海南省后万岭铅锌矿矿床地质特征及找矿标志分析

The Prospecting Kriteria of Peripheral Houwanling Lead-zinc Deposit in Hainan

海南省后万岭铅锌矿位于五指山褶皱系边缘,产于千家超单元侵入体之中。矿体受南北向断裂构造控制,热液成矿痕迹明显,具产于中酸性侵入体的热液型铅锌矿地质特征。通过分析后万岭铅锌矿成矿地质特征,可选出矿床易于辨认矿化信息作为找矿标志。

Hou wan ling lead-zinc deposit is located in the edge of Wu zhi shan group fold system, produced on the late Cretaceous intermediate acidic intrusive rocks in Stage of Yanshan. The ore bodies are controlled by the North South faults, with obvious signs of hydrothermal mineralization and produced in the intermediate acid intrusive hydrothermal type lead-zinc ore deposit geological characteristics. Through the analysis of Huo wan ling lead-zinc deposit mineralization geological features which can be selected easily recognizable mineralization information as the prospecting marks.