摘要
0 INTRODUCTION Southern Hunan Province(SHP),positioned at the convergence of the Qin-Hang zone and the Nanling belt,is distinguished by its extensive Mesozoic magmatic activities and contemporaneous polymetallic deposits(Mao et al.,2021,2013;Ding et al.,2016).
基金
financially supported by the Open Fund of the China Geological Survey(Nos.DD20230342,DD20190154)
the National Natural Science Foundation of China(No.41972198)
the National Natural Science Foundation of Hunan Province(No.2022JJ30702)
the Research Center for Petrogenesis and Mineralization of Granitoid Rocks,the China Geological Survey(Nos.PM202308,PMGR202108)
the China Scholarship Council(No.CSC 202206370119)。
