Episodes of Abnormally High Intensity of Tectonic Dislocations


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Resumo

It is shown for the structures of the Late Permian–Early Triassic, Early–Late Cretaceous, and Early–Middle Miocene stages in the formation of the eastern margin of Asia that the evolution of the Earth’s crust included periods of tectonic reconstructions, which occurred practically instantaneously from the geological viewpoint. These periods are often shorter than the resolution of both local isotope and paleontological methods of dating.

Sobre autores

V. Golozubov

Far East Geological Institute, Far East Branch, Russian Academy of Sciences

Autor responsável pela correspondência
Email: golozubov@fegi.ru
Rússia, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022

M. Zheldak

Far East Geological Institute, Far East Branch, Russian Academy of Sciences

Email: kruk@igm.nsc.ru
Rússia, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022

N. Kruk

Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

Autor responsável pela correspondência
Email: kruk@igm.nsc.ru
Rússia, pr. Akademika Koptyuga 3, Novosibirsk, 630090

S. Kasatkin

Far East Geological Institute, Far East Branch, Russian Academy of Sciences

Email: kruk@igm.nsc.ru
Rússia, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022


Declaração de direitos autorais © Pleiades Publishing, Ltd., 2019

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