| 太行山中段银洞金矿成矿条件探讨 |
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| 引用本文： | 耿洪,崔文亚.太行山中段银洞金矿成矿条件探讨[J].黄金地质,1999,5(1):30-36. |
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| 作者姓名： | 耿洪 崔文亚 |
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| 作者单位： | 黄金第八支队 |
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| 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、氢氧同位素及生量元素研究分析，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。
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| 关 键 词： | 地质特征 河北 金矿床 成矿条件 |
DISCUSSION ON MINERALIZING CONDITION OF YINDONG GOLD DEPOSIT IN THE CENTRAL SECTION OF TAIHANG MOUNTAIN |
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| Geng Hong,Cui Wenya,Zhao Zhilong.DISCUSSION ON MINERALIZING CONDITION OF YINDONG GOLD DEPOSIT IN THE CENTRAL SECTION OF TAIHANG MOUNTAIN[J].Gold Geology,1999,5(1):30-36. |
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| Authors: | Geng Hong Cui Wenya Zhao Zhilong |
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| Abstract: | 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. |
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| Keywords: | gold deposit geological feature Hebei |
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