摘要
云南石林天生关铅锌矿为沉积改造型矿床，矿体赋存于下石炭统大塘组，矿体主要受近NE60°～70°断裂及次级断裂构造控制，岩性控矿十分明显。
The ore bodies of Tianshengguan Pb-Zn Ore Deposit, Shilin, Yunnan, exist at the juncture parts between the lime rocks and dolomite rocks of the Datang Formation of the lower Carboniferous. The ore bodies are predominatively controlled by the 60°-70° NE-trending faults and the secondary faults. And it is also obvious that the rocks control the orebodies. The deposit is a sedimentary-reworked one.
出处
《矿业工程》
CAS
2006年第4期10-12,共3页
Mining Engineering
关键词
沉积矿床
铅锌矿床
地质特征
sedimentary deposit
Pb-Zn ore deposit eological characteristics
