摘要
对矿化蚀变带进行分析研究,矿床位于中-下石炭统接触裂隙破碎带中,总结成矿规律,建立找矿标志,为该区的地质找矿指明方向。
According to the analysis and study of metallogenesis alteration zone, the ore deposit is in the Mid- dle - Lower Carboniferous contact fracture zone, we have reduced, summarized the metallogenesis rule, set up the prospecting criteria and pointed out the direction for geological prospecting.
出处
《云南地质》
2010年第1期29-31,共3页
Yunnan Geology
关键词
中-下石炭统
构造破碎带
玉髓化-高岭土化
低温热液蚀变
云南孟连回林
Middle - Lower Carboniferous
Structural Fracture Zone
Calcedonization - Kaolinization
Low T Hydrothermal Alteration
Menglian, Yunnan
