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Luming Mo-(Au) deposit, Tieli City, Yichun, Heilongjiang, Chinai
Regional Level Types
Luming Mo-(Au) depositDeposit
Tieli CityCity
YichunPrefecture
HeilongjiangProvince
ChinaCountry

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Latitude & Longitude (WGS84):
47° 21' 24'' North , 128° 34' 0'' East
Latitude & Longitude (decimal):
47.35694,128.56667
GeoHash:
G#: yb7mmt56h
GRN:
N32E64
Type:
Deposit
Köppen climate type:
Dwb : Monsoon-influenced warm-summer humid continental climate
Nearest Settlements:
PlacePopulationDistance
Yichun155,762 (2012)46.7km
Langxiang57,318 (2013)50.7km
Youhao78,402 (2013)58.7km
Mindat Locality ID:
229610
Long-form identifier:
mindat:1:2:229610:7
GUID (UUID V4):
0
Name(s) in local language(s):
鹿鸣钼(金)矿, 铁力市, 伊春市, 黑龙江省, 中国


Porphyry molybdenum-(gold) deposit, hosted in Mesozoic fine-grained porphyritic monzogranite and and medium-grained monzogranite porphyry.

The estimated mineral resource of that work is 814 million metric tons, with an average Mo grade of 0.092%, containing a total Mo metal of 751 thousand metric tons. The Luming PMD is defined by a dominant orebody, which is distributed within monzogranite, granite porphyry, and hydrothermal breccias between exploration lines 27N and 28N. The orebody exhibits a donut-shaped configuration on the plane, with an approximate surface exposure length and width of 1200 m and an area of about 1.5 km2. The elevation depth of the orebody ranges from 540 m to –220 m. From an industrial perspective, the near-surface portion of Luming PMD is primarily composed of oxide ores. The thickness of the oxide zone ranges from 0.8 m to 42.4 m, with an average thickness of 16 m. The oxidation rates of the zone range from 10.7% to 92.9%, with an average of 28%. Below this zone are all sulfide ores, without mixed ore zones. Four alteration zones developed around the orebody: silicification-K-feldsparization-biotitization zone, silicification-illitization-K-feldsparization zone, silicification-illitization-chloritization zone, and silicification-pyritization-chloritization zone. The central distribution of the silicification-K-feldsparization-biotitization zone is primarily associated with the economic Mo mineralization occurring at its periphery. The silicification-illitization-K-feldsparization zone is characterized by quartz and illite replacement on feldspar, with some residual early-stage K-feldsparization. The majority of economic ore bodies are found within this alteration zone. The degree of silicification and illitization is relatively limited in the silicification-illitization-chloritization zone. Four distinct phases of mineralization were identified: a quartz-pyrite phase; a quartz-molybdenite-chalcopyrite phase; a quartz-polymetallic (molybdenite-chalcopyrite-galena-sphalerite) phase; and a quartz-calcite-pyrite phase.

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


27 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:

ⓘ Albite
Formula: Na(AlSi3O8)
ⓘ Albite var. Oligoclase
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
ⓘ 'Allanite Group'
Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
ⓘ 'Amphibole Supergroup'
Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ Anorthite
Formula: Ca(Al2Si2O8)
ⓘ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
References:
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Arsenopyrite
Formula: FeAsS
ⓘ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Bornite
Formula: Cu5FeS4
ⓘ Calcite
Formula: CaCO3
ⓘ 'Calcium Amphibole Subgroup'
Formula: AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ 'Calcium Amphibole Subgroup var. Hornblende'
Formula: AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ Chalcopyrite
Formula: CuFeS2
ⓘ 'Chlorite Group'
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Chloritoid
Formula: Fe2+Al2O(SiO4)(OH)2
ⓘ Covellite
Formula: CuS
ⓘ Digenite
Formula: Cu9S5
ⓘ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘ 'Feldspar Group'
References:
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ 'Feldspar Group var. Perthite'
ⓘ Galena
Formula: PbS
ⓘ Ilmenite
Formula: Fe2+TiO3
ⓘ Jarosite
Formula: KFe3+3(SO4)2(OH)6
ⓘ Kaolinite
Formula: Al2(Si2O5)(OH)4
ⓘ 'K Feldspar'
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ 'Limonite'
ⓘ Magnesio-hornblende
Formula: ◻Ca2(Mg4Al)(Si7Al)O22(OH)2
ⓘ Magnetite
Formula: Fe2+Fe3+2O4
References:
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
ⓘ Magnetite var. Titanium-bearing Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
ⓘ Molybdenite
Formula: MoS2
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Molybdite
Formula: MoO3
ⓘ Montmorillonite
Formula: (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
ⓘ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
ⓘ Muscovite var. Illite
Formula: K0.65Al2.0[Al0.65Si3.35O10](OH)2
ⓘ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
References:
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Pyrite
Formula: FeS2
ⓘ Pyrrhotite
Formula: Fe1-xS
ⓘ Quartz
Formula: SiO2
References:
Yongming Shi, Bin Cui, and Weilin Jia (2007): Geology and Prospecting 43(2), 19-22
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Mineral Deposits 31(6), 1301-1310
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Rutile
Formula: TiO2
ⓘ Sphalerite
Formula: ZnS
ⓘ Titanite
Formula: CaTi(SiO4)O
References:
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Geology and Exploration 46(5), 852-862
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
ⓘ Zircon
Formula: Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
ⓘDigenite2.BA.10Cu9S5
ⓘBornite2.BA.15Cu5FeS4
ⓘCovellite2.CA.05aCuS
ⓘSphalerite2.CB.05aZnS
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘGalena2.CD.10PbS
ⓘMolybdenite2.EA.30MoS2
ⓘPyrite2.EB.05aFeS2
ⓘArsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘvar. Titanium-bearing Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘQuartz4.DA.05SiO2
ⓘRutile4.DB.05TiO2
ⓘMolybdite4.E0.10MoO3
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘJarosite7.BC.10KFe3+3(SO4)2(OH)6
Group 9 - Silicates
ⓘZircon9.AD.30Zr(SiO4)
ⓘChloritoid9.AF.85Fe2+Al2O(SiO4)(OH)2
ⓘTitanite9.AG.15CaTi(SiO4)O
ⓘEpidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘMagnesio-hornblende9.DE.10◻Ca2(Mg4Al)(Si7Al)O22(OH)2
ⓘMuscovite
var. Illite		9.EC.15K0.65Al2.0[Al0.65Si3.35O10](OH)2
ⓘ9.EC.15KAl2(AlSi3O10)(OH)2
ⓘvar. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘMontmorillonite9.EC.40(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
ⓘKaolinite9.ED.05Al2(Si2O5)(OH)4
ⓘAlbite9.FA.35Na(AlSi3O8)
ⓘAnorthite9.FA.35Ca(Al2Si2O8)
ⓘAlbite
var. Oligoclase		9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
Unclassified
ⓘ'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
ⓘ'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
ⓘ'Chlorite Group'-
ⓘ'Feldspar Group'-
ⓘ'Calcium Amphibole Subgroup
var. Hornblende'		-AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ'Limonite'-
ⓘ'Feldspar Group
var. Perthite'		-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'K Feldspar'-
ⓘ'Apatite'-Ca5(PO4)3(Cl/F/OH)
ⓘ'Calcium Amphibole Subgroup'-AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
ⓘ'Allanite Group'-(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)

List of minerals for each chemical element

HHydrogen
Hⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Hⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hⓘ ChloritoidFe2+Al2O(SiO4)(OH)2
Hⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Hⓘ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Hⓘ JarositeKFe33+(SO4)2(OH)6
Hⓘ KaoliniteAl2(Si2O5)(OH)4
Hⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Hⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Hⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Hⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Hⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Hⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Hⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
CCarbon
Cⓘ CalciteCaCO3
OOxygen
Oⓘ AlbiteNa(AlSi3O8)
Oⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Oⓘ AnorthiteCa(Al2Si2O8)
Oⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oⓘ CalciteCaCO3
Oⓘ ChloritoidFe2+Al2O(SiO4)(OH)2
Oⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Oⓘ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Oⓘ IlmeniteFe2+TiO3
Oⓘ JarositeKFe33+(SO4)2(OH)6
Oⓘ KaoliniteAl2(Si2O5)(OH)4
Oⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Oⓘ MagnetiteFe2+Fe23+O4
Oⓘ MolybditeMoO3
Oⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Oⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Oⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Oⓘ QuartzSiO2
Oⓘ RutileTiO2
Oⓘ TitaniteCaTi(SiO4)O
Oⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
Oⓘ ZirconZr(SiO4)
Oⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Oⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Oⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
FFluorine
Fⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Fⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Fⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Fⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
NaSodium
Naⓘ AlbiteNa(AlSi3O8)
Naⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Naⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mgⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Mgⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
AlAluminium
Alⓘ AlbiteNa(AlSi3O8)
Alⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Alⓘ AnorthiteCa(Al2Si2O8)
Alⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alⓘ ChloritoidFe2+Al2O(SiO4)(OH)2
Alⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Alⓘ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Alⓘ KaoliniteAl2(Si2O5)(OH)4
Alⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Alⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Alⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Alⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Alⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Alⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
SiSilicon
Siⓘ AlbiteNa(AlSi3O8)
Siⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Siⓘ AnorthiteCa(Al2Si2O8)
Siⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siⓘ ChloritoidFe2+Al2O(SiO4)(OH)2
Siⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Siⓘ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Siⓘ KaoliniteAl2(Si2O5)(OH)4
Siⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Siⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Siⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Siⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Siⓘ QuartzSiO2
Siⓘ TitaniteCaTi(SiO4)O
Siⓘ ZirconZr(SiO4)
Siⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Siⓘ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
PPhosphorus
Pⓘ ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
Sⓘ ArsenopyriteFeAsS
Sⓘ BorniteCu5FeS4
Sⓘ ChalcopyriteCuFeS2
Sⓘ CovelliteCuS
Sⓘ DigeniteCu9S5
Sⓘ GalenaPbS
Sⓘ JarositeKFe33+(SO4)2(OH)6
Sⓘ MolybdeniteMoS2
Sⓘ PyriteFeS2
Sⓘ PyrrhotiteFe1-xS
Sⓘ SphaleriteZnS
ClChlorine
Clⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Clⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Clⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Clⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
KPotassium
Kⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kⓘ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Kⓘ JarositeKFe33+(SO4)2(OH)6
Kⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Kⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caⓘ AnorthiteCa(Al2Si2O8)
Caⓘ CalciteCaCO3
Caⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caⓘ Calcium Amphibole Subgroup var. HornblendeAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
Caⓘ Magnesio-hornblende◻Ca2(Mg4Al)(Si7Al)O22(OH)2
Caⓘ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Caⓘ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Caⓘ TitaniteCaTi(SiO4)O
Caⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caⓘ ApatiteCa5(PO4)3(Cl/F/OH)
Caⓘ Calcium Amphibole SubgroupAnCa2(Z2+5-mZm3+)(Si8-(n+m)Al(n+m))(OH,F,Cl)2
TiTitanium
Tiⓘ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Tiⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Tiⓘ IlmeniteFe2+TiO3
Tiⓘ RutileTiO2
Tiⓘ TitaniteCaTi(SiO4)O
Tiⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
FeIron
Feⓘ ArsenopyriteFeAsS
Feⓘ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feⓘ BorniteCu5FeS4
Feⓘ ChalcopyriteCuFeS2
Feⓘ ChloritoidFe2+Al2O(SiO4)(OH)2
Feⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feⓘ IlmeniteFe2+TiO3
Feⓘ JarositeKFe33+(SO4)2(OH)6
Feⓘ MagnetiteFe2+Fe23+O4
Feⓘ PyriteFeS2
Feⓘ PyrrhotiteFe1-xS
Feⓘ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
CuCopper
Cuⓘ BorniteCu5FeS4
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ CovelliteCuS
Cuⓘ DigeniteCu9S5
ZnZinc
Znⓘ SphaleriteZnS
AsArsenic
Asⓘ ArsenopyriteFeAsS
ZrZirconium
Zrⓘ ZirconZr(SiO4)
MoMolybdenum
Moⓘ MolybdeniteMoS2
Moⓘ MolybditeMoO3
PbLead
Pbⓘ GalenaPbS

Other Regions, Features and Areas containing this locality

Amur PlateTectonic Plate
AsiaContinent
Eurasian Plate

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References

Yongming Shi, Bin Cui, and Weilin Jia (2007): Geological features of Luming molybdenum deposit at Tieli in Heilongjiang Province. Geology and Prospecting 43(2), 19-22.
Zhenhe Han, Zheyan Jin, Jun Lü, Guochen Li, and Kun Zhang (2010): Characteristics of diagenesis and mineralization of the ore-bearing granite and its tectonic setting in the Early Mesozoic era in the Luming-Xing'an-Qianjin area, southeastern Lesser Hingan Mountains. Geology and Exploration 46(5), 852-862.
Jun Shao, Hongzhi Yang, Bin Jia, and Mingsheng Peng (2012): Geological characteristics and ore-forming age of Luming Mo deposit in Heilongjiang Province. Mineral Deposits 31(6), 1301-1310 (in Chinese with English abstract).
Qu, P., Niu, H. C., Weng, Q., Li, N. B., Zhao, Y., & Zhang, H. J. (2022). Apatite and zircon geochemistry for discriminating ore-forming intrusions in the Luming giant porphyry Mo deposit, Northeastern China. Ore Geology Reviews, 104771.
Qu, P., Niu, H. C., Weng, Q., Yang, W. B., Yang, Y. Y., & Zhang, D. (2022). In situ U-Pb geochronology, elemental and Nd isotopic compositions of titanite from the Mesozoic porphyry Mo deposits, NE China. Ore Geology Reviews, 144, 104817.
[2]Ouyang, Hegen, Caulfield, John (2023) UNDERSTANDING Cu DEFICIENCY AND Mo ENRICHMENT IN THE JURASSIC ZHANGGUANGCAI-LESSER XING’AN CONTINENTAL ARC (NE CHINA): INSIGHTS FROM THE LUMING PORPHYRY MO DEPOSIT. Economic Geology, 118 (4) 857-881 doi:10.5382/econgeo.4989
[1]Gao, Bangfei, Dong, Minghua, Xie, Hui, Liu, Zhiliang, Li, Yihang, Zhou, Tong (2024) Discovery and Exploration of the Luming Porphyry Mo Deposit, Northeastern China: Implications for Regional Prospecting. Minerals, 14 (7) doi:10.3390/min14070718
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