摘要
哈拉郭勒金矿位于布尔汗布达山华力西一印支期钴、金、铜、玉石成矿带,为热液蚀变岩型金矿。金矿体呈脉状,分布于石炭系地层的控矿构造中,具有强烈的围岩蚀变。通过对该区金矿地质特征进行分析,对矿体成因进行初步的探讨。
Halaguole gold deposit is located in burhan budai mountains of the Variscan -Indosinian cobalt, gold, copper, jade metallogenic belt , it is hydrothermal altered rock type gold deposit. Gold orebodies are vein, In the ore controlling structure of carboniferous strata, with strong wall rock alteration. Based on the analysis of the geological features of the gold deposits in this area, the origin of the ore bodies is preliminarily discussed.
出处
《甘肃冶金》
2017年第1期56-59,共4页
Gansu Metallurgy
关键词
哈拉郭勒金矿
热液蚀变岩型金矿
围岩蚀变
成因探讨
Halaguole gold
hydrothermal altered rock type gold deposit
wall rock alteration
discussion on origin
