The low-grade metamorphic rocks in southern DabieMt. refer to Susong and Zhangbaling Groups. The Susong Group is a sequence of the Yangtze passive continental sediments, which unconformably overlies the crystalline basement of the Yangtze craton-the Dabie complex. The Zhangbaling Group is documented to be the oceanic crust of ancient DabieOcean plate, which together with the shallow metamorphic rocks in northern DabieMountains fairly consists with the major tectonic elements of a subduction orogen.
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