摘要
本文总结对比彝良毛坪与威宁云炉河坝地区铅锌矿床地质特征,并辅以成矿物质来源、成矿时代等证据基础上,认为区内铅锌矿成矿具典型的"逆冲断层运移—背斜翼部贯入成矿"特征,并据此分析云炉河坝铅锌矿区银厂沟—新营上深部位于唐家坪子背斜北西翼有利于含矿流体贯入成矿,而具较好找矿前景,为区内铅锌找矿提供了思路和依据。
The geological characteristics of Heba area in Maoping and Yunlu are summarized,on the basis of mineral source and metallogenic era,it＇s thought the areal lead-zinc deposit has typical features of ‘trust fault migration-anticlinal flanks injection ore-formation＇,it analysis that the up and deep Yinchanggou-Xinying of Heba lead-zinc deposit located in the northwest anticlinal flanks and it＇s better for injection ore-formation,it has good exploration prospective and affords idea and accordance for lead-zinc exploration in this area.
出处
《贵州地质》
2017年第3期160-168,共9页
Guizhou Geology
基金
贵州省地矿局“银厂坡-石门铅锌矿找矿研究”(课题编码201601-2)资助
关键词
找矿远景
逆冲断层运移—背斜翼部贯入成矿
铅锌矿床特征对比
彝良毛坪—威宁云炉河坝地区
滇黔边界
Exploration prospective
Trust fault migration-anticlinal flanks injection ore-formation
Leadzinc deposit characteristic compsrison
Heba area in Maoping of Yiliang and Yunlu of Weining
Boundary of Yunnan and Guizhou
