Qidashan Fe Mine, Qianshan District, Anshan, Liaoning, Chinai
| Regional Level Types | |
|---|---|
| Qidashan Fe Mine | Mine |
| Qianshan District | District |
| Anshan | Prefecture-level City |
| Liaoning | Province |
| China | Country |
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Latitude & Longitude (WGS84):
41° 9' 39'' North , 123° 6' 14'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Anshan | 1,199,275 (2018) | 10.4km |
| Liaoyang | 687,890 (2014) | 13.6km |
| Jiupu | 123,843 (2018) | 16.6km |
| Gongchangling | 70,761 (2012) | 29.4km |
| Nantai | 56,478 (2012) | 36.4km |
Name(s) in local language(s):
齐大山铁矿, 千山区, 鞍山市, 辽宁省, 中国
Algoma-type iron deposit, consisting of layered bodies concordant to their host rocks of chlorite schist, micaschist, phyllite and quartzite of the Anshan Group. The layers are up to 300 m thick and 15 km long.
The ore-hosting formation of the Qidashan iron deposit is the Yingtaoyuan Formation of the Neoarchean Anshan Group. The Yingtaoyuan Formation comprise mainly sericite-chlorite schist, mica quartzite, and chlorite schist. This formation experienced greenschist-phase metamorphism. The main body of the Qidashan iron deposit is a low-grade iron ore layer striking NW and dipping SW, with dip angles ranging from 75° to 90°, and the layer is approximately 5000 m in length and 170 to 250 m in thickness. The deposit also contains oxidized near-surface ore bodies dominated by hematite and primary magnetite at depth.
The Qidashan iron deposit has been mined since 1918, with proven iron ore reserves reaching 1.641 billion tons as of 2008. However, Li et al. first documented altered rock (including greisen and chlorite rock)-hosted Nb-Ta mineralization associated with high-grade iron ore within the deposit. Samples collected from this zone yielded an average Nb-Ta grade of 0.019%, indicating significant exploration potential. The outcrop strata in the Qidashan iron deposit mainly consist of the Yingtaoyuan Formation of the Neoarchean Anshan Group, the Langzishan Formation of the Lower Paleoproterozoic Liaohe Group, and the Quaternary. The iron ore bodies, including the low-grade banded iron formations (BIFs) and high-grade ore bodies, are all hosted in the Yingtaoyuan Formation. The Nb-Ta mineralization within the greisens and chlorites are characterized by columbite-group minerals (CGMs), which are spatially associated with high-grade iron ores. The geological–geochemical profile indicates that the greisens are all Nb-Ta-mineralized, which can be divided into greisen and tourmaline greisen based on their mineral compositions, and tourmaline unevenly aggregate in the central zone of the greisen in the profile.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
8 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 References: |
| ⓘ Bismuthinite Formula: Bi2S3 References: |
| ⓘ 'Chlorite Group' |
| ⓘ 'Columbite-(Fe)-Columbite-(Mn) Series' References: |
| ⓘ Hematite Formula: Fe2O3 References: |
| ⓘ Hematite var. Martite Formula: Fe2O3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 References: |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Bismuth Formula: Bi References: |
| ⓘ Quartz Formula: SiO2 References: |
| ⓘ 'Tourmaline' Formula: AD3G6(T6O18)(BO3)3X3Z References: |
| ⓘ Uraninite Formula: UO2 References: |
| ⓘ 'Xenotime' References: |
| ⓘ Zircon Formula: Zr(SiO4) References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Bismuth | 1.CA.05 | Bi |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | var. Martite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Uraninite | 4.DL.05 | UO2 |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Xenotime' | - | |
| ⓘ | 'Columbite-(Fe)-Columbite-(Mn) Series' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | Oxygen | |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Hematite var. Martite | Fe2O3 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Uraninite | UO2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Columbite-(Fe)-Columbite-(Mn) Series | |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Bismuthinite | Bi2S3 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mn | Manganese | |
| Mn | ⓘ Columbite-(Fe)-Columbite-(Mn) Series | |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Hematite var. Martite | Fe2O3 |
| Fe | ⓘ Columbite-(Fe)-Columbite-(Mn) Series | |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Nb | Niobium | |
| Nb | ⓘ Columbite-(Fe)-Columbite-(Mn) Series | |
| Bi | Bismuth | |
| Bi | ⓘ Native Bismuth | Bi |
| Bi | ⓘ Bismuthinite | Bi2S3 |
| U | Uranium | |
| U | ⓘ Uraninite | UO2 |
Other Regions, Features and Areas containing this locality
AsiaContinent
China
- North China OrogenOrogen
Eurasian PlateTectonic Plate
- North China Craton
- Longgang BlockShield
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References
[1]Jia, Sanshi; Fu, Jianfei; Leng, Wenfang; Cui, Shengnan; Zhao, Binbo; Meng, Jiaqi (2026) Identification and location of high-grade iron deposits in the Anshan-Benxi area, China, using integrated geophysical techniques. Ore Geology Reviews, 188. 107056 doi:10.1016/j.oregeorev.2025.107056
[2]Xiao, Yang; Gao, Rongzhen; Sun, Qing; Fu, Jianfei; Yao, Yuzeng; Jia, Sanshi; Chen, Jiale (2026) Geological Characteristics and Genesis of the Greisen-Hosted Nb-Ta Mineralization in the Qidashan Iron Deposit, Liaoning Province, China, and Its Implications. Minerals, 16 (3). doi:10.3390/min16030312