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Origin of Middle Triassic high-K calc-alkaline granitoids and their potassic microgranular enclaves from the western Kunlun orogen, northwest China: A record of the closure of Paleo-Tethys

OrogenyEngineeringEast Asian StudiesPrecambrian GeologyNorthwest ChinaWestern Kunlun OrogenTectonic EvolutionEast Asian LanguagesLanguage StudiesGeochronologyPotassic Microgranular EnclavesTectonics