| 四川摩挲营地区某金矿成因浅析 |
| |
| 引用本文： | 徐彬.四川摩挲营地区某金矿成因浅析[J].四川地质学报,2014(1):39-43. |
| |
| 作者姓名： | 徐彬 |
| |
| 作者单位： | 四川省地矿局四○四队,四川 西昌615000 |
| |
| 摘 要： | 摩挲营地区处于扬子地台西缘康滇地轴北段,属南北向康滇构造岩浆带中的摩挲营花岗岩体南端突出部位。该区金矿主要产在摩挲营二长花岗岩(晋宁期侵入岩)的压扭性断裂中。成矿物质主要来源于元古界会理群天宝山组的海底火山沉积岩,成因类型属中温热液充填型金矿床。
|
| 关 键 词： | 金矿 矿体特征 成因类型 摩挲营 |
On Genesis of a Gold Deposit in Mosuoying,Sichuan |
| |
| XU Bin.On Genesis of a Gold Deposit in Mosuoying,Sichuan[J].Acta Geologica Sichuan,2014(1):39-43. |
| |
| Authors: | XU Bin |
| |
| Institution: | XU Bin (No. 404 Geological Team, BGEEMRSP, Xichang, Sichuan 615000) |
| |
| Abstract: | The Mosuoying lies in the northern section of the Kangdian axis. The gold deposit is confined to a compresso-shear fault in the Mosuoying monzogranite rockmass. Ore material was derived from submarine volcanic-sedimentary rock of the Tianbaoshan Formation of the Proterozoic Huili Group. The deposit is of mesothermal genesis. |
| |
| Keywords: | gold deposit geological feature genetic type Mosuoying |
| 本文献已被 CNKI 维普 等数据库收录！ |
