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Qidashan Fe Mine, Qianshan District, Anshan, Liaoning, Chinai
Regional Level Types
Qidashan Fe MineMine
Qianshan DistrictDistrict
AnshanPrefecture-level City
LiaoningProvince
ChinaCountry

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Latitude & Longitude (WGS84):
41° 9' 39'' North , 123° 6' 14'' East
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Anshan1,199,275 (2018)10.4km
Liaoyang687,890 (2014)13.6km
Jiupu123,843 (2018)16.6km
Gongchangling70,761 (2012)29.4km
Nantai56,478 (2012)36.4km
Mindat Locality ID:
143446
Long-form identifier:
mindat:1:2:143446:3
GUID (UUID V4):
0
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 Elements

Commodity 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 Diagram

Detailed Mineral List:

'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Bismuthinite
Formula: Bi2S3
'Chlorite Group'
'Columbite-(Fe)-Columbite-(Mn) Series'
Hematite
Formula: Fe2O3
Hematite var. Martite
Formula: Fe2O3
Magnetite
Formula: Fe2+Fe3+2O4
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Native Bismuth
Formula: Bi
Quartz
Formula: SiO2
'Tourmaline'
Formula: AD3G6(T6O18)(BO3)3X3Z
Uraninite
Formula: UO2
'Xenotime'
Zircon
Formula: Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Bismuth1.CA.05Bi
Group 2 - Sulphides and Sulfosalts
Bismuthinite2.DB.05Bi2S3
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Hematite4.CB.05Fe2O3
var. Martite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Uraninite4.DL.05UO2
Group 9 - Silicates
Zircon9.AD.30Zr(SiO4)
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(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

HHydrogen
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
H MuscoviteKAl2(AlSi3O10)(OH)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
BBoron
B TourmalineAD3G6(T6O18)(BO3)3X3Z
OOxygen
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
O HematiteFe2O3
O MagnetiteFe2+Fe23+O4
O Hematite var. MartiteFe2O3
O MuscoviteKAl2(AlSi3O10)(OH)2
O QuartzSiO2
O TourmalineAD3G6(T6O18)(BO3)3X3Z
O UraniniteUO2
O ZirconZr(SiO4)
O Columbite-(Fe)-Columbite-(Mn) Series
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
FFluorine
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgMagnesium
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlAluminium
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si ZirconZr(SiO4)
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
S BismuthiniteBi2S3
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
K MuscoviteKAl2(AlSi3O10)(OH)2
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
TiTitanium
Ti BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MnManganese
Mn Columbite-(Fe)-Columbite-(Mn) Series
FeIron
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fe HematiteFe2O3
Fe MagnetiteFe2+Fe23+O4
Fe Hematite var. MartiteFe2O3
Fe Columbite-(Fe)-Columbite-(Mn) Series
ZrZirconium
Zr ZirconZr(SiO4)
NbNiobium
Nb Columbite-(Fe)-Columbite-(Mn) Series
BiBismuth
Bi Native BismuthBi
Bi BismuthiniteBi2S3
UUranium
U UraniniteUO2

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian PlateTectonic Plate

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