| 玉水铜多金属矿床地质特征及深部找矿浅析 |
| |
| 引用本文： | 陈文强. 玉水铜多金属矿床地质特征及深部找矿浅析[J]. 资源环境与工程, 2006, 20(6): 755-759 |
| |
| 作者姓名： | 陈文强 |
| |
| 作者单位： | 广东省梅州市玉水硫铜矿,广东,梅州,514743 |
| |
| 摘 要： | 玉水矿床为一以富铜为主的特富铜铅锌多金属矿床,产于壶天群灰岩与忠信组石英砂岩的接触界面上,矿体厚度大,品位高,矿物成分以黄铜矿、斑铜矿为主,具水平、垂直分带现象。其成因为海底的热液沉积矿床。根据-208中段F11断层对矿体的错动关系及相邻矿体的产状、形态及层控特征,提出-208 m中段东部可作为新的找矿地段,预计可获铅锌矿石量50 000~80 000 t。
|
| 关 键 词： | 玉水多金属矿床 矿化特征 F11断层 深部找矿 |
| 文章编号： | 1671-1211(2006)06-0755-05 |
| 收稿时间： | 2006-07-25 |
| 修稿时间： | 2006-08-28 |
Geology of Yushui copper polymetal deposit and the ore prospecting in deep ground |
| |
| CHEN Wen-qiang. Geology of Yushui copper polymetal deposit and the ore prospecting in deep ground[J]. Resources Environment & Engineering, 2006, 20(6): 755-759 |
| |
| Authors: | CHEN Wen-qiang |
| |
| Affiliation: | Yushui Copper Mine,Meizhou,Guangdong 514743 |
| |
| Abstract: | The Yushui deposit is a copper - rich lead - zinc polymetal deposit which lies between the Hutian limestone and Zhongxin quartz sandstone. The orebody is thick and of high tenor, with horizontal and vertical zonation. Its components are mainly chalcopyrite and bornite ,which are from hydrothermal sedimentation on the seafloor. The author considers that the east segment at -208m level will be the prospecting target, after analyzing the fault, distribution and shape of orebody. The lead - zinc ore may add 50 000 - 80 000 ton. |
| |
| Keywords: | Yushui polymetal deposit mineralization fault F_(11) ore prospecting in deep area |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
