【摘 要】
：
As one of the most famous orogen of China,Qinling orogen has long been regarded as an important boundary dividing the North and South China.After two ophiolite mélange zones were recognized in the lat
【机 构】
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Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China
【出 处】
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The International Conference on Continental Dynamics(2014年大陆
论文部分内容阅读
As one of the most famous orogen of China,Qinling orogen has long been regarded as an important boundary dividing the North and South China.After two ophiolite mélange zones were recognized in the late 1970s (Li et al.,1978),which representing later identified the Early Palaeozoic Shangdan suture zone and the Late Palaeozoic Mianlue suture zone respectively (Zhang et al.,1995;Li et al.,1996;Meng et al.,1999),laid the foundation of modern tectonic framework of Qinling orogen.However,controversies about the Late Palaeozoic Mianlue ophiolite zone still remain so far.
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