Formation Mechanism of Arcuate Tectonic Structures around Northeast Tibetan Plateau: Insight from 3‐D Numerical Modeling
Author:
Affiliation:
1. Key Laboratory of Computational Geodynamics College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China
Funder
National Natural Science Foundation of China
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12519
Reference37 articles.
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3. Three-dimensional thermal structure of subduction zones: effects of obliquity and curvature
4. Geology of the Haiyuan Fault Zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the Northeastern Margin of the Tibetan Plateau
5. Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir–Tien Shan transition zone for the Cretaceous and Palaeogene
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1. Geodynamics of progressive growth of arcuate fold-and-thrust belts: Insights from numerical modeling of the NE margin of the Qinghai-Tibetan plateau;Journal of Structural Geology;2023-10
2. Assessment of the relative tectonic activity of the Longxian–Baoji Fault Zone in the northeastern Tibetan Plateau based on geomorphic indices;Geosciences Journal;2023-08-24
3. Tectonic evolution of the Liupan Shan fold-and-thrust belt, NE Tibetan Plateau during the late Cenozoic: numerical simulations;Geophysical Journal International;2022-07-26
4. Introduction to the special issue “Tibetan tectonics and its effect on the long‐term evolution of climate, vegetation and environment”;Terra Nova;2022-03-04
5. Formation Mechanism of Arcuate Tectonic Structures around Northeast Tibetan Plateau: Insight from 3‐D Numerical Modeling;Terra Nova;2021-02-04
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