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This is an early access version, the complete PDF, HTML, and XML versions will be available soon. Open AccessArticle by Shun Yang 1,*, Xin Han 2, Qiyun Lei 1, Peng Du 1, Chao Liu 1 and Zeshan Li 1 1 Earthquake Agency of Ningxia Hui Autonomous Region, Yinchuan 750001, China 2 Earthquake Agency of Gansu Province, Lanzhou 73000, China * Author to whom correspondence should be addressed. Appl. Sci.
Analysis of the locus, style, and rate of faulting is fundamental to understanding the kinematics of continental deformation. The Ordos Plateau lies to the northeast of Tibet, within the India-Eurasia collision zone. Previous studies have suggested that it behaves rigidly and rotates anticlockwise within a large-scale zone of ENE-WSW left-lateral shearing.
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