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- W2016165298 abstract "Abstract The tectonic map of the east of Asia, scale 1:2,500,000, has been compiled at the Geological Institute of the U.S.S.R. Academy of Sciences, Moscow, and the Northeast Complex Research Institute, Magadan U.S.S.R. The tectonic zoning of the continental block was determined according to the time of formation of the stable continental crust. Accordingly, the following epochs of the continental crust formation are distinguished: pre-Riphean, Late Paleozoic, Late Mesozoic, and Late Cretaceous—Paleogene. The tectonic zoning of those areas where the earth's crust is of the continental type that is being formed now was determined according to the time of appearance of a granite-metamorphic layer. Five epochs of formation of such a layer can be singled out: Lower Carboniferous, Albian—Cenomanian, Senonian, Paleogene, Neogene. The analysis of the map shows that in eastern Asia the active continental margins existed at least since the Early Paleozoic. Along with the processes of growth of the continental crust the phenomena of tectonic destruction took place along the continental margins of the same zones. The structural evolution of the near-oceanic mobile zone, and formation, in its place, of areas with the continental type crust is the essence of geosynclinal development of the active continental margin." @default.
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- W2016165298 date "1980-12-01" @default.
- W2016165298 modified "2023-09-23" @default.
- W2016165298 title "Active continental margins of the Northwest Pacific" @default.
- W2016165298 doi "https://doi.org/10.1016/0040-1951(80)90018-9" @default.
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