Re-Os age report of pyrrhotite in the Dhi Samir amprophyre-type copper-nickel sulfide deposit in Yemen  

作　　者：Li-yan Zuo Rong-fu Pei Hui-feng Wang 

机构地区：[1]Development Research Center of China Geological Survey,Ministry of Natural Resources,Beijing 100037,China [2]Institute of Mineral Resources,Chinese Academy of Geological Sciences,China Geological Survey,Ministry of Natural Resources,Beijing 100037,China [3]Chinese Research Academy of Environmental Sciences,Beijing 100012,China

出　　处：《China Geology》2019年第2期238-239,共2页中国地质（英文）

摘　　要：1.Objectives The Dhi Samir copper-nickel sulfide deposit is located in the Taiz Province, South Yemen. The ore-bearing rock bodies occurred in the Neoproterozoic magmatic veins (Fig. 1). Different from most magmatic copper-nickel sulfide deposits, the Dhi Samir copper-nickel deposit is produced in the lamprophyre rather than in the mafic-ultramafic rocks such as peridotite, norite and gabbro.

关 键 词：Yemen DHI Samir amprophyre-type RE-OS 

分 类 号：P[天文地球]