Multistage exhumation and partial melting of high-T ultrahigh-pressure metamorphic rocks in continental subduction-collision zones

High-temperature （HT, 〉850℃） metamorphism in continental collision orogens, particularly for those ultrahigh-pressure （UHP） metamorphic rocks, has become one of the remarkable topics in Earth science. It has bearing on the element and isotope behaviors of UHP rocks, their partial melting and related...

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