Email this article Change in the Geodynamic Settings in the Pacific‒Eurasia Transition Zone at the End of the Early Cretaceous
- Authors: Didenko A.N.1, Khanchuk A.I.2
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Affiliations:
- Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
- Far East Geological Institute, Far East Branch, Russian Academy of Sciences
- Issue: Vol 487, No 2 (2019)
- Pages: 873-876
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/195296
- DOI: https://doi.org/10.1134/S1028334X19080026
- ID: 195296
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Abstract
An attempt to provide a new explanation for the change in the geodynamic regime in the Early Cretaceous is presented below. It accounts for data on a number of global geodynamic characteristics in the range of 200–65 Ma reflecting processes both deep in the Earth and on the surface, and seemingly directly unrelated to the formation of a transform margin in Eastern Asia. It has been found that the geodynamic regime changed in the range of 115‒110 Ma.
About the authors
A. N. Didenko
Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences
Author for correspondence.
Email: itig@itig.as.khb.ru
Russian Federation, Khabarovsk, 680000
A. I. Khanchuk
Far East Geological Institute, Far East Branch, Russian Academy of Sciences
Email: itig@itig.as.khb.ru
Russian Federation, Vladivostok, 690022
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