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, “Hydrothermal evolution and ore genesis of the Beiya giant Au polymetallic deposit, western Yunnan, China: Evidence from fluid inclusions and HOSPb isotopes”, Ore Geology ReviewsOre Geology Reviews, vol. 90, pp. 847-862, 2017.
Compilation and indexing terms, Copyright 2018 Elsevier Inc.20165203171531Fluid inclusionHomogenization temperaturesHydrothermal activityHydrothermal fluidsIsotopic compositionPb isotopesSanjiang Tethyan metallogenic domainSkarn
