云南省会泽县金牛厂铅锌矿构造控矿特征及找矿方向

详细信息

收稿日期: 2016-06-01

修回日期: 2016-08-23

刊出日期: 2017-06-30

STRUCTURAL CONTROLLING CHARACTERISTICS AND PROSPECTING GUIDE OF THE JINNIUCHANG LEAD-ZINC DEPOSIT IN HUIZE COUNTY, YUNNAN PROVINCE

Received Date: 01 June 2016

Revised Date: 23 August 2016

Publish Date: 30 June 2017

摘要: 金牛厂铅锌矿区的铅锌矿体赋存于NWW向羽状断裂中.研究认为坪箐背斜是区域NW-SE向构造应力长期作用的结果，为矿区的主要控矿褶皱.NE向的关仓箐逆断层为矿区的导矿构造，NWW向次级张扭性断裂为矿区的主要容矿构造.矿区内矿体受构造控制明显，深部和边部具有良好的找矿前景.
- 构造控矿 /
- 金牛厂铅锌矿 /
- 找矿方向 /
- 会泽县 /
- 云南省
Abstract: The orebodies in the Jinniuchang Pb-Zn deposit occur in the NWW-trending plumose fractures. Study shows that the Pingqing anticline, which is the results of regional NW-SE structural stress, serves as the main ore-controlling structure. The NE-trending Guancangqing reverse fault is the passage-way for ore fluid. The secondary NWW-trending tenso-shearing fault is the main host structure. The orebodies are obviously controlled by structures in the orefield, therefore the deep and surrounding areas are prospective for ore-searching.
- structural controlling /
- Jinniuchang Pb-Zn deposit /
- ore-prospecting /
- Huize County /
- Yunnan Province