摘要
银洞金矿产于太古宇阜平群下亚群地层中，通过成矿地质特征、流体包裹体、氢氧同位素及微量元素研究分析，认为团泊口组及南营组为矿源层，成矿热液是以被加热的大气降水为主体的混合热液。
Yindong gold deposit is hosted in the lower levels of Fuping Group Archaeozoic stratum. According to the analysing of metallogenetic geological features, fluid inclusions, H and O isotopes, and microelements, it is considered that the ore source layer are in Tuanbokou and Nanying stratum, and the ore forming fluid is a mixed hydrothermal fluid dominated by heated meteoric water.
出处
《黄金地质》
1999年第1期30-36,共7页
Gold Geology
