Slip rate deficit partitioned by fault-fold system on the active Haiyuan fault zone, Northeastern Tibetan Plateau
Author:
Publisher
Elsevier BV
Subject
Geology
Reference48 articles.
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2. Low quaternary slip rate reconciles geodetic and geologic rates along the Altyn Tagh fault, northwestern Tibet;Cowgill;Geology,2009
3. Conjugate Riedel deformation band shear-zones;Davis;J. Struct. Geol.,2000
4. Variations in the geometry and amount of slip on the Haiyuan (Nanxihuashan) fault zone, China, and the surface rupture of the 1920 Haiyuan earthquake;Deng,1986
5. Tectonic development of the northeastern Tibetan Plateau as constrained by high-resolution deep seismic reflection data;Gao;Lithosphere,2013
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