摘要
The Jiangshan-Shaoxing fault zone (JSFZ) was formed by the amalgamation of the Yangtze and Cathaysia blocks in the Neoproterozoic.Since the Paleozoic,the JSFZ has experienced three episodes of tectonic activities:the Early Paleozoic ductile strike-slip shear,Early Mesozoic thrust,and the Late Mesozoic extension.
The Jiangshan-Shaoxing fault zone (JSFZ) was formed by the amalgamation of the Yangtze and Cathaysia blocks in the Neoproterozoic.Since the Paleozoic,the JSFZ has experienced three episodes of tectonic activities:the Early Paleozoic ductile strike-slip shear,Early Mesozoic thrust,and the Late Mesozoic extension.
基金
funded by the National Science and Technology Major Project (2008ZX05005–001)
China Geological Survey Project (Grant No.1212011120160)