Orogenic Gold Deposits:Mineralization Mechanism and Research Perspectives  

作　　者：Shao-Yong Jiang Ying Ma De-Liang Liu Wen-Tian Li 

机构地区：[1]State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Resources,Collaborative Innovation Center for Exploration of Strategic Mineral Resources,China University of Geosciences,Wuhan 430074,China

出　　处：《Journal of Earth Science》2023年第6期1758-1761,共4页地球科学学刊（英文版）

基　　金：financially supported by the National Natural Science Foundation of China(Nos.42321001,41973044);the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(No.MSFGPMR03-2).

摘　　要：0 INTRODUCTION Gold has been historically functioned as a strategic commodity,serving as a hard currency for international reserves,and increasingly plays a pivotal role in modern electronic communications,aerospace,and other high-tech industries.A range of geological processes (e.g.,magmatic activity,regional metamorphism,tectonic event) can result in formation of different types of gold deposits hosted in various through time.Based on tectonic background and genetic model,gold deposits can be classified into orogenic-,porphyry-,epithermal-,Carlin-,IOCG-(iron-oxide copper-gold)(IOCG),VMS-(volcanogenic massive sulfide),and SEDEX-(sedimentary exhalative) gold types (Kerrich et al.,2000).

关 键 词：MAGMATIC TECTONIC GOLD 

分 类 号：P618.51[天文地球—矿床学]