内蒙古大黄花地区铜多金属矿地质特征及找矿建议

详细信息

收稿日期: 2015-03-16

修回日期: 2015-04-22

刊出日期: 2015-12-31

GEOLOGICAL CHARACTERISTICS AND PROSPECTING SUGGESTION FOR THE COPPER POLYMETALLIC DEPOSIT IN DAHUANGHUA AREA IN INNER MONGOLIA

Received Date: 16 March 2015

Revised Date: 22 April 2015

Publish Date: 31 December 2015

摘要: 大黄花铜多金属矿区位于赤峰金银多金属成矿带南部，是在近年来开展1：5万数字化区域地质矿产调查野外工作中发现的.区内构造处于赤峰-开原深大断裂带中.含矿围岩主要为石炭系酒局子组地层，又叠加了中生代大规模的火山喷发作用及岩浆侵入活动，具有较好的成矿地质条件.
- 铜多金属矿 /
- 酒局子组 /
- 破碎带 /
- 大黄花地区 /
- 内蒙古
Abstract: The Dahuanghua Cu-polymetallic deposit, located in the south of Chifeng Au-Ag-polymetallic ore belt, is found during the 1:50 000 digital regional geological survey in recent years. The study area belongs to the Chifeng-Kaiyuan deep fracture zone. The ore bearing rock is the Carboniferous Jiujuzi Formation, superimposed by Mesozoic large-scale volcanic eruption and magmatic activities, which provide good geological conditions for metallogenesis.
- Dahuanghua Cu-polymetallic deposit /
- Jiujuzi Formation /
- fracture zone /
- Dahuanghua area /
- Inner Mongolia