Transition from oceanic to continental lithosphere subduction in southern Tibet: Evidence from the Late Cretaceous–Early Oligocene (~91–30Ma) intrusive rocks in the Chanang–Zedong area, southern Gangdese
Transition from oceanic to continental lithosphere subduction in southern Tibet: Evidence from the Late Cretaceous–Early Oligocene (~91–30Ma) intrusive rocks in the Chanang–Zedong area, southern Gangdese
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