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In the Langshan region, northwestern China, marked multi‐stage intraplate deformation events have occurred since the Mesozoic, including (1) northeast‐striking ductile left‐lateral strike slip during the Middle‐Late Triassic, which is closely related to the collision between the North China and the Yangtze plates; (2) top‐to‐the‐southeast thrust with northwest‐southeast trending maximum compression...
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