摘要
汗牛铜镍铂族硫化物矿床产于康滇地轴断裂带上的基性岩体中。通过汗牛矿区成矿地质背景、含矿基性—超基性岩体的岩石地球化学特征及矿床成因的研究,探讨了汗牛地区铜镍铂族硫化物矿床的成因类型,分析了已有工作中的不足,结合优越的地质背景和良好的成矿地质条件,认为汗牛矿区具有良好的找矿前景。
Hanniu Cu-Ni-PEG sulfide deposit is located at basic rock mass in Kang-Dian earth＇ s axis fault zone. Through the analysis on metallogenic geological background of Hanniu ore district, lithogeochemical characteristics of basic-ultrabasic ore-bearing intrusion, and deposit genesis, the authors discuss the genesis types of Cu-Ni-PEG sulfide deposit in Hanniu, and its ore prospecting potential.
出处
《资源环境与工程》
2008年第6期565-568,共4页
Resources Environment & Engineering
关键词
铜镍铂族硫化物矿床
热液充填
四川汗牛
Cu-Ni-PGE sulfide deposits
hydrothermal filling
Hanniu in Sichuan
