Discovery and Significance of Layered Chromite Mineralization in Mafic-Ultramafic Rocks from the Gayahe Area of the East Kunlun Orogenic Belt,Northwestern China  

作　　者：Shao-Yong Jiang Hailin Xie Wenqi Ren Bin Wang Feng Yuan Xiufeng Liu Hui-Min Su 

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]Qinghai Engineering Research Center of Deep Exploration Technology for Large and Ultra-Large Gold Deposits around Qaidam Basin,First Geological Exploration Institute of Qinghai Province,Haidong 810600,China

出　　处：《Journal of Earth Science》2024年第4期1367-1372,共6页地球科学学刊（英文版）

基　　金：supported by projects from the Ministry of Science and Technology National Key R&D Pro-gram of China(No.2022YFC2903504);the National Natural Science Foundation of China(No.42321001);the Bureau of Geological Exploration&Development of Qinghai Province(No.2024-67);the Kunlun Talents Project of Qinghai Prov‐ince(2023).

摘　　要：0 INTRODUCTION Chromium(Cr)is one of the most important strategic critical metals in China.The primary chromite deposits can be divided into two types according to their geological setting and occurrences:podiform chromite and stratiform/layered chromite(Stowe,1994;Paktunc,1990).Podiform chromites mainly occur in ophiolites or mantle peridotites(Yang et al.,2022,2010;Bao et al.,1999).

关 键 词：China MANTLE SETTING 

分 类 号：P618.31[天文地球—矿床学] P618.33[天文地球—地质学]