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Huayangchuan U-Nb-Pb deposit, Huayin City, Weinan, Shaanxi, Chinai
| Regional Level Types | |
|---|---|
| Huayangchuan U-Nb-Pb deposit | Deposit |
| Huayin City | County |
| Weinan | Prefecture |
| Shaanxi | Province |
| China | Country |
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Latitude & Longitude (WGS84):
34° 27' 29'' North , 110° 4' 59'' East
Latitude & Longitude (decimal):
Type:
Kรถppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Huayin | 242,488 (2016) | 12.0km |
Name(s) in local language(s):
ๅ้ณๅท้้้
็ฟๅบ, ๅ้ดๅธ, ๆธญๅๅธ, ้่ฅฟ็, ไธญๅฝ
Extends over an area of 50 km2. The lithologies surrounding the Huayangchuan deposit mainly comprise the gneiss of the Taihua Group, the Proterozoic Xiaohe granitoids and granitic porphyry, and Mesozoic granitoids with some Paleoproterozoic pegmatite dikes, carbonatites, and mafic rocks. The Taihua Group in the Huayangchuan deposit contains amphibole-plagioclase gneiss, plagioclase gneiss, biotite-plagioclase gneiss, granitic gneiss, amphibole-gneiss, and migmatite.
The mineralization of uranium, niobium, and REEs in the Huayangchuan deposit is most closely related to carbonatite rocks, which are mostly in the form of irregular network veins, lenses, or dendrites. The mineral resources (e.g., U, Nb, REE, Ba, and Sr; excluding Pb) are mostly associated with or hosted in carbonatite dikes. The mineralization usually presents as dissemination in carbonatites or contact zones between carbonatite dikes and wall rocks. These ore-bearing veins along the brittle fracture intruded the basement rocks of the ArcheanโPaleoproterozoic Taihua Group, Paleoproterozoic Xiongโer Group, Proterozoic granite pegmatite, and monzonite granite. Carbonatite rocks in the Huayangchuan deposit are widely developed with varying degrees of typical wall rock alteration, including fenitization, silicitization, biotitization, chloritization, and actinolitization. According to the paragenetic association of the altered minerals, carbonatite veins can be roughly divided into three types: light-colored quartzโcalcite veins, aegirineโbiotite quartzโcalcite ore-bearing veins, and zeolite-bearing quartzโcalcite veins. The mineralization zonation at Huayangchuan commonly occurs as veinlets and (locally) stockworks in the carbonatite dykes. Over 40 ore and gangue minerals were identified at Huayangchuan.
The carbonatite mineralization can be divided into three substages, i.e., sulfate (BaโSr), alkali-rich U, and REE-U mineralization. Sulfate assemblages (barite-celestite โ+ โcalcite โ+ โphlogopite โ+ โyellowish barite-celestite) commonly occur as aggregates. The alkali-rich U assemblage contains pyrochlore (red coarse-grained euhedral) โ+ โcalcite โ+ โaegirine-augite โ+ โtitanite โ+ โapatite โยฑ โquartz โยฑ โmagnetite โยฑ โmicrocline โยฑ โamphibole โยฑ โ(galena โ+ โpyrite). REE-U mineral assemblage contains pyrochlore (medium-fine grained) โ+ โcalcite โ+ โmonazite โ+ โallanite โ+ โphlogopite โยฑ โbiotite โยฑ โmolybdenite, and commonly occurs as crumb or aggregates.
The Huayangchuan UโNbโREE deposit, located in the northern QOB, contains distinctive Nb and REE mineralization, with estimated resources of 111 kt Nb at 0.019 % and 550 kt REE at 0.085 %. Most ore bodies are hosted by carbonatite dykes derived from carbonatitic precursors that intrude the ArcheanโPaleoproterozoic Taihua Group. The Taihua Group TTG gneiss is the oldest crystalline basement (2.6โ2.2 Ga) in the Huayangchuan district. The ore-bearing carbonatite dikes are mainly localized along the NW-SE trending tensional faults and the associated secondary fractures. The ore bodies are developed as veins, stockworks, and lenticular bodies, extending for approximately 2650 m from Yangyugou in the northwest to Liujiagou in the southeast, with strike directions of 120ยฐโ130ยฐ. Over the exposed elevation interval of 1450โ750 m a.s.l., these ore bodies show a steep northwestward attitude, with dips mostly ranging from 60ยฐ to 70ยฐ. Petrographic observations indicate the presence of two carbonatite types in the Huayangchuan UโNbโPb deposit. Both showing extensive signs of overprinting and post-magmatic features: Type I (calcite + aegirine-augite + quartz + uranopyrochlore ยฑ feldspar) and Type II (calcite + quartz + barite + galena ยฑ zeolite) carbonatite.
The mineralization of uranium, niobium, and REEs in the Huayangchuan deposit is most closely related to carbonatite rocks, which are mostly in the form of irregular network veins, lenses, or dendrites. The mineral resources (e.g., U, Nb, REE, Ba, and Sr; excluding Pb) are mostly associated with or hosted in carbonatite dikes. The mineralization usually presents as dissemination in carbonatites or contact zones between carbonatite dikes and wall rocks. These ore-bearing veins along the brittle fracture intruded the basement rocks of the ArcheanโPaleoproterozoic Taihua Group, Paleoproterozoic Xiongโer Group, Proterozoic granite pegmatite, and monzonite granite. Carbonatite rocks in the Huayangchuan deposit are widely developed with varying degrees of typical wall rock alteration, including fenitization, silicitization, biotitization, chloritization, and actinolitization. According to the paragenetic association of the altered minerals, carbonatite veins can be roughly divided into three types: light-colored quartzโcalcite veins, aegirineโbiotite quartzโcalcite ore-bearing veins, and zeolite-bearing quartzโcalcite veins. The mineralization zonation at Huayangchuan commonly occurs as veinlets and (locally) stockworks in the carbonatite dykes. Over 40 ore and gangue minerals were identified at Huayangchuan.
The carbonatite mineralization can be divided into three substages, i.e., sulfate (BaโSr), alkali-rich U, and REE-U mineralization. Sulfate assemblages (barite-celestite โ+ โcalcite โ+ โphlogopite โ+ โyellowish barite-celestite) commonly occur as aggregates. The alkali-rich U assemblage contains pyrochlore (red coarse-grained euhedral) โ+ โcalcite โ+ โaegirine-augite โ+ โtitanite โ+ โapatite โยฑ โquartz โยฑ โmagnetite โยฑ โmicrocline โยฑ โamphibole โยฑ โ(galena โ+ โpyrite). REE-U mineral assemblage contains pyrochlore (medium-fine grained) โ+ โcalcite โ+ โmonazite โ+ โallanite โ+ โphlogopite โยฑ โbiotite โยฑ โmolybdenite, and commonly occurs as crumb or aggregates.
The Huayangchuan UโNbโREE deposit, located in the northern QOB, contains distinctive Nb and REE mineralization, with estimated resources of 111 kt Nb at 0.019 % and 550 kt REE at 0.085 %. Most ore bodies are hosted by carbonatite dykes derived from carbonatitic precursors that intrude the ArcheanโPaleoproterozoic Taihua Group. The Taihua Group TTG gneiss is the oldest crystalline basement (2.6โ2.2 Ga) in the Huayangchuan district. The ore-bearing carbonatite dikes are mainly localized along the NW-SE trending tensional faults and the associated secondary fractures. The ore bodies are developed as veins, stockworks, and lenticular bodies, extending for approximately 2650 m from Yangyugou in the northwest to Liujiagou in the southeast, with strike directions of 120ยฐโ130ยฐ. Over the exposed elevation interval of 1450โ750 m a.s.l., these ore bodies show a steep northwestward attitude, with dips mostly ranging from 60ยฐ to 70ยฐ. Petrographic observations indicate the presence of two carbonatite types in the Huayangchuan UโNbโPb deposit. Both showing extensive signs of overprinting and post-magmatic features: Type I (calcite + aegirine-augite + quartz + uranopyrochlore ยฑ feldspar) and Type II (calcite + quartz + barite + galena ยฑ zeolite) carbonatite.
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
32 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| โ | Galena | 2.CD.10 | PbS |
| โ | Molybdenite | 2.EA.30 | MoS2 |
| โ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| โ | 'Pyrochlore Group' | 4.00. | A2Nb2(O,OH)6Z |
| โ | 'var. Uranpyrochlore (of Hogarth 1977)' | 4.00. | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| โ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| โ | Minium | 4.BD.05 | Pb3O4 |
| โ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| โ | Quartz | 4.DA.05 | SiO2 |
| โ | Rutile | 4.DB.05 | TiO2 |
| โ | Changbaiite | 4.DF.10 | PbNb2O6 |
| โ | Uraninite | 4.DL.05 | UO2 |
| Group 5 - Nitrates and Carbonates | |||
| โ | Calcite | 5.AB.05 | CaCO3 |
| โ | Cerussite | 5.AB.15 | PbCO3 |
| โ | Strontianite | 5.AB.15 | SrCO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| โ | Anglesite | 7.AD.35 | PbSO4 |
| โ | Baryte | 7.AD.35 | BaSO4 |
| โ | Celestine | 7.AD.35 | SrSO4 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| โ | Monazite-(Ce) | 8.AD.50 | Ce(PO4) |
| โ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
| Group 9 - Silicates | |||
| โ | Thorite | 9.AD.30 | Th(SiO4) |
| โ | Zircon | 9.AD.30 | Zr(SiO4) |
| โ | Thorite var. Uranothorite | 9.AD.30 | (Th,U)SiO4 |
| โ | Titanite | 9.AG.15 | CaTiO(SiO4) |
| โ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| โ | Zoisite | 9.BG.10 | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| โ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| โ | Aegirine-augite | 9.DA.20 | (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 |
| โ | Aegirine | 9.DA.25 | NaFe3+Si2O6 |
| โ | Actinolite | 9.DE.10 | โปCa2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| โ | Arfvedsonite | 9.DE.25 | NaNa2(Fe2+4Fe3+)Si8O22(OH)2 |
| โ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| โ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| โ | Phlogopite | 9.EC.20 | KMg3(AlSi3O10)(OH)2 |
| โ | Microcline | 9.FA.30 | K(AlSi3O8) |
| โ | Albite | 9.FA.35 | Na(AlSi3O8) |
| โ | 'Zeolite Group' | 9.G0. | |
| Unclassified | |||
| โ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| โ | 'Bastnรคsite' | - | (Ce/Nd/Y/REE)(CO3)F |
| โ | 'Pyrochlore Supergroup var. Betafite (of Hogarth 1977)' | - | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| โ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| โ | 'Chlorite Group' | - | |
| โ | 'Clay minerals' | - | |
| โ | 'Feldspar Group' | - | |
| โ | 'Calcium Amphibole Subgroup var. Hornblende' | - | AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| โ | 'Limonite' | - | |
| โ | 'Monazite Group' | - | REE(PO4) |
| โ | 'Wad' | - | |
| โ | 'Xenotime' | - | |
| โ | 'Columbite-(Fe)-Columbite-(Mn) Series' | - | |
| โ | 'Hornblende Root Name Group' | - | โปCa2(C2+4C3+)(AlSi7O22)W2 |
| โ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| โ | 'K Feldspar' | - | |
| โ | 'Pyroxene Group' | - | ADSi2O6 |
| โ | 'Garnet Group' | - | X3Z2(SiO4)3 |
| โ | 'Fergusonite' | - | |
| โ | 'Pyrochlore Supergroup' | - | A2-mD2X6-wZ1-n |
| โ | 'Apatite' | - | Ca5(PO4)3A |
| โ | 'Calcium Amphibole Subgroup' | - | AnCa2(C2+5-mC3+m)(Si8-(n+m)Al(n+m))W2 |
| โ | 'Chevkinite Group' | - | |
| โ | 'Allanite Group' | - | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| H | โ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| H | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| H | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| H | โ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| H | โ Pyrochlore Group | A2Nb2(O,OH)6Z |
| H | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| H | โ Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| H | โ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| H | โ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| C | Carbon | |
| C | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| C | โ Calcite | CaCO3 |
| C | โ Cerussite | PbCO3 |
| C | โ Strontianite | SrCO3 |
| O | Oxygen | |
| O | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| O | โ Aegirine | NaFe3+Si2O6 |
| O | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| O | โ Albite | Na(AlSi3O8) |
| O | โ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | โ Anglesite | PbSO4 |
| O | โ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| O | โ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | โ Baryte | BaSO4 |
| O | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| O | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| O | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | โ Calcite | CaCO3 |
| O | โ Celestine | SrSO4 |
| O | โ Cerussite | PbCO3 |
| O | โ Changbaiite | PbNb2O6 |
| O | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | โ Fluorapatite | Ca5(PO4)3F |
| O | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| O | โ Ilmenite | Fe2+TiO3 |
| O | โ Magnetite | Fe2+Fe23+O4 |
| O | โ Microcline | K(AlSi3O8) |
| O | โ Minium | Pb3O4 |
| O | โ Monazite Group | REE(PO4) |
| O | โ Monazite-(Ce) | Ce(PO4) |
| O | โ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| O | โ Pyrochlore Group | A2Nb2(O,OH)6Z |
| O | โ Quartz | SiO2 |
| O | โ Rutile | TiO2 |
| O | โ Strontianite | SrCO3 |
| O | โ Thorite | Th(SiO4) |
| O | โ Titanite | CaTiO(SiO4) |
| O | โ Uraninite | UO2 |
| O | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| O | โ Zircon | Zr(SiO4) |
| O | โ Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| O | โ Thorite var. Uranothorite | (Th,U)SiO4 |
| O | โ Columbite-(Fe)-Columbite-(Mn) Series | |
| O | โ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| O | โ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | โ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | โ Pyroxene Group | ADSi2O6 |
| O | โ Garnet Group | X3Z2(SiO4)3 |
| O | โ Apatite | Ca5(PO4)3A |
| O | โ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| F | Fluorine | |
| F | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| F | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| F | โ Fluorapatite | Ca5(PO4)3F |
| F | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| F | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Na | Sodium | |
| Na | โ Aegirine | NaFe3+Si2O6 |
| Na | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Na | โ Albite | Na(AlSi3O8) |
| Na | โ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Na | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| Na | โ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Mg | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Mg | โ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Al | Aluminium | |
| Al | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Al | โ Albite | Na(AlSi3O8) |
| Al | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Al | โ Microcline | K(AlSi3O8) |
| Al | โ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Al | โ Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| Al | โ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Al | โ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | โ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | โ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | Silicon | |
| Si | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Si | โ Aegirine | NaFe3+Si2O6 |
| Si | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Si | โ Albite | Na(AlSi3O8) |
| Si | โ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Si | โ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Si | โ Microcline | K(AlSi3O8) |
| Si | โ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Si | โ Quartz | SiO2 |
| Si | โ Thorite | Th(SiO4) |
| Si | โ Titanite | CaTiO(SiO4) |
| Si | โ Zircon | Zr(SiO4) |
| Si | โ Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| Si | โ Thorite var. Uranothorite | (Th,U)SiO4 |
| Si | โ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Si | โ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | โ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | โ Pyroxene Group | ADSi2O6 |
| Si | โ Garnet Group | X3Z2(SiO4)3 |
| Si | โ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | โ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| P | Phosphorus | |
| P | โ Fluorapatite | Ca5(PO4)3F |
| P | โ Monazite Group | REE(PO4) |
| P | โ Monazite-(Ce) | Ce(PO4) |
| P | โ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | โ Anglesite | PbSO4 |
| S | โ Baryte | BaSO4 |
| S | โ Celestine | SrSO4 |
| S | โ Galena | PbS |
| S | โ Molybdenite | MoS2 |
| S | โ Pyrite | FeS2 |
| Cl | Chlorine | |
| Cl | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| K | Potassium | |
| K | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | โ Microcline | K(AlSi3O8) |
| K | โ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | โ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| K | โ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Ca | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Ca | โ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| Ca | โ Calcite | CaCO3 |
| Ca | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | โ Fluorapatite | Ca5(PO4)3F |
| Ca | โ Calcium Amphibole Subgroup var. Hornblende | AnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Ca | โ Titanite | CaTiO(SiO4) |
| Ca | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Ca | โ Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| Ca | โ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Ca | โ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | โ Apatite | Ca5(PO4)3A |
| Ca | โ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Ti | Titanium | |
| Ti | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| Ti | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | โ Ilmenite | Fe2+TiO3 |
| Ti | โ Rutile | TiO2 |
| Ti | โ Titanite | CaTiO(SiO4) |
| Ti | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Mn | Manganese | |
| Mn | โ Columbite-(Fe)-Columbite-(Mn) Series | |
| Fe | Iron | |
| Fe | โ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Fe | โ Aegirine | NaFe3+Si2O6 |
| Fe | โ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
| Fe | โ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Fe | โ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | โ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | โ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | โ Ilmenite | Fe2+TiO3 |
| Fe | โ Magnetite | Fe2+Fe23+O4 |
| Fe | โ Pyrite | FeS2 |
| Fe | โ Columbite-(Fe)-Columbite-(Mn) Series | |
| Sr | Strontium | |
| Sr | โ Celestine | SrSO4 |
| Sr | โ Strontianite | SrCO3 |
| Y | Yttrium | |
| Y | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| Zr | Zirconium | |
| Zr | โ Zircon | Zr(SiO4) |
| Nb | Niobium | |
| Nb | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| Nb | โ Changbaiite | PbNb2O6 |
| Nb | โ Pyrochlore Group | A2Nb2(O,OH)6Z |
| Nb | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Nb | โ Columbite-(Fe)-Columbite-(Mn) Series | |
| Mo | Molybdenum | |
| Mo | โ Molybdenite | MoS2 |
| Ba | Barium | |
| Ba | โ Baryte | BaSO4 |
| Ce | Cerium | |
| Ce | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| Ce | โ Monazite-(Ce) | Ce(PO4) |
| Ce | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Nd | Neodymium | |
| Nd | โ Bastnรคsite | (Ce/Nd/Y/REE)(CO3)F |
| Ta | Tantalum | |
| Ta | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| Ta | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| Pb | Lead | |
| Pb | โ Anglesite | PbSO4 |
| Pb | โ Cerussite | PbCO3 |
| Pb | โ Changbaiite | PbNb2O6 |
| Pb | โ Galena | PbS |
| Pb | โ Minium | Pb3O4 |
| Th | Thorium | |
| Th | โ Thorite | Th(SiO4) |
| Th | โ Thorite var. Uranothorite | (Th,U)SiO4 |
| U | Uranium | |
| U | โ Pyrochlore Supergroup var. Betafite (of Hogarth 1977) | (Ca,Na,U)2(Ti, Nb,Ta)2O6Z(OH) |
| U | โ Uraninite | UO2 |
| U | โ Pyrochlore Group var. Uranpyrochlore (of Hogarth 1977) | (Ca,U,Ce)2(Nb,Ti,Ta)2O6(OH,F) |
| U | โ Thorite var. Uranothorite | (Th,U)SiO4 |
Geochronology
Mineralization age: Early Jurassic : 181 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
| Geologic Time | Rocks, Minerals and Events | ||||||
|---|---|---|---|---|---|---|---|
| Phanerozoic | |||||||
| Mesozoic | |||||||
| Jurassic | |||||||
| Early Jurassic |
| ||||||
Other Regions, Features and Areas containing this locality
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References
Li, Putao, Li, Yongjun, Gu, Pingyang, He, Shiping, Zhuang, Yujun, Chen, Ruiming (2023) Paleoproterozoic U Mineralization in Huayangchuan Deposit, Xiaoqinling Area: Evidence from the U–Rich Granitic Pegmatite. Minerals, 13 (7) doi:10.3390/min13070936
[1]Wang, Wenyi, Tan, Shuang, Wan, Jianjun, Hu, Xuelian, Peng, Haoyang, Liu, Chengdong (2024) Insights from Dikes for Multistage Granitic Magmatism in the Huayangchuan Uranium Polymetallic Deposit, Qinling Orogen. Minerals, 14 (3) doi:10.3390/min14030261
[3]Zeng, Tao; Tang, Li; Lv, Peng-Rui; Fusswinkel, Tobias; Wagner, Thomas; Li, Wei; Jia, Li-Hui; Chen, Long-Long (2026) Hydrothermal REE redistribution in carbonatite system: Fluorapatite evidence from the Huayangchuan deposit, Qinling orogenic Belt, central China. Ore Geology Reviews, 198. p.107569. doi:10.1016/j.oregeorev.2026.107569