Jinqingding Au deposit, Rushan ore field, Muping-Rushan metallogenic belt, Rushan Co., Weihai, Shandong, Chinai
| Regional Level Types | |
|---|---|
| Jinqingding Au deposit | Deposit |
| Rushan ore field | Ore Field |
| Muping-Rushan metallogenic belt | Mineral Belt |
| Rushan Co. | County |
| Weihai | Prefecture |
| Shandong | Province |
| China | Country |
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Latitude & Longitude (WGS84):
37° 7' 0'' North , 121° 38' 49'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Name(s) in local language(s):
金青顶金矿, 乳山矿田, 乳山市, 威海市, 胶东半岛, 山东省, 中国
Granitoid-related gold deposit, hosted in Kunyushan gneissic granite, and consisting of quartz veins, veinlets and disseminations. At shallow depth, copper ore bodies occur locally. Gold is mainly hosted in pyrite, chalcopyrite, sphalerite and galena, as interstitial and fissure fillings, and as inclusions. Sixteen orebodies have been discovered in the Jinqingding deposit; orebody No. II is the largest and contains 96% of the proven reserve.
The Paleoarchean Jingshan Group biotite schist occurs as small enclaves within the Kunyu Mountain granite. The lamprophyre veins and granodiorite porphyry are closely associated with the gold veins. The Jinqingding gold deposit has previously been discovered to have a total of 18 ore bodies, all of which are of the quartz vein type. The No. II ore body accounts for 96% of the confirmed resource reserves. The No. II ore body is distributed in a vein-like manner between exploration lines 0 to 35, controlled overall by the F3 fault, which is part of the regional General Jiangjunshi fault. The F1 fault is located in the middle of ore body, causing localized fracturing and displacement of the ore body. The F2 fault is parallel to the F1 fault but is far from the ore body, exerting no direct impact on the ore body. The ore body exhibits a gentle wave-like pattern along its strike and trend. The thickness of the ore body is generally around 2 m, with gold grades ranging from 2 × 10−6 to 20 × 10−6. The elevation range of the ore body is from 120 m to 1220 m. The No. II ore body is plate-like in shape, with a surface length of 245 m, trending SE (an overall trend of 20°), dipping NE (angle of 85° to 90°), and extending to a depth greater than 1200 m.
The hydrothermal alteration in the Jinqingding gold deposit is relatively strong, and mainly distributed along faults. From the near ore to the far ore, there is a sequential development of pyritized sericite alteration, sericite alteration, and potassic feldspathization, approximately symmetrically distributed around the ore body.
The Jinqingding deposit can be divided into three or four stages): (1) the pre-ore pyrite–quartz stage (subdivisible into two substages), characterized by the limited development of metallic sulfides, where pyrite predominantly occurs as disseminated, veinlet, and massive forms within milky-white quartz; (2) the main-ore quartz–polymetallic sulfide stage, dominated by smoky-gray gangue quartz with ore minerals consisting primarily of pyrite alongside chalcopyrite, marcasite, sphalerite, native gold, and various Te/Bi minerals; (3) the post-ore quartz–calcite stage. With an average grade of 6.44 g/t, the proven gold resource exceeds 32 tons.
Exploration has confirmed more than 35 tonnes of gold at an average grade of ∼ 10 g/t, making Jinqingding the largest deposit in this belt. The rocks exposed in the mining area are mainly the Paleoproterozoic Jingshan Group, including biotite-plagioclase gneiss, amphibolite, marble and Quaternary sediments. These metamorphic rocks are intruded by the Kunyushan granitic suite. Gold grades in stage 3 reaches peaks of 1000 g/t.
The Paleoarchean Jingshan Group biotite schist occurs as small enclaves within the Kunyu Mountain granite. The lamprophyre veins and granodiorite porphyry are closely associated with the gold veins. The Jinqingding gold deposit has previously been discovered to have a total of 18 ore bodies, all of which are of the quartz vein type. The No. II ore body accounts for 96% of the confirmed resource reserves. The No. II ore body is distributed in a vein-like manner between exploration lines 0 to 35, controlled overall by the F3 fault, which is part of the regional General Jiangjunshi fault. The F1 fault is located in the middle of ore body, causing localized fracturing and displacement of the ore body. The F2 fault is parallel to the F1 fault but is far from the ore body, exerting no direct impact on the ore body. The ore body exhibits a gentle wave-like pattern along its strike and trend. The thickness of the ore body is generally around 2 m, with gold grades ranging from 2 × 10−6 to 20 × 10−6. The elevation range of the ore body is from 120 m to 1220 m. The No. II ore body is plate-like in shape, with a surface length of 245 m, trending SE (an overall trend of 20°), dipping NE (angle of 85° to 90°), and extending to a depth greater than 1200 m.
The hydrothermal alteration in the Jinqingding gold deposit is relatively strong, and mainly distributed along faults. From the near ore to the far ore, there is a sequential development of pyritized sericite alteration, sericite alteration, and potassic feldspathization, approximately symmetrically distributed around the ore body.
The Jinqingding deposit can be divided into three or four stages): (1) the pre-ore pyrite–quartz stage (subdivisible into two substages), characterized by the limited development of metallic sulfides, where pyrite predominantly occurs as disseminated, veinlet, and massive forms within milky-white quartz; (2) the main-ore quartz–polymetallic sulfide stage, dominated by smoky-gray gangue quartz with ore minerals consisting primarily of pyrite alongside chalcopyrite, marcasite, sphalerite, native gold, and various Te/Bi minerals; (3) the post-ore quartz–calcite stage. With an average grade of 6.44 g/t, the proven gold resource exceeds 32 tons.
Exploration has confirmed more than 35 tonnes of gold at an average grade of ∼ 10 g/t, making Jinqingding the largest deposit in this belt. The rocks exposed in the mining area are mainly the Paleoproterozoic Jingshan Group, including biotite-plagioclase gneiss, amphibolite, marble and Quaternary sediments. These metamorphic rocks are intruded by the Kunyushan granitic suite. Gold grades in stage 3 reaches peaks of 1000 g/t.
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
40 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 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold var. Electrum | 1.AA.05 | (Au,Ag) |
| ⓘ | 1.AA.05 | Au | |
| ⓘ | Native Silver | 1.AA.05 | Ag |
| ⓘ | var. Küstelite | 1.AA.05 | Ag |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | Hessite | 2.BA.60 | Ag2Te |
| ⓘ | Petzite | 2.BA.75 | Ag3AuTe2 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Altaite | 2.CD.10 | PbTe |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pilsenite ? | 2.DC.05 | Bi4Te3 |
| ⓘ | Tellurobismuthite | 2.DC.05 | Bi2Te3 |
| ⓘ | Calaverite | 2.EA.10 | AuTe2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | Volynskite | 2.JA.20 | AgBiTe2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | var. Milky Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Siderite | 5.AB.05 | FeCO3 |
| ⓘ | Calcite var. Iron-bearing Calcite | 5.AB.05 | (Ca,Fe)CO3 |
| ⓘ | Ankerite | 5.AB.10 | Ca(Fe2+,Mg)(CO3)2 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| ⓘ | var. Iron-bearing Dolomite | 5.AB.10 | Ca(Mg,Fe)(CO3)2 |
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Group 9 - Silicates | |||
| ⓘ | Thorite | 9.AD.30 | Th(SiO4) |
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Titanite | 9.AG.15 | CaTiO(SiO4) |
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Muscovite var. Illite | 9.EC.15 | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| ⓘ | 9.EC.15 | KAl2(AlSi3O10)(OH)2 | |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Montmorillonite | 9.EC.40 | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| ⓘ | Halloysite | 9.ED.10 | Al2Si2O5(OH)4 · n(H2O) |
| ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| ⓘ | var. Oligoclase | 9.FA.35 | (Na,Ca)[Al(Si,Al)Si2O8] |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5(T8O22)W2 |
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Monazite Group' | - | REE(PO4) |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'K Feldspar' | - | |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
| ⓘ | 'Tetrahedrite Group' | - | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Halloysite | Al2Si2O5(OH)4 · n(H2O) |
| H | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | ⓘ Siderite | FeCO3 |
| C | ⓘ Calcite var. Iron-bearing Calcite | (Ca,Fe)CO3 |
| C | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Amphibole Supergroup | AB2C5(T8O22)W2 |
| O | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Halloysite | Al2Si2O5(OH)4 · n(H2O) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| O | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Microcline | K(AlSi3O8) |
| O | ⓘ Monazite Group | REE(PO4) |
| O | ⓘ Muscovite | KAl2(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 | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Siderite | FeCO3 |
| O | ⓘ Thorite | Th(SiO4) |
| O | ⓘ Titanite | CaTiO(SiO4) |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Quartz var. Milky Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Calcite var. Iron-bearing Calcite | (Ca,Fe)CO3 |
| O | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| O | ⓘ Apatite | Ca5(PO4)3A |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(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 |
| Mg | Magnesium | |
| Mg | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
| Mg | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Halloysite | Al2Si2O5(OH)4 · n(H2O) |
| Al | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Microcline | K(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(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. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Halloysite | Al2Si2O5(OH)4 · n(H2O) |
| Si | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Microcline | K(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(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 | ⓘ Quartz | SiO2 |
| Si | ⓘ Thorite | Th(SiO4) |
| Si | ⓘ Titanite | CaTiO(SiO4) |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Quartz var. Milky Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| P | Phosphorus | |
| P | ⓘ Monazite Group | REE(PO4) |
| P | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Acanthite | Ag2S |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Galena | PbS |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tetrahedrite Group | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| K | ⓘ Microcline | K(AlSi3O8) |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
| Ca | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
| Ca | ⓘ Titanite | CaTiO(SiO4) |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | ⓘ Calcite var. Iron-bearing Calcite | (Ca,Fe)CO3 |
| Ca | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Ca | ⓘ Apatite | Ca5(PO4)3A |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Rutile | TiO2 |
| Ti | ⓘ Titanite | CaTiO(SiO4) |
| Fe | Iron | |
| Fe | ⓘ Ankerite | Ca(Fe2+,Mg)(CO3)2 |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Siderite | FeCO3 |
| Fe | ⓘ Calcite var. Iron-bearing Calcite | (Ca,Fe)CO3 |
| Fe | ⓘ Dolomite var. Iron-bearing Dolomite | Ca(Mg,Fe)(CO3)2 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Ag | Silver | |
| Ag | ⓘ Acanthite | Ag2S |
| Ag | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Ag | ⓘ Hessite | Ag2Te |
| Ag | ⓘ Petzite | Ag3AuTe2 |
| Ag | ⓘ Native Silver | Ag |
| Ag | ⓘ Volynskite | AgBiTe2 |
| Ag | ⓘ Native Silver var. Küstelite | Ag |
| Te | Tellurium | |
| Te | ⓘ Altaite | PbTe |
| Te | ⓘ Calaverite | AuTe2 |
| Te | ⓘ Hessite | Ag2Te |
| Te | ⓘ Petzite | Ag3AuTe2 |
| Te | ⓘ Pilsenite | Bi4Te3 |
| Te | ⓘ Tellurobismuthite | Bi2Te3 |
| Te | ⓘ Volynskite | AgBiTe2 |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| Au | Gold | |
| Au | ⓘ Calaverite | AuTe2 |
| Au | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Au | ⓘ Native Gold | Au |
| Au | ⓘ Petzite | Ag3AuTe2 |
| Pb | Lead | |
| Pb | ⓘ Altaite | PbTe |
| Pb | ⓘ Galena | PbS |
| Bi | Bismuth | |
| Bi | ⓘ Pilsenite | Bi4Te3 |
| Bi | ⓘ Tellurobismuthite | Bi2Te3 |
| Bi | ⓘ Volynskite | AgBiTe2 |
| Th | Thorium | |
| Th | ⓘ Thorite | Th(SiO4) |
Other Regions, Features and Areas containing this locality
AsiaContinent
China
- Shandong
- Jiaodong Peninsula (Jiaodong Gold Province)Peninsula
- Muping-Rushan ore beltMineral Belt
- Jiaodong Peninsula (Jiaodong Gold Province)Peninsula
Eurasian PlateTectonic Plate
- North China CratonOrogen
- Su-Lu Belt (Su-Lu ultra high-pressure terrane)Accretionary Complex
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References
Qiu, Yumin, Groves, David I., McNaughton, Neal J., Wang, Liang-gen, Zhou, Taihe (2002) Nature, age, and tectonic setting of granitoid-hosted, orogenic gold deposits of the Jiaodong Peninsula, eastern North China craton, China. Mineralium Deposita, 37 (3) 283-305 doi:10.1007/s00126-001-0238-3
Chen, Binghan, Deng, Jun, Wei, Hantao, Ji, Xingzhong (2019) Trace Element Geochemistry in Quartz in the Jinqingding Gold Deposit, Jiaodong Peninsula, China: Implications for the Gold Precipitation Mechanism. Minerals, 9 (5) 326 doi:10.3390/min9050326
[1]Huang, Xin, Sun, Deyou, Yu, Song, Wang, Yongjun, Shen, Lijun, Shao, Yubao, Lu, Changyong, Song, Qian, Xiao, Tingting (2024) The Sources of Ore-Forming Materials and Fluids for the Jinqingding Gold Deposit in the Mouping–Rushan Metallogenic Belt, Jiaodong Peninsula: Evidence from S-H-O Isotopes and Trace Elements in Pyrite. Minerals, 14 (11). doi:10.3390/min14111064
Cai, Wenyan, Song, Mingchun, Santosh, M., Li, Jian (2024) The gold-telluride connection: Evidence for multiple fluid pulses in the Jinqingding telluride-rich gold deposit of Jiaodong Peninsula, Eastern China. Geoscience Frontiers, 15 (3) 101795 doi:10.1016/j.gsf.2024.101795
[2]Li, Shi-Sheng; Zang, Chun-Juan; Li, Lin; Li, Sheng-Rong; Tao, Wei; Cheng, Xiang (2025) Geochemistry, isotopes, and morphology of coarse-grained pyrite from the Jinqingding gold deposit, Jiaodong Peninsula: Implications for episodic ore-forming fluid evolution. Ore Geology Reviews, 184. 106742 doi:10.1016/j.oregeorev.2025.106742
[3]Liu, Kun; Chen, Qi; Du, Zezhong; Zhang, Hankuo; Wang, Shuchun; Wang, Huisheng; Yu, Jiantao; Li, Long (2025) Decoding the driving mechanisms of high-grade gold enrichment in the Jiaodong Peninsula: Insights from episodic releases of gold-rich fluids in the Jinqingding deposit. Ore Geology Reviews, 187. 106975 doi:10.1016/j.oregeorev.2025.106975