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Huxingshan W deposit, Linxiang Co., Yueyang, Hunan, Chinai
Regional Level Types
Huxingshan W depositDeposit
Linxiang Co.County
YueyangPrefecture-level City
HunanProvince
ChinaCountry

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Latitude & Longitude (WGS84):
29° 38' 44'' North , 113° 24' 28'' East
Latitude & Longitude (decimal):
29.64562,113.40781
GeoHash:
G#: wt28ssv43
GRN:
N20E71
Type:
Deposit
Köppen climate type:
Cfa : Humid subtropical climate
Nearest Settlements:
PlacePopulationDistance
Xindi175,761 (2015)19.8km
Yueyang1,200,000 (2018)42.7km
Puqi132,891 (2012)46.6km
Fengkou67,139 (2013)49.1km
Mindat Locality ID:
455751
Long-form identifier:
mindat:1:2:455751:0
GUID (UUID V4):
0


The exposed stratigraphy in this region comprises Neoproterozoic low-grade volcanoclastic-sedimentary rocks of the Lengjiaxi group and conglomerate of the Banxi groups, and Cambrian-Permian carbonate and siliciclastic sediments rocks. Huxingshan tungsten deposit contains resources of 206,500 metric tons of WO3 at an average grade of 0.3 %, representing the first large-scale tungsten deposit discovered in the northeastern Hunan Province. Recent field mapping has identified seven major vein-type orebodies (No. 1–7) in the Huxingshan deposit. They are primarily hosted within the fracture zone (F1) and the underlying Niutitang formation, within minor orebodies occurring in the Yijiaqiao formation. The No. 1 orebody hosted by the F1 fault is the largest, which contains more than 60 % of the W resource at Huxingshan. It extends along the F1 fault strike for over 2670 m, plunging from the surface to depths exceeding 700 m vertically. The No. 2–7 orebodies are parallel to the F1 fault but show shorter length compared to No. 1 orebody. Two stages of alteration and mineralization have been defined at the Huxingshan W deposit. The early-stage skarn alteration within the Niutitang formation carbonate rocks is limited exposed by current geological exploration, with no significant economic skarn-type W mineralization identified to date. The late-stage vein type mineralization is predominantly distributed in the F1 fracture zone and Niutitang formation (where it is either superimposed on carbonate rocks or crosscuts pre-existing barren skarn), only subordinately in the Yijiaqiao formation. These veins have variable widths ranging from 0.5 to 10 cm, with scheelite grains distributed in the veins and adjacent wall rocks, representing the orebodies in the Huxingshan deposit.

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


12 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

ⓘ Calcite
Formula: CaCO3
ⓘ 'Chlorite Group'
ⓘ Diopside
Formula: CaMgSi2O6
ⓘ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘ Fluorite
Formula: CaF2
ⓘ 'Monazite Group'
Formula: REE(PO4)
ⓘ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
ⓘ Pyrophyllite
Formula: Al2Si4O10(OH)2
ⓘ Quartz
Formula: SiO2
ⓘ Scheelite
Formula: Ca(WO4)
ⓘ Talc
Formula: Mg3Si4O10(OH)2
ⓘ Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2
ⓘ Wollastonite
Formula: Ca3(Si3O9)
ⓘ Zircon
Formula: Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 3 - Halides
ⓘFluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘScheelite7.GA.05Ca(WO4)
Group 9 - Silicates
ⓘZircon9.AD.30Zr(SiO4)
ⓘEpidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘDiopside9.DA.15CaMgSi2O6
ⓘTremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
ⓘWollastonite9.DG.05Ca3(Si3O9)
ⓘTalc9.EC.05Mg3Si4O10(OH)2
ⓘPyrophyllite9.EC.10Al2Si4O10(OH)2
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
ⓘ'Chlorite Group'-
ⓘ'Monazite Group'-REE(PO4)

List of minerals for each chemical element

HHydrogen
Hⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Hⓘ PyrophylliteAl2Si4O10(OH)2
Hⓘ TalcMg3Si4O10(OH)2
Hⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
CCarbon
Cⓘ CalciteCaCO3
OOxygen
Oⓘ CalciteCaCO3
Oⓘ DiopsideCaMgSi2O6
Oⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oⓘ Monazite GroupREE(PO4)
Oⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Oⓘ PyrophylliteAl2Si4O10(OH)2
Oⓘ QuartzSiO2
Oⓘ ScheeliteCa(WO4)
Oⓘ TalcMg3Si4O10(OH)2
Oⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Oⓘ WollastoniteCa3(Si3O9)
Oⓘ ZirconZr(SiO4)
FFluorine
Fⓘ FluoriteCaF2
MgMagnesium
Mgⓘ DiopsideCaMgSi2O6
Mgⓘ TalcMg3Si4O10(OH)2
Mgⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
AlAluminium
Alⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Alⓘ PyrophylliteAl2Si4O10(OH)2
SiSilicon
Siⓘ DiopsideCaMgSi2O6
Siⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Siⓘ PyrophylliteAl2Si4O10(OH)2
Siⓘ QuartzSiO2
Siⓘ TalcMg3Si4O10(OH)2
Siⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Siⓘ WollastoniteCa3(Si3O9)
Siⓘ ZirconZr(SiO4)
PPhosphorus
Pⓘ Monazite GroupREE(PO4)
KPotassium
Kⓘ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caⓘ CalciteCaCO3
Caⓘ DiopsideCaMgSi2O6
Caⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caⓘ FluoriteCaF2
Caⓘ ScheeliteCa(WO4)
Caⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Caⓘ WollastoniteCa3(Si3O9)
FeIron
Feⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ZrZirconium
Zrⓘ ZirconZr(SiO4)
WTungsten
Wⓘ ScheeliteCa(WO4)

Other Regions, Features and Areas containing this locality

AsiaContinent
China
Eurasian Plate
Yangtze PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

[1]Zhu, Lei; Li, Bin; Lu, An-Huai; Zhang, De-Xian (2025) Formation of the Huxingshan tungsten deposit by pulsed magmatic-hydrothermal fluids: Insights from scheelite mineral assemblage, texture, and trace elements. Ore Geology Reviews, 182. 106649 doi:10.1016/j.oregeorev.2025.106649
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