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Heilongtan Au deposit, Sui Co., Suizhou, Hubei, Chinai
| Regional Level Types | |
|---|---|
| Heilongtan Au deposit | Deposit |
| Sui Co. | County |
| Suizhou | Prefecture |
| Hubei | Province |
| China | Country |
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Latitude & Longitude (WGS84):
32° 6' North , 113° 19' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Other/historical names associated with this locality:
Xiejiagou, Heilongtan, Wangjiawan, Shizikou
Xiejiagou is 3km SE of Heilongtan.
The Heilongtan-Xiejiagou Au deposit is composed of Heilongtan, Wangjiawan and Xiejiagou ore blocks, distributed along the Heilongtan fault from northwest to southeast. As a medium-sized Au deposit, the Heilongtan-Xiejiagou deposit contains average Au grade of 5.04 g/t and Ag grade between 155.6 and 221.6 g/t. This deposit is one of the most economic deposits discovered in recent years. Heilongtan is located about 45 km northwestern of the Suizhou city.
Nineteen exposed and five concealed ore bodies are identified recently that comprise 1595 kg Au and 46762 kg Ag. These ore bodies occur in the alteration zone and appear bedded, lentoid and veined, which share some similar occurrences.
The mine area is underlain mainly by Proterozoic volcanic–sedimentary sequences of the Wudang and Yaolinghe groups. The Wudang Group consists chiefly of intermediate- to felsic volcaniclastic-derived schists, including muscovite–albite schist, chlorite–epidote–albite schist, and albite leptynite. The Yaolinghe Group is dominated by intermediate- to mafic metavolcanic rocks, mainly actinolite–epidote–albite schist and chlorite–actinolite–epidote schist, and commonly contains epidote-rich segregations and locally preserved amygdaloidal textures. Gold mineralization is discontinuously developed along a ca. 4 km long corridor trending NW to NWW within strongly deformed greenschist-facies rocks.
Four blocks controlled by shear zones are recognized along strike, from northwest to southeast: Heilongtan, Wangjiawan, Xiejiagou, and Shizikou. In the Heilongtan block, 24 orebodies have been delineated, including 19 exposed and 5 concealed bodies, with estimated resources of ∼1.6 t Au and ∼46.8 t Ag. In the Wangjiawan, Xiejiagou, and Shizikou blocks, 18 gold orebodies have been identified, with estimated resources of ∼4.8 t Au and ∼23.4 t Ag. Ore grades vary markedly, ranging from 1.28 to 70.06 g/t Au (mean ∼3.66 g/t) and from 1 to 80 g/t Ag (mean ∼16.68 g/t). The ores also contain minor base metals, with mean contents of ∼0.12 wt% Cu, ∼0.01 wt% Pb, and ∼0.04 wt% Zn.
The three stages are defined as follows: quartz–sericite–pyrite stage (Stage I); quartz–pyrite stage (Stage II); quartz–polymetallic sulfide stage (Stage III).
The Heilongtan-Xiejiagou Au deposit is composed of Heilongtan, Wangjiawan and Xiejiagou ore blocks, distributed along the Heilongtan fault from northwest to southeast. As a medium-sized Au deposit, the Heilongtan-Xiejiagou deposit contains average Au grade of 5.04 g/t and Ag grade between 155.6 and 221.6 g/t. This deposit is one of the most economic deposits discovered in recent years. Heilongtan is located about 45 km northwestern of the Suizhou city.
Nineteen exposed and five concealed ore bodies are identified recently that comprise 1595 kg Au and 46762 kg Ag. These ore bodies occur in the alteration zone and appear bedded, lentoid and veined, which share some similar occurrences.
The mine area is underlain mainly by Proterozoic volcanic–sedimentary sequences of the Wudang and Yaolinghe groups. The Wudang Group consists chiefly of intermediate- to felsic volcaniclastic-derived schists, including muscovite–albite schist, chlorite–epidote–albite schist, and albite leptynite. The Yaolinghe Group is dominated by intermediate- to mafic metavolcanic rocks, mainly actinolite–epidote–albite schist and chlorite–actinolite–epidote schist, and commonly contains epidote-rich segregations and locally preserved amygdaloidal textures. Gold mineralization is discontinuously developed along a ca. 4 km long corridor trending NW to NWW within strongly deformed greenschist-facies rocks.
Four blocks controlled by shear zones are recognized along strike, from northwest to southeast: Heilongtan, Wangjiawan, Xiejiagou, and Shizikou. In the Heilongtan block, 24 orebodies have been delineated, including 19 exposed and 5 concealed bodies, with estimated resources of ∼1.6 t Au and ∼46.8 t Ag. In the Wangjiawan, Xiejiagou, and Shizikou blocks, 18 gold orebodies have been identified, with estimated resources of ∼4.8 t Au and ∼23.4 t Ag. Ore grades vary markedly, ranging from 1.28 to 70.06 g/t Au (mean ∼3.66 g/t) and from 1 to 80 g/t Ag (mean ∼16.68 g/t). The ores also contain minor base metals, with mean contents of ∼0.12 wt% Cu, ∼0.01 wt% Pb, and ∼0.04 wt% Zn.
The three stages are defined as follows: quartz–sericite–pyrite stage (Stage I); quartz–pyrite stage (Stage II); quartz–polymetallic sulfide stage (Stage III).
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
19 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 |
| ⓘ | Weishanite | 1.AD.20a | (Au,Ag,Hg) |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite var. Gold-bearing Pyrite | 2.EB.05a | FeS2 |
| ⓘ | 2.EB.05a | FeS2 | |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Group 9 - Silicates | |||
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Actinolite | 9.DE.10 | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Monazite Group' | - | REE(PO4) |
| ⓘ | 'K Feldspar' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| O | Oxygen | |
| O | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Monazite Group | REE(PO4) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Mg | Magnesium | |
| Mg | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| P | Phosphorus | |
| P | ⓘ Monazite Group | REE(PO4) |
| S | Sulfur | |
| S | ⓘ Acanthite | Ag2S |
| S | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Covellite | CuS |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ti | Titanium | |
| Ti | ⓘ Rutile | TiO2 |
| Fe | Iron | |
| Fe | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Fe | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Ag | Silver | |
| Ag | ⓘ Acanthite | Ag2S |
| Ag | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Ag | ⓘ Native Silver | Ag |
| Ag | ⓘ Weishanite | (Au,Ag,Hg) |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| Au | Gold | |
| Au | ⓘ Native Gold var. Electrum | (Au,Ag) |
| Au | ⓘ Native Gold | Au |
| Au | ⓘ Weishanite | (Au,Ag,Hg) |
| Hg | Mercury | |
| Hg | ⓘ Weishanite | (Au,Ag,Hg) |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
AsiaContinent
Eurasian Plate
- Kunlun/South Qilian Fold BeltVolcanic Arc
- North China CratonOrogen
Yangtze PlateTectonic Plate
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References
Kamitani, M., Okumura, K., Teraoka, Y., Miyano, S., Watanabe, Y. (2007) Mineral Resources Map of East Asia, Geological Survey of Japan.
[1]Zhou, Jun-Jie; Li, Zhan-Ke; Yang, Mei-Zhen; Ke, Da; Zhao, Shao-Rui; Zong, Ke-Qing; Wang, Zaicong; Zu, Bo; Ding, Le-Le (2026) Multiple Au enrichment processes in the Early Cretaceous Heilongtan–Xiejiagou deposit, Tongbai Orogen, Central China. Ore Geology Reviews, 195. p.107421. doi:10.1016/j.oregeorev.2026.107421