| 四川阿加隆洼金矿床的地质特征及矿床成因 |
| |
| 引用本文： | 朱华平.四川阿加隆洼金矿床的地质特征及矿床成因[J].黄金,2007,28(6):18-20. |
| |
| 作者姓名： | 朱华平 |
| |
| 作者单位： | 成都地质矿产研究所 |
| |
| 基金项目： | 致谢：本研究的野外调查和室内资料整理过程中,得到成都地质矿产研究所范文玉、高大发、罗茂金、张林奎、高建华等同志大力支持及澳大利亚0xiana公司提供部分资料.在此深表感谢! |
| |
| 摘 要： | 甘孜-理塘断裂带是一发育在同名洋脊型火山岩-蛇绿岩带之上以金为主的成矿带,金矿化围岩以晚二叠-晚三叠世的火山-沉积岩系为主.阿加隆洼金矿床为产于成矿带中段的中型金矿床,矿床严格受断裂带控制,其容矿岩石主要为变碎屑岩和构造角砾岩,经综合分析,得出该矿床为构造蚀变岩型金矿床.
|
| 关 键 词： | 矿床成因 地质特征 甘孜-理塘断裂带 阿加隆洼金矿床 |
| 文章编号： | 1001-1277（2007）06-0018-03 |
| 修稿时间： | 2007-01-12 |
Geological characteristics and genesis of Ajialongwa gold deposit, Sichuan province |
| |
| Zhu Huaping.Geological characteristics and genesis of Ajialongwa gold deposit, Sichuan province[J].Gold,2007,28(6):18-20. |
| |
| Authors: | Zhu Huaping |
| |
| Affiliation: | Chengdu Institute of Geology and Mineral Resources |
| |
| Abstract: | Garze-Litang fault belt is an important gold metallogenic belt, which develops on the same name ocean ridge volcanic-ophiolite zone. The mineralization wall rock is mainly volcanic-sedimentary rock series in late Permianlate Triassic. Ajialongwa gold deposit lies in the middle section of the metallogenic belt, controlled by fault zone. The host rock is meta-clastic rock and breccia. According to comprehensive research, we conclude that the Ajialongwa deposit is structural-altered rock gold deposit. |
| |
| Keywords: | genesis of deposit geological characteristic Garze-Litang fault belt Ajialongwa goldd |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
