Episodes of Abnormally High Intensity of Tectonic Dislocations
- Authors: Golozubov V.V.1, Zheldak M.V.1, Kruk N.N.2, Kasatkin S.A.1
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Affiliations:
- Far East Geological Institute, Far East Branch, Russian Academy of Sciences
- Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
- Issue: Vol 13, No 1 (2019)
- Pages: 1-10
- Section: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211550
- DOI: https://doi.org/10.1134/S1819714019010020
- ID: 211550
Cite item
Abstract
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.
About the authors
V. V. Golozubov
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Author for correspondence.
Email: golozubov@fegi.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022
M. V. Zheldak
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: kruk@igm.nsc.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022
N. N. Kruk
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Author for correspondence.
Email: kruk@igm.nsc.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090
S. A. Kasatkin
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: kruk@igm.nsc.ru
Russian Federation, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022