摘要
哥日卓托金铜矿位于布喀达坂峰-阿尼玛卿山华力西期钴(金、锑)成矿带上,成矿地质条件优越。但受自然条件的制约,哥日卓托金矿床发现较晚,且工作程度较低,找矿方向不明确。通过对成矿地质背景、矿床地质特征等资料综合研究,认为矿区主要发育与华力西期花岗闪长岩密切相关的矽卡岩型铜矿,以及与东西向构造作用密切相关的蚀变岩型金矿。为此,笔者依托近年来承担该矿床的矿床勘查工作取得的资料,通过矿床地质特征和成矿作用的总结,对矿区找矿前景和找矿方向进行探讨,以期对矿区矿产勘查工作有所裨益。
Gerizhuotuo gold-copper deposit is located at Variscan cobalt (gold, Antimony) meta- logenic belt of Buka Daba Mountain-Anyemaqen Mountains and has superior ore-forming geolog- ical conditions. But restricted by the natural condition, the Gerizhuotuo gold deposit has been found very late, its geological work degree is low and the prospecting direction is not clear. Based on the comprehensive analysis of the metallogenic geological background and the geological char- acteristics of this deposit, it's considered that skarn type copper deposit and alterd rock type gold deposit were mainly developed in this mining area, the former is closely related to the variscan di- orite while the later has close relationship with EW-trending tectonic process. Relying on the data obtained from the deposit exploration work in recent years, the metallogenic geological character- istics and mineralization have been sunnarized, the prospecting direction and potential have been discussed in this paper for benefiting the exploring work in this deposit.
出处
《西北地质》
CAS
CSCD
2016年第1期153-161,共9页
Northwestern Geology
基金
青海省都兰县哥日卓托地区金铜矿普查
关键词
金铜矿
成矿特征
找矿标志
哥日卓托
gold-copper deposit
geological characteristics, prospecting criteria, Gerizhuotuo