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Late Quaternary strike-slip along the Taohuala Shan-Ayouqi fault zone and its tectonic implications in the Hexi Corridor and the southern Gobi Alashan, China

Abstract:

The Hexi Corridor and the southern Gobi Alashan are composed of discontinuous a set of active faults with various strikes and slip motions that are located to the north of the northern Tibetan Plateau. Despite growing understanding of the geometry and kinematics of these active faults, the late Quaternary deformation pattern in the Hexi Corridor and the southern Gobi Alashan remains controversial. The active E-W trending Taohuala Shan-Ayouqi fault zone is located in the southern Gobi Alashan....

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.tecto.2017.09.014

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More from this funder
Name:
Chinese Academy of Sciences
Grant:
XDB03020201
More from this funder
Name:
Public Service Funds for Earthquake Studies
Grant:
201408023
More from this funder
Name:
National Science Foundation of China
Grant:
41372220, 41590861, 41661134011
Publisher:
Elsevier
Journal:
Tectonophysics More from this journal
Volume:
721
Pages:
28-44
Publication date:
2017-09-23
Acceptance date:
2017-09-19
DOI:
ISSN:
0040-1951
Keywords:
Pubs id:
pubs:734422
UUID:
uuid:8d234804-fb1c-439e-a16d-1b3e2cc45c8b
Local pid:
pubs:734422
Source identifiers:
734422
Deposit date:
2017-10-06

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