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Mianhuakeng U deposit (U deposit No. 305), Changjiang Uranium ore field (Uranium ore field No. 211), Renhua Co., Shaoguan, Guangdong, Chinai
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Latitude & Longitude (WGS84):
25° 12' 11'' North , 113° 46' 14'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Low temperature hydrothermal uranium deposit, hosted in granite within a fracture zone.
This deposit has been mined out.
(302 deposit?)
Notably, the vertical distribution of uranium mineralization spans a considerable range, extending from the surface (elevation 500 m) to depths (elevation −900 m). The uranium ores can be classified into two types: (1) reddened alteration ore, characterized by iron oxides/hydroxides formed during fluid-granite interactions, with a mineral assemblage of pitchblende, coffinite, brannerite, reddish microcrystalline quartz, hematite and chlorite; (2) gray-black ore, composed of pitchblende, coffinite, gray-black microcrystalline quartz, pyrite, fluorite, and calcite. Hydrothermal alteration of the Mianhuakeng uranium deposit can be divided into two distinct types: firstly high temperature alterations and secondly medium to low-temperature alterations. The high temperature alteration type mainly includes albitization and potassic feldspathization, while the medium to low-temperature alteration mainly involves fluoritization, silicification, hematization, sericitization, chloritization, pyritization and carbonatation. In the medium to low-temperature alterations, there is a close relationship between silicification, hematization, pyritization as well as fluoritization and uranium mineralization. Four episodes of uranium metallogenic activities have been dated: approximately 120 Ma, 102 Ma, 92–90 Ma, and 68–60 Ma.
The primary types of mineralization in the deposit consist of silicification zone-type and fractured rock-type mineralization, with fewer instances of intersection-type uranium mineralization occurring at the junctions of mafic dykes and fault zones.
This deposit has been mined out.
(302 deposit?)
Notably, the vertical distribution of uranium mineralization spans a considerable range, extending from the surface (elevation 500 m) to depths (elevation −900 m). The uranium ores can be classified into two types: (1) reddened alteration ore, characterized by iron oxides/hydroxides formed during fluid-granite interactions, with a mineral assemblage of pitchblende, coffinite, brannerite, reddish microcrystalline quartz, hematite and chlorite; (2) gray-black ore, composed of pitchblende, coffinite, gray-black microcrystalline quartz, pyrite, fluorite, and calcite. Hydrothermal alteration of the Mianhuakeng uranium deposit can be divided into two distinct types: firstly high temperature alterations and secondly medium to low-temperature alterations. The high temperature alteration type mainly includes albitization and potassic feldspathization, while the medium to low-temperature alteration mainly involves fluoritization, silicification, hematization, sericitization, chloritization, pyritization and carbonatation. In the medium to low-temperature alterations, there is a close relationship between silicification, hematization, pyritization as well as fluoritization and uranium mineralization. Four episodes of uranium metallogenic activities have been dated: approximately 120 Ma, 102 Ma, 92–90 Ma, and 68–60 Ma.
The primary types of mineralization in the deposit consist of silicification zone-type and fractured rock-type mineralization, with fewer instances of intersection-type uranium mineralization occurring at the junctions of mafic dykes and fault zones.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
18 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 | |||
|---|---|---|---|
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 3 - Halides | |||
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | var. Microcrystalline quartz | 4.DA.05 | SiO2 |
| ⓘ | Brannerite | 4.DH.05 | UTi2O6 |
| ⓘ | Uraninite var. Pitchblende | 4.DL.05 | UO2 |
| ⓘ | 4.DL.05 | UO2 | |
| ⓘ | Goethite | 4.FD.10 | Fe3+O(OH) |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Group 9 - Silicates | |||
| ⓘ | Coffinite | 9.AD.30 | U(SiO4) · nH2O |
| ⓘ | Thorite | 9.AD.30 | Th(SiO4) |
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Thorite var. Uranothorite | 9.AD.30 | (Th,U)SiO4 |
| ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
| ⓘ | 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 |
| ⓘ | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'K Feldspar' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Coffinite | U(SiO4) · nH2O |
| H | ⓘ Goethite | Fe3+O(OH) |
| H | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| H | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Brannerite | UTi2O6 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Coffinite | U(SiO4) · nH2O |
| O | ⓘ Diopside | CaMgSi2O6 |
| O | ⓘ Goethite | Fe3+O(OH) |
| 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 | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Uraninite var. Pitchblende | UO2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Thorite | Th(SiO4) |
| O | ⓘ Uraninite | UO2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Thorite var. Uranothorite | (Th,U)SiO4 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| F | ⓘ Fluorite | CaF2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | ⓘ Diopside | CaMgSi2O6 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Al | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Coffinite | U(SiO4) · nH2O |
| Si | ⓘ Diopside | CaMgSi2O6 |
| Si | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Si | ⓘ Kaolinite | Al2(Si2O5)(OH)4 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Thorite | Th(SiO4) |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Thorite var. Uranothorite | (Th,U)SiO4 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| S | Sulfur | |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| 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 | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Diopside | CaMgSi2O6 |
| Ca | ⓘ Fluorite | CaF2 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Brannerite | UTi2O6 |
| Fe | Iron | |
| Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
| Th | Thorium | |
| Th | ⓘ Thorite | Th(SiO4) |
| Th | ⓘ Thorite var. Uranothorite | (Th,U)SiO4 |
| U | Uranium | |
| U | ⓘ Brannerite | UTi2O6 |
| U | ⓘ Coffinite | U(SiO4) · nH2O |
| U | ⓘ Uraninite var. Pitchblende | UO2 |
| U | ⓘ Uraninite | UO2 |
| U | ⓘ Thorite var. Uranothorite | (Th,U)SiO4 |
Other Regions, Features and Areas containing this locality
AsiaContinent
China
- Nanling metallogenic beltMineral Belt
- Southern China Li Mineral BeltMineral Belt
Eurasian Plate
- West CathaysiaOrogenic Belt
- Zhuguangshan U districtMining District
Yangtze PlateTectonic Plate
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References
Dahlkamp, Franz J. (2009) Uranium Deposits of the World - Asia. Springer Berlin Heidelberg. doi:10.1007/978-3-540-78558-3pp.31-156
DeHai, WU; Fei, XIA; JiaYong, PAN; GuoQi, LIU; GuoLong, HUANG; WenQuan, LIU; JianYong, WU (2019) Characteristics of hydrothermal alteration and material migration of Mianhuakeng uranium deposit in northern Guangdong Province. Acta Petrologica Sinica, 35 (9). p.2745-2764. doi:10.18654/1000-0569/2019.09.08
JiaMing, QI; Ba, ZHU; JianYong, WU; HaoJie, CAO; WenQuan, LIU; ZhengQi, XU (2019) The evolution of ore-forming fluid and its constraint on mineralization process in Mianhuakeng uranium deposit, northern Guangdong, China. Acta Petrologica Sinica, 35 (9). p.2711-2726. doi:10.18654/1000-0569/2019.09.06
Lan, Qing, Fu, Shanling, Lin, Jinrong (2022) Characteristics of Mineralization-Forming Fluid and Metallogenic Mechanism for the Mianhuakeng Uranium Deposit in South China: Constraints from In Situ Geochemical Signatures and Sulfur Isotopes of Syn-Mineralization Pyrite and Pitchblende. Minerals, 12 (2) 227 doi:10.3390/min12020227
Zhong, Fujun; Zhang, Xiaotian; Wang, Kaixing; Wu, Bin; Liu, Jungang; Pan, Jiayong; Xia, Fei (2023) Genesis of the Mianhuakeng granite-related uranium deposit, South China: Insights from cathodoluminescence imaging, fluid inclusions, and trace elements composition of hydrothermal quartz. Ore Geology Reviews, 154. 105308 doi:10.1016/j.oregeorev.2023.105308
[1]Liu, Bin; Chen, Weifeng; Wei, Wenfang; Qi, Jiaming; Ye, Yongqin; Ling, Hongfei (2025) Geochemistry of iron oxides in the Mianhuakeng uranium deposit in South China: Implications for uranium mineralization genesis and prospecting. Ore Geology Reviews, 187. 106950 doi:10.1016/j.oregeorev.2025.106950