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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

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
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Publisher:
Elsevier Publisher's website
Journal:
Tectonophysics Journal website
Volume:
721
Pages:
28-44
Publication date:
2017-09-23
Acceptance date:
2017-09-19
DOI:
ISSN:
0040-1951
Source identifiers:
734422
Keywords:
Pubs id:
pubs:734422
UUID:
uuid:8d234804-fb1c-439e-a16d-1b3e2cc45c8b
Local pid:
pubs:734422
Deposit date:
2017-10-06

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