of uplifts and downwarpings on the East European Platform. International Geology Review: Vol. 21, No. 2, pp. 217-218.
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Late Precambrian and Early Cambrian in the East European platform
Precambrian Research, 1981Abstract In recent years the problem of the Cambrian—Precambrian boundary has again attracted the attention of a large number of geologists both in the U.S.S.R. and elsewhere. The study of regions with perfect outcrops of stratigraphically complete sections of Vendian—Cambrian deposits is of great importance for the solution of this question.
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Basement influence on formation of the East European platform latest structure
Moscow University Bulletin. Series 4. Geology, 2019Structural and geomorphological researches of the most part of the East European platform revealed arch-block style of the latest dislocations. 3D geodynamic modeling showed direct correlation (To =0, 26) of the basement structures with the modern relief surface that demonstrates direct geodynamic basement influence on the cover structure of the ...
L. V. Panina, V. A. Zaitsev
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Carboniferous bryozoans of the order Rhabdomesida of the East European Platform
Paleontological Journal, 2011This paper deals with the revision of Carboniferous bryozoans of the order Rhabdomesida from the East European Platform. Based on evolutionary and morphological analysis and on astogenetic method, the criteria of classification are refined and the taxonomic system of Carboniferous rhabdomesids of this region is studied in more detail.
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Riphean stromatolitic formations fringing the East European platform
Stratigraphy and Geological Correlation, 2007Riphean stromatolitic formations flank the East European epi-Karelian platform only in the east and northeast. They are traceable as long (over 3600 km) relatively narrow belt consisting of two rectilinear segments, one running along the Urals western flank from southern extremity of the Bashkirian meganticlinorium to the Polyudov Ridge and the other ...
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