Upper Crustal Collapse Reconstructed the Topography and Remodeled the Fault System of the Chuandian Fragment in the Southeastern Edge of the Tibetan Plateau, Evidenced by Anisotropy of Magnetic Susceptibility Data Sets-Reference-Cited by-同舟云学术

Upper Crustal Collapse Reconstructed the Topography and Remodeled the Fault System of the Chuandian Fragment in the Southeastern Edge of the Tibetan Plateau, Evidenced by Anisotropy of Magnetic Susceptibility Data Sets

Published:2022-04 Issue:4 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Tong Yabo¹²^ORCID,Yang Zhenyu²³^ORCID,Pei Junling¹²,Wang Heng⁴,Wu Zhonghai¹⁵^ORCID,Li Jianfeng¹

Affiliation:

1. Institute of Geomechanics Chinese Academy of Geological Sciences Beijing China

2. Key Laboratory of Paleomagnetism and Tectonic Reconstruction Ministry of Natural Resources Beijing China

3. College of Resources, Environment and Tourism Capital Normal University Beijing China

4. Institute of Geology China Earthquake Administration Beijing China

5. Key Laboratory of Neotectonic Movement and Geohazard Institute of Geomechanics Beijing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021TC007126

Reference75 articles.

1. Red River and associated faults, Yunnan Province, China: Quaternary geology, slip rates, and seismic hazard

2. Late Cenozoic right-lateral strike-slip faulting in southern Tibet

3. Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging

4. Magnetic fabrics may proxy as neotectonic stress trajectories, Polis rift, Cyprus

5. Tectonic applications of magnetic susceptibility and its anisotropy

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