摘要
通过研究琼河坝地区的含矿岩系、铜金矿化、流体包裹体和氢氧同位素，认为２０２铜矿为斑岩型矿床，绿石沟铜矿为夕卡岩型矿床，剥蚀程度是本区铜金找矿的关键。
After studying ore-bearing rock series,Cu-Au Mineralization,fluid inclusion and H-O isotopes,it is believed that 202 Cu deposit is a porphyry one,and that Lushigou Cu deposit is a skarn.Then,it is pointed out that the key to prospecting Cu and Au in studied area is the depth of denudation.
出处
《地质与勘探》
CAS
CSCD
北大核心
1995年第1期26-31,共6页
Geology and Exploration
关键词
铜矿床
金矿床
矿化
地质特征
成因
Cu-Au mineralization,skarn,porphyry,the depth of denudation,Qiongheba
