| 广东圆顶山金矿地质特征及前景 |
| |
| 引用本文： | 温永文. 广东圆顶山金矿地质特征及前景[J]. 黄金科学技术, 2005, 13(3): 21-24 |
| |
| 作者姓名： | 温永文 |
| |
| 作者单位： | 广东省地质勘查局719地质大队, 广东省 肇庆市 526020 |
| |
| 摘 要： | 圆顶山金矿属于桂东-粤西金矿带的一部分,区内寒武系浅变质岩系地层,其金含量较高,认为是金矿成矿的初始矿源层。矿区内EW向及NW向构造发育,所发现的主矿体均受控于NW向断裂,呈脉状或复脉状产于构造破碎带中,属破碎带变质热液含金石英脉型金矿。在综合研究矿区地质特征的基础上总结矿床成矿规律,指出找矿标志及目标。
|
| 关 键 词： | 金矿 矿床特征 找矿前景 广东 |
| 文章编号： | 1005-2518(2005)03-0021-04 |
| 收稿时间： | 2004-12-21 |
| 修稿时间： | 2004-12-21 |
The Geological Characteristic and the Prospect of Yuandingshan Golden Deposit,in Guangdong Province |
| |
| WEN Yongwen. The Geological Characteristic and the Prospect of Yuandingshan Golden Deposit,in Guangdong Province[J]. Gold Science and Technololgy, 2005, 13(3): 21-24 |
| |
| Authors: | WEN Yongwen |
| |
| Affiliation: | N o. 719 Geological Survey of Guangdong Province Geologic Exploration Bureau,Guangdong Zhaoqing 526020, China |
| |
| Abstract: | Yuandingshan golden deposit is a part of eastern Guangxi and western Guangdong gold belt. In region gold is rich in Cambrain system lower metamorphic rock series stratum which is regarded as original source bed. EW and NW structures develop in mining area. Main orebodies are controlled by NW faults that exist in the form of vein or compound vein in structural fracture zone, therefore this golden deposit is of metamorphic hydrothermal quartz vein golden deposit in fracture zone. On the base of synthetic research of geological characteristic, ore-forming rule is generalized, indicating prospecting marks and target. |
| |
| Keywords: | Guangdong Province Yuandingshan Golden Deposit Geological Characteristic and the Prospect |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《黄金科学技术》浏览原始摘要信息 |
|
点击此处可从《黄金科学技术》下载全文 |
