Mingyang Cu-Ni polymetallic deposit, Guazhou Co., Jiuquan, Gansu, Chinai
| Regional Level Types | |
|---|---|
| Mingyang Cu-Ni polymetallic deposit | Deposit |
| Guazhou Co. | County |
| Jiuquan | Prefecture-level City |
| Gansu | Province |
| China | Country |
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Latitude & Longitude (WGS84):
41° 6' 1'' North , 95° 15' 13'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
The regional stratigraphy, from oldest to newest, includes the Ordovician Huaniushan Group, Devonian Dundunshan Group, Carboniferous Hongliuyuan and Shibanshan Formations, Permian Shuangbaotang and Jinta Formations, and the Quaternary. The area features well-developed fault structures, predominantly nearly east–west and northeast trending, with the former being more prominent. These faults significantly influence regional stratigraphy, metamorphic deformation, and mineral distribution. Frequent magmatic intrusion activities occurred from the Ordovician to the Triassic, primarily forming bands or sheets. The lithology is complex, with outcrops ranging from ultrabasic to acidic rocks, predominantly intermediate-acidic types, which are closely linked to the genesis of various mineral types in the region.
Commodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Rock Types Recorded
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Alphabetical List Tree DiagramList of minerals for each chemical element
Other Regions, Features and Areas containing this locality
AsiaContinent
- Gobi DesertDesert
Eurasian PlateTectonic Plate
- Tian Shan
- South Tian ShanOrogenic Belt
- Tian Shan FoldbeltOrogenic Belt
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