摘要
得耳布尔银铅锌矿床位于额尔古纳成矿带得耳布尔干成矿亚带,产于陆相火山岩分布区,与次火山岩关系密切,矿体受断层控制。矿床成因类型为浅成低温热液型。断裂构造、热液蚀变、铁帽、物化探异常为重要的找矿标志。
The Deerbuer Ag--Pb--Zn deposit is located in Deerbuer ore--forming subelt that belongs to the Eerguna metallogenic belt, which is occurred in continental volcanic rock area, of which related to sub-volcanic rock, ore bodies are controlled by the fault. The genetic type of deposit belongs to shallow epithermal hydrothermal one. The faulted structure, hydrothermal alteration, gossan, geophysical--geochemical exploration anomalies are comprehensive ore--hunting indicators.
出处
《吉林地质》
2007年第3期18-21,共4页
Jilin Geology
关键词
银铅锌矿床
地质特征
找矿标志
得耳布尔
Ag--Pb--Zn deposit
geologic features
ore--hunting indicator
Deerbuer
