云南富源县哈播铅锌矿地质特征及控矿因素

THE GEOLOGICAL FEATURE AND ORE CONTROL FACTOR OF HABO PB-ZN DEPOSIT IN FUYUAN,YUNNAN

云南富源县哈播铅锌矿体呈似层状赋存于中二叠统阳新组(P2y)厚层、块状灰岩与白云岩之层间断裂裂隙带中;层间断裂裂隙构造是主要的控矿因素,中二叠统阳新组(P2y)不同岩性界面为次要的控矿条件。

Habo Pb-Zn ore body is stratoid in interbed fault fissure zone of Middle Permian Yangxin Formation （P2y） thick bedded, massive limestone and dolomitite. The interbed fault fissure structure is the main ore control factor. The interface of different rocks of Middle Permian Yangxin Formation （ P2y） is the secondary ore control condition.