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Interseismic Slip and Coupling along the Haiyuan Fault Zone Constrained by InSAR and GPS Measurements

The Haiyuan fault zone is an important tectonic boundary and strong seismic activity belt in northeastern Tibet, but no major earthquake has occurred in the past ∼100 years, since the Haiyuan M8.5 event in 1920. The current state of strain accumulation and seismic potential along the fault zone have...

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Autors principals: Xin Qiao, Chunyan Qu, Xinjian Shan, Dezheng Zhao, Lian Liu
Format: Artigo
Idioma:Inglês
Publicat: MDPI AG 2021-08-01
Col·lecció:Remote Sensing
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Accés en línia:https://www.mdpi.com/2072-4292/13/16/3333
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