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作 者:CHENG Yongsheng WANG Yong TAN Ruofa
机构地区:[1]Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring,Ministry of Education,Central South University,Changsha,Hunan 410083 [2]School of Geosciences and Info-Physics,Central South University,Changsha,Hunan 410083 [3]Hunan Shizhuyuan Nonferrous Metal Co.,Ltd.,Chenzhou,Hunan 423037
出 处:《Acta Geologica Sinica(English Edition)》2017年第S1期175-176,共2页地质学报(英文版)
基 金:granted by the National Natural Science Foundation of China (Grant Nos. 41202051 and 41672076);the Hunan Provincial Natural Science Outstanding Youth Foundation of China (Grant No. 2016JJ1022);the Open-End Fund for the Valuable and Precision Instruments of Central South University, China (Grant No. CSUZC201601);the Special Program of the Postdoctoral Science Foundation of China (Grant No. 2014T70886);China Postdoctoral Science Foundation (Grant No. 2012M521721)
摘 要:1 Introduction Both the Qiziqiao Formation and Shetianqiao Formation,which controls the occurrence and distribution of a great deal of metal mineral resources,are extensively developed in southern Hunan province(Liu et al.,1998),showing quite important indicative significance to deep concealed metal mineral resources(Yu et al.,2003).The geochemistry characteristics of Devonian strata could not affect the spatial occurrence shape of orebody
关 键 词:LI Trace Element Geochemistry of Devonian Strata in the Shizhuyuan Ore District Hunan Province REE ROCK
分 类 号:P534.44[天文地球—古生物学与地层学] P618.2[天文地球—地质学]
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