Orogeny refers to the process of the lithospheric thickening on the convergent plate margins and formation of mountain belts. Its timing has long been disputed. Study of the deformation structures of the orogen indicates that thrusting is the main deforma
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张传恒 王自强.1997.论造山运动的时间特征[J].地质学报,71(1). Zhang Chuanheng, Wang Ziqiang, Jia Weimin.1997. ON TIMING OF OROGENY[J]. Acta Geologica Sinica,71(1).
