西北地质2017，Vol.50Issue(3)：180-186,7.
青海夏日哈木铜镍矿床成矿特征及找矿研究
Reserch on Mineralization characters and Prospecting of the Xiarihamu Magematic Ni-Cu Sufide Deposit
摘要
Abstract
The Xiarihamu super-large nickel deposit is located in the middle part of the western segment of the East Kunlun orogenic belt.Submassive-massive,sideronitic and disseminated sulfide ores are dominant in the orebody.The former type is formed by deep liquating injected magmaalong the early-formed weak tectonic zone or fracture penetration.The latter two types are formed by liquation and fractional crystallization of mantle-derived magma,which are occurred in peridotite and pyroxenite.It is an effective way for prospecting prospect to understand mineralization enrichment regularity according to the diagenesis mineralization and ore-controlling factors.关键词
铜镍矿床/成矿特征/找矿/夏日哈木/青海省Key words
Cu-Ni deposit/metallogenic characteristics/prospecting/Xiarihamu/Qinghai province分类
天文与地球科学引用本文复制引用
杜玮,汤中立,杜玉良,姜常义,贾群子..青海夏日哈木铜镍矿床成矿特征及找矿研究[J].西北地质,2017,50(3):180-186,7.基金项目
国家自然科学基金项目(41302070,41102045)和中央高校基本科研业务费(2014G1271066,310827173401,310827172004)共同资助 （41302070,41102045）
