新疆青河县哈里恒金矿地质特征

详细信息

收稿日期: 2016-02-17

修回日期: 2016-03-17

刊出日期: 2016-12-31

GEOLOGICAL CHARACTERISTICS OF THE HALIHENG GOLD DEPOSIT IN QINGHE COUNTY, XINJIANG

Received Date: 17 February 2016

Revised Date: 17 March 2016

Publish Date: 31 December 2016

摘要: 哈里恒金矿处于东准噶尔华力西褶皱带，属于额尔齐斯金矿带的东段，断裂构造发育，区内发现3个土壤组合异常.在Ⅱ号异常内发现金矿体，已基本查明该矿为韧性剪切带型金矿.Ⅲ号异常面积大，Au异常分带性强，浓集中心明显，异常值高，与已知矿体具有相似的地质特征.
- 韧性剪切带型 /
- 金矿 /
- 找矿前景 /
- 土壤异常 /
- 哈里恒 /
- 新疆
Abstract: The Haliheng gold deposit is located in the Eastern Junggar Variscan fold belt, belonging to the eastern section of the Ertix gold belt, with developed fault structures. There are three soil assemblage anomalies in the area, among which gold deposit has been found in No. 2 anomaly and proved as ductile shear zone type. The No. 3 anomaly covers a large area, with high Au anomaly value, well zonation and obvious concentration center. The geological characteristics of the anomalies resemble those of the known orebodies, with a good prospecting potential.
- ductile shear zone type /
- gold deposit /
- prospecting potential /
- soil anomaly /
- Haliheng /
- Xinxiang