摘要
通过介绍东昆仑夏日哈木铜镍硫化物矿床的发现,以及对矿床特征的初步研究,进一步阐明"小岩体成大矿"的地质事实及这一理论对勘查找矿工作的理论指导和实践意义。同时阐明该矿床的发现昭示区内该类型矿床具有巨大的成矿潜力,其对东昆仑地区寻找同类矿床具有重大指导意义。
Through introducing the discovery process of the Cu-Ni sulfide deposit in XiariHamu and stud- ying a preliminary exploration on characteristics of the deposit, this paper further expounds the geological theory of ＇small intrusions forming large deposits＇ , and the theoretical guidance and practical significance of exploration. Meanwhile, this paper elucidates that the new discovery of deposit shows this type of de- posits have enormous potential of mineralization, and makes great guiding significance for East K＇ un lun area to search and find similar deposits.
出处
《西北地质》
CAS
CSCD
2012年第4期185-191,共7页
Northwestern Geology
基金
青海省地勘基金项目"青海省东昆仑地区岩浆型铜镍硫化物矿床成矿环境及找矿潜力研究"(青国土资矿[2012]209号)
青海省地矿局勘查基金项目"青海省格尔木市夏日哈木铜多金属矿普查"(青地矿地[2012]18号)
关键词
小岩体成大矿
夏日哈木铜镍矿
找矿突破
启示及意义
small intrusions forming large deposits
Cu-Ni sulfide deposit
ore-search breakthrough
sig- nificance
