| 河南银洞坡金矿床特征及成因探讨 |
| |
| 引用本文： | 楚柏林,山正红.河南银洞坡金矿床特征及成因探讨[J].黄金地质,2000,6(1):32-37. |
| |
| 作者姓名： | 楚柏林 山正红 |
| |
| 作者单位： | 银洞坡金矿!河南桐柏474735 |
| |
| 摘 要： | 银洞坡金矿矿源层岩石建造为火山 -沉积建造 ,矿源层对矿床的形成及矿体的产状、形态、规模起到双重控制作用 ,金矿床具有层控矿床的特征。成矿热液来源是变质热液 ,矿质来源于矿源层 ,矿源层的成矿元素来源于地幔。矿床成因类型为层控火山 -沉积 -变质热液矿床。
|
| 关 键 词： | 金矿 矿床特征 矿床成因 河南 |
Discussion on the characteristics and genesis of Yindongpo gold deposit, Henan |
| |
| CHU Bai lin,SHAN Zheng hong,WANG Guang.Discussion on the characteristics and genesis of Yindongpo gold deposit, Henan[J].Gold Geology,2000,6(1):32-37. |
| |
| Authors: | CHU Bai lin SHAN Zheng hong WANG Guang |
| |
| Abstract: | The rock formation of the source bed in Yindongpo gold deposit is a volcano sedimentary formation. The formation of the deposit and the occurrence, size and morphology of the orebody are doublely controlled by the source bed. The gold deposit has the characteristic of stratabound.The source of the mineralizing solution is metamorphic hydrothermal solution. The mineral is from the source bed while the ore forming element of the source bed is from mantle. The type of the genesis is stratabound volcano sedimentary metamorphic hydrothermal deposit. |
| |
| Keywords: | gold deposit characteristic of the deposit genesis of the deposit Henan |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
