Late Mesozoic topographic evolution of western Transbaikalia: Evidence for rapid geodynamic changes from the Mongol–Okhotsk collision to widespread rifting

Late Mesozoic topographic evolution of western Transbaikalia: Evidence for rapid geodynamic changes from the Mongol–Okhotsk collision to widespread rifting

The Mesozoic geodynamic evolution of Transbaikalia has been largely controlled by the scissors-like closure of the Mongol–Okhotsk Ocean that separated Siberia from Mongolia–North China continents. Following the oceanic closure, the tectonic evolution of that region was characterized by collisional u...

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Bibliographic Details
Main Authors: A.V. Arzhannikova, E.I. Demonterova, M. Jolivet, S.G. Arzhannikov, E.A. Mikheeva, A.V. Ivanov, V.B. Khubanov, L.A. Pavlova
Format: Article
Language:English
Published: Elsevier 2020-09-01
Series:Geoscience Frontiers
Subjects:
U–Pb detrital zircons dating
Topographic evolution
Mongol–Okhotsk collision
Transbaikalia
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987120300281

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http://www.sciencedirect.com/science/article/pii/S1674987120300281

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