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pro vyhledávání: '"E.E. Milanovsky"'
Autor:
E.E. Milanovsky
Publikováno v:
Episodes. 27:101-106
Autor:
L.A. Pevzner, S.L. Belyakov, V. G. Groshev, E.E. Milanovsky, V.I. Gorbachev, Leopold Lobkovsky, Sierd Cloetingh, Anco Lankreijer, Anatoly M. Nikishin, M.A. Korneev, P.A. Fokin, Y.A. Volozh
Publikováno v:
Default journal
Lobkovsky, L I, Cloetingh, S A P L, Nikishin, A, Volozh, Y A, Lankreijer, A C, Belyakov, S L, Groshev, V G, Fokin, P A, Milanovsky, E E, Pevzner, L A, Gorbachev, V I & Korneev, M A 1996, ' Extensional basins of the former Soviet Union: structure, basin formation mechanisms and subsidence history ', Default journal . https://doi.org/10.1016/S0040-1951(96)00193-X
Lobkovsky, L I, Cloetingh, S A P L, Nikishin, A, Volozh, Y A, Lankreijer, A C, Belyakov, S L, Groshev, V G, Fokin, P A, Milanovsky, E E, Pevzner, L A, Gorbachev, V I & Korneev, M A 1996, ' Extensional basins of the former Soviet Union: structure, basin formation mechanisms and subsidence history ', Default journal . https://doi.org/10.1016/S0040-1951(96)00193-X
We review the structure and evolution of a number of Riphean-Phanerozoic rifts and extensional basins within the territory of the former Soviet Union (FSU). Horst-and-graben formation in strong crustal and subcrustal lithosphere layers can explain th
Autor:
E.E. Milanovsky
Publikováno v:
Tectonophysics. 215:55-68
Aulacogens and aulacogeosynclinal zones represent intra-continental palaeorifts and inverted palaeorifts. They were formed in the process of the break-up of continents during the Late Proterozoic. Inversion of such basins occurred variably during the
Autor:
E.E. Milanovsky
Publikováno v:
Tectonophysics. 73:213-248
Riphean and Palaeozoic linear graben-like platform depressions — aulacogens —jointly with linear swell uplifts in a platform cover, intraplatform folded zones and Meso-Cenozoic epi-platform rift zones are different morphological manifestations of
Autor:
E.E. Milanovsky
Publikováno v:
Tectonophysics. 94:599-607
Linear extensional rift and rift-like structures have been generated many times during various periods of the Earth's history since early times. These structures have varied with time, however, in scale, morphology, formations, paragenesis of tectoni
Autor:
E.E. Milanovsky
Publikováno v:
Tectonophysics. 143:103-118
Rift and rift-like zones, global linear extensional structures of the crust, have appeared during most periods of the Earth's history. Rifting as a geological process has undergone a complex evolution, with its historical “roots” in the early Pre
Publikováno v:
Tectonophysics. 15:71-81
Numerous age determination: on volcanic rocks from the Gregory Rift make it possible to represent its structural and magmatic evolution in six chronological stages (in m.y.B.P.): 1. (1) 23-16; 2. (2) 13.5-12; 3. (3) 10-5; 4. (4) 5-2; 5. (5) 2-0.7; 6.
Autor:
E.E. Milanovsky
Publikováno v:
Tectonophysics. 15:65-70
The rift zones may be classified as oceanic, continental and intercontinental (e.g., the Red Sea and Gulf of Aden). Most of the rift zones are connected and form the world rift system. A notable exception is the Lake Baikal Rift. The Cenozoic contine
Publikováno v:
Tectonophysics. 143:IX