青海省石头坑德铜镍矿成矿机理及找矿潜力和未来展望  

Metallogenic mechanism and prospecting potential of shitoukengde copper nickel deposit in Qinghai ProvinceAnd future prospects

作　　者：黄华良[1] 尹建华[1] HUANG Hua-liang;YIN Jian-hua(geological team of Sichuan Bureau of Geology and mineral exploration and development,Chongzhou 611230,China)

机构地区：[1]四川省地质矿产勘查开发局一0八地质队,四川崇州611230

出　　处：《世界有色金属》2021年第19期180-181,184,共3页World Nonferrous Metals

摘　　要：矿产资源是我国经济发展的重要物资保证,勘查矿产资源分布区域是顺利完成矿产资源开发的关键举措。本文将从青海省石头坑德铜镍勘查角度出发,分析岩浆熔离型铜镍硫化物矿床成矿机理,同时分析与概述找矿潜力和未来发展展望。Mineral resources are an important material guarantee for China's economic development.Exploring the distribution area of mineral resources is the key measure to successfully complete the development of mineral resources.From the perspective of shitoukeng de copper nickel exploration in Qinghai Province,this paper will analyze the metallogenic mechanism of magmatic detachment copper nickel sulfide deposit,analyze and summarize the prospecting potential and future development prospect.

关 键 词：岩浆熔离型矿床 铜镍矿 成矿机理 找矿措施 

分 类 号：P618.2[天文地球—矿床学]