【摘 要】
：
The Qinling Orogenic Belt (QOB) was constructed by subduction and collision of the North China Craton (NCC) with South China Craton (Zhang et al.,2001).As an important part of the QOB,the southern mar
【机 构】
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School of Earth Sciences and Resources,China University of Geosciences Beijing,29 Xueyuan Road,Beiji
【出 处】
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The International Conference on Continental Dynamics(2014年大陆
论文部分内容阅读
The Qinling Orogenic Belt (QOB) was constructed by subduction and collision of the North China Craton (NCC) with South China Craton (Zhang et al.,2001).As an important part of the QOB,the southern margin of the NCC was involved in the Palaeozoic collisional orogen and the Mesozoic-Cenozoic intra-continental orogenic deformation (Zhang et al.,2001,Dong et al.,2011).The Taihua Group and Tietonggou Group define the amphibolite facies Archean- Paleoproterozoic basement complexes of the southern NCC (Zhang et al.,2001).The Taihua Group is mainly distributed in five regions:Xiaoqinling.
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