New Discovery of the Jinshui Tin Deposit in the Middle Section of the East Kunlun Orogenic Belt,Northwestern China:Mineralization Age and Exploration Significance  

作　　者：Xingkai Zhang Shao-Yong Jiang Hui-Min Su Wei Wang Qinglin Xia Yunpeng Liu Shien Li 

机构地区：[1]State Key Laboratory of Geological Processes and Mineral Resources,Collaborative Innovation Center for Exploration of Strategic Mineral Resources,School of Earth Resources,China University of Geosciences,Wuhan 430074,China [2]Third Geological Exploration Institute of Qinghai Nonferrous Geological and Mineral Exploration Bureau,Xining 810000,China

出　　处：《Journal of Earth Science》2024年第4期1373-1377,共5页地球科学学刊（英文版）

基　　金：financially supported by projects from the National Natural Science Foundation of China (Nos. 92162323, 42321001);the Qinghai Provincial Non-ferrous Metal Geological and Minerals Exploration Bureau (No.2023jgky01);the Kunlun Talents project of Qinghai Province (2023)

摘　　要：Tin,as one of the most important critical metals,has at-tracted great attention worldwide(Jiang et al.,2023,2020).China has the largest amount of tin resources in the world,ac-counting for nearly one-fourth of the world’s total(Jiang et al.,2020;Chen and Sheng,2015).Tin deposits in China mainly occur in the Nanling Range in southern China,the Sanjiang Basin in southwestern China,and the Great Xing’an Range in northeastern China,which account for 98%of the country’s tin resources,whereas tin deposits are relatively rare in north-western China(Ni et al.,2023;Chen et al.,2014,1992).

关 键 词：MIDDLE NORTHEASTERN SOUTHWESTERN 

分 类 号：P618.44[天文地球—矿床学]