| 铲子坪金矿北西向构造蚀变带特征及其研究意义 |
| |
| 引用本文： | 陈明扬.铲子坪金矿北西向构造蚀变带特征及其研究意义[J].湖南地质,1996,15(2):78-80. |
| |
| 作者姓名： | 陈明扬 |
| |
| 作者单位： | 中南工业大学地质系 |
| |
| 摘 要： | 铲子坪金矿区北西向构造蚀变带，在剖面上由中心硅化岩带向外依次为石英细脉带，硅化含砾砂板岩带，在性质上兼具韧性变形和脆性变形特征，反映了构造及热液流动的多次性。金矿化与早期灰白色奎化岩密切相关。
|
| 关 键 词： | 金矿床 构造蚀变带 矿化 |
Characteristics of Alteration Zone of NW Structure in Chanziping Gold Deposit and its Significance of Research |
| |
| Chen Mingyang.Characteristics of Alteration Zone of NW Structure in Chanziping Gold Deposit and its Significance of Research[J].Hunan Geology,1996,15(2):78-80. |
| |
| Authors: | Chen Mingyang |
| |
| Institution: | Department of Geology of Central South University of Technology |
| |
| Abstract: | NW structural belt of Chanziping gole deposit can be divided into three zones outwards. From the centre to each side they are: silicified rock zone, quarts veinlet sone and silicified pebble-bearing sand-slate zone. The NW structural belt is of deformation both flexible and fragile in nature. So this area has undergone many times of hydrothermal and structural activities. Mineralization relates closely to the grey-white silicified rock. |
| |
| Keywords: | Chanziping gold deposit NW structure |
| 本文献已被 CNKI 维普 等数据库收录！ |
