摘要
金沙厂铅锌矿床的主要赋矿层为灯影组上统第二岩性段和寒武系下统梅树村组。矿体在空间分布上严格受到含矿建造的控制。本文通过对矿床地质特征及矿床成因进行论述,对下一步找矿方向进行了阐述。
The Jinshachang lead-zinc deposit is mainly hosted in 2nd lithologic member of Upper Sinian Dengying Formation and Lower Cambrian Meishucun Formation,and ore bodies are spatially strictly controlled by the ore-bearing formation.Based on a description of the geological characteristics and genesis of the ore deposit,this paper deals with the ore-prospecting orientations in further exploration work.
作者
荣惠锋
贺胜辉
徐恒
张贤峰
蒲利国
RONG Hui-feng;HE Sheng-hui;XU Heng;ZHANG Xian-feng;PU Li-guo(Institute of Geological,Geophysical and Geochemical Exploration,Yunnan Nonferrous Metals Geological Bureau,Kunming,Yunnan 650216)
出处
《地球学报》
CAS
CSCD
北大核心
2013年第S01期81-86,共6页
Acta Geoscientica Sinica
关键词
地质特征
金沙厂铅锌矿
云南
geological characteristics
hot brine
Jinshachang lead-zinc deposit
Yunnan
