摘要
矿床位于华北地台北缘、白云鄂博裂谷带中,赋存于中元古界白云鄂博群地层中,属中低温热液矿床,受断裂破碎带控制。本文通过对矿床区域成矿地质背景、矿区及矿体地质特征研究,探讨了矿床成因及控矿因素。
The deposit is located in the northern margin of the North China Platform and Bayunebo rift belt,hosted in Proterozoic strata of the Bayunebo Group,which is in the low-temperature hydrothermal deposit,controlled by the fractured zone.Based on the deposits in the regional geological setting,mining and geological characteristics of ore body,explores the genesis and ore-controlling factors.
出处
《甘肃冶金》
2011年第2期89-91,103,共4页
Gansu Metallurgy
关键词
内蒙古太仆寺旗
金豆子山铅锌矿
地质特征
成因
Taipusi Banner in the Inner Mongolia
Jindouzishan lead-zinc deposit
geological characteristics
genesis
