| 大青山金矿床地质特征及成矿条件浅析 |
| |
| 引用本文： | 张国成.大青山金矿床地质特征及成矿条件浅析[J].地质找矿论丛,2003,18(Z1):84-87. |
| |
| 作者姓名： | 张国成 |
| |
| 作者单位： | 中国冶金地质勘查工程总局,西北地质勘查院,陕西,西安,710061 |
| |
| 摘 要： | 大青山金矿床位于北山古生代裂谷系,呈脉状、透镜状产于石炭系下统红柳园组下亚组含炭碎屑岩中,骆驼峰-大青山-险峰断裂带及其派生的断裂组为其提供了有利的导矿、容矿空间.矿化体中金的富集与石英脉的空间分布、矿石的结构构造、金属硫化物的含量、粒度有着密切的关系.
|
| 关 键 词： | 大青山金矿 地质特征 成矿条件 新疆 |
| 文章编号： | 1001-1412(2003)S0-0084-04 |
| 修稿时间： | 2003年10月12 |
THE ANALYSIS ON THE CHARACTER AND THE ORE-FORMING CONDITIONS OF GOLD DEPOSIT IN DAQINGSHAN |
| |
| ZHANG Guo-cheng.THE ANALYSIS ON THE CHARACTER AND THE ORE-FORMING CONDITIONS OF GOLD DEPOSIT IN DAQINGSHAN[J].Contributions to Geology and Mineral Resources Research,2003,18(Z1):84-87. |
| |
| Authors: | ZHANG Guo-cheng |
| |
| Abstract: | The gold deposit of Daqingshan lies in Paleozoic rift system of Beishan, occuring as vein and lefts at carbonceous elastic rock of Lower sub-formation of lower Carboniferous, and the fracture zone of the Luotuofeng-Daqingshan-Xianfeng and the related fracture are the ore-transportation and host space. The enrichment of the gold is closely related to the spatial distributon of the quartz vein, the fabric and structure of the ore, and the content and granularity of the metal sulfides. |
| |
| Keywords: | Daqingshan gold ore geologic character mineralization condition Xinjiang |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
