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Objective The Bayingou ophiolitic melange is located in Northern Tianshan Mountains of the southern Central Asian Orogenic Belt which is the largest accretionary orogen among the European,Siberian,Tarim and North China cratons.The Bayingou ophiolitic melange provide a critical geological record for unraveling regional tectonic history
Objective The Bayingou ophiolitic melange is located in Northern Tianshan Mountains of the southern Central Asian Orogenic Belt which is the largest accretionary orogen among the European, Siberian, Tarim and North China cratons. Bayingou ophiolitic melange provide a critical geological record for unraveling regional tectonic history