| 湖南川口杨林坳钨矿床控矿因素与成矿规律研究 |
| |
| 引用本文： | 欧阳玉飞,黄满湘,郑平.湖南川口杨林坳钨矿床控矿因素与成矿规律研究[J].矿产与地质,2008,22(4):285-288. |
| |
| 作者姓名： | 欧阳玉飞 黄满湘 郑平 |
| |
| 作者单位： | 中南大学地学与环境工程学院,长沙,410083 |
| |
| 基金项目： | 中南大学横向科研项目 |
| |
| 摘 要： | 杨林坳钨矿是以白钨矿为主的岩浆期后高一中温热液充填交代矿床，白钨矿主要产于上古生界泥盆系杨林坳组砂岩和板溪群板岩中，受断裂构造和不整合面控制明显，岩浆活动为成矿提供了物质来源。文章在分析控矿因素的基础上，对成矿规律进行了探讨，并提出了下一步找矿预测的方向。
|
| 关 键 词： | 钨矿床 控矿因素 成矿规律 杨林坳 湖南 |
Research on the ore-controlling factors and ore-forming rules of the Yanglin'ao W deposit in Chuankou, Hunan |
| |
| OU YANG-Yufei,HUANG Man-xiang,ZHENG Ping.Research on the ore-controlling factors and ore-forming rules of the Yanglin''ao W deposit in Chuankou, Hunan[J].Mineral Resources and Geology,2008,22(4):285-288. |
| |
| Authors: | OU YANG-Yufei HUANG Man-xiang ZHENG Ping |
| |
| Institution: | (College of Geosciences and Environmental Engineering, Central South University, Changsha 410083, China) |
| |
| Abstract: | The Yanglin＇ao W deposit, most mineralization of which is seheelite,is a post magmatie deposit formed by high-middle temperature hydrothermal filling and metasomatism. The scheelite deposit mainly occurred in sandstones of the Yanglin＇ao Formation and slates of the Banxi Group in Devonian of Upper Paleozoic, which is obviously controlled by fault structures and unconformity surfaces with the ore-forming matters provided by magmatic movements. Based on analyzing ore-controlling factors, it has discussed the oreforming rules and put forward the predicting direction for further prospecting. |
| |
| Keywords: | W deposit ore-controlling factors ore-forming rules Yanglin＇ao Hunan |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
