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作 者:Qizhi Yang Tianyang Hu Youyue Lu Lei Liu Funian Huang Jianfeng Li Zunzun Zhang
机构地区:[1]State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China [2]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China [3]Mineral Resource Investigation of Hunan Province,Changsha 410100,China [4]Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring,Ministry of Education,School of Geosciences and Info-Physics,Central South University,Changsha 410083,China [5]Wuhan Centre of Geological Survey,China Geological Survey(Central South China Innovation Center for Geosciences),Wuhan430205,China [6]School of Geographical Sciences,Liaoning Normal University,Dalian 1160292,China
出 处:《Journal of Earth Science》2024年第5期1781-1785,共5页地球科学学刊(英文版)
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)。
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).
关 键 词:HUNAN METALLIC distinguished
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