摘要
嵩县和尚庵铅锌矿赋存于烧瓦窑断裂的次级构造蚀变破碎带内。矿体严格受北西西向断裂和北东东向次级断裂控制,熊耳期的岩浆侵入为矿物元素的活化提供动力,并提供了一部分物质来源。矿床成因属构造蚀变型。通过勘查,研究该区矿床成矿地质条件,探讨成因类型,为周边找矿指出方向。
Heshangan lead-zinc ore in Songxian exist in the second-order tectonic-alteration belt of Shaowayao fault. Ore body is strictly controlled by NWW, NEE second-order fractures. Magmatite in Xionger time also provides part of lead-zinc for the deposit in addition to the power of the mineral elementaries＇s activation. The genetic type of this deposit is tectonic-alteration-type lead-zinc deposit. Through perambulating and studing the geological characteristics and genesis of this deposit,we will find a way to look for ore more easy around here.
出处
《西部探矿工程》
CAS
2010年第9期116-118,121,共4页
West-China Exploration Engineering
关键词
铅锌矿
地质特征
成因
和尚庵
lead-zinc deposit
geological characteristics
genesis
Heshangan
