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Kigom, Jos Plateau, Plateau, Nigeriai
| Regional Level Types | |
|---|---|
| Kigom | Complex |
| Jos Plateau | Plateau |
| Plateau | State |
| Nigeria | Country |
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Latitude & Longitude (WGS84):
9° 45' 50'' North , 8° 37' 31'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
A small pluton (6 km across) of alkali amphibole bearing and peralkaline granites belonging to the Younger Granites suite of Nigeria. Molybdenum mining took place intermittently since the 1940's.
The KGM Complex, located ∼26 km southwest of JBK, forms a ∼36 km2 circular intrusion. The earliest arfvedsonite granite occurs as a 3.2 km-long roof pendant within the dominant riebeckite granite, defining the complex’s ring structure. Three textural variants are distinguished by arfvedsonite-riebeckite crystal habits. Contacts are leucocratic and equigranular. The cycle concludes with aegirine microgranite intruding the western hills, flooring a depression with scree-obscured contacts.
The KGM Hills contains minor sub-economic pyrochlore in riebeckite granite. Mineralization manifests in three principal types: (1) silver-rich galena veins (>200 oz Ag/ton) in northern greisen, that follow an aplite dyke of Younger Granite origin, pinching and swelling to a maximum width of 8 in. over at least 70 yd in strike length; (2) molybdenite deposits at the granite's northern margin within poikilitic riebeckite facies. The molybdenum mineralization exhibits multiple styles within potassic-altered arfvedsonite-riebeckite granite, with vertical zonation from a Mo-bearing zone (7–10 cm wide) downward to a K-altered zone with Fe-oxide overprinting. and (3) a cassiterite-bearing quartz vein following a basaltic dike orientation 1.2 km north, with an abandoned mine shaft marking the most extensive Mo deposit.
The KGM Complex, located ∼26 km southwest of JBK, forms a ∼36 km2 circular intrusion. The earliest arfvedsonite granite occurs as a 3.2 km-long roof pendant within the dominant riebeckite granite, defining the complex’s ring structure. Three textural variants are distinguished by arfvedsonite-riebeckite crystal habits. Contacts are leucocratic and equigranular. The cycle concludes with aegirine microgranite intruding the western hills, flooring a depression with scree-obscured contacts.
The KGM Hills contains minor sub-economic pyrochlore in riebeckite granite. Mineralization manifests in three principal types: (1) silver-rich galena veins (>200 oz Ag/ton) in northern greisen, that follow an aplite dyke of Younger Granite origin, pinching and swelling to a maximum width of 8 in. over at least 70 yd in strike length; (2) molybdenite deposits at the granite's northern margin within poikilitic riebeckite facies. The molybdenum mineralization exhibits multiple styles within potassic-altered arfvedsonite-riebeckite granite, with vertical zonation from a Mo-bearing zone (7–10 cm wide) downward to a K-altered zone with Fe-oxide overprinting. and (3) a cassiterite-bearing quartz vein following a basaltic dike orientation 1.2 km north, with an abandoned mine shaft marking the most extensive Mo deposit.
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Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities21 valid minerals.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 3 - Halides | |||
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | 'Pyrochlore Group' | 4.00. | A2Nb2(O,OH)6Z |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Cassiterite | 4.DB.05 | SnO2 |
| Group 9 - Silicates | |||
| ⓘ | Fayalite | 9.AC.05 | Fe2+2(SiO4) |
| ⓘ | Thorite | 9.AD.30 | Th(SiO4) |
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Titanite | 9.AG.15 | CaTiO(SiO4) |
| ⓘ | Aegirine | 9.DA.25 | NaFe3+Si2O6 |
| ⓘ | Astrophyllite | 9.DC.05 | K2NaFe2+7Ti2[Si4O12]2O2(OH)4F |
| ⓘ | Arfvedsonite | 9.DE.25 | NaNa2(Fe2+4Fe3+)Si8O22(OH)2 |
| ⓘ | Riebeckite | 9.DE.25 | ◻Na2(Fe2+3Fe3+2)Si8O22(OH)2 |
| ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| ⓘ | Genthelvite | 9.FB.10 | Be3Zn4(SiO4)3S |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| H | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| H | ⓘ Riebeckite | ◻Na2(Fe32+Fe23+)Si8O22(OH)2 |
| Be | Beryllium | |
| Be | ⓘ Genthelvite | Be3Zn4(SiO4)3S |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | Oxygen | |
| O | ⓘ Aegirine | NaFe3+Si2O6 |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| O | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Cassiterite | SnO2 |
| O | ⓘ Fayalite | Fe22+(SiO4) |
| O | ⓘ Genthelvite | Be3Zn4(SiO4)3S |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Orthoclase | K(AlSi3O8) |
| O | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Riebeckite | ◻Na2(Fe32+Fe23+)Si8O22(OH)2 |
| O | ⓘ Thorite | Th(SiO4) |
| O | ⓘ Titanite | CaTiO(SiO4) |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Zircon | Zr(SiO4) |
| F | Fluorine | |
| F | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| F | ⓘ Fluorite | CaF2 |
| Na | Sodium | |
| Na | ⓘ Aegirine | NaFe3+Si2O6 |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Na | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| Na | ⓘ Riebeckite | ◻Na2(Fe32+Fe23+)Si8O22(OH)2 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)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 | ⓘ Orthoclase | K(AlSi3O8) |
| Si | Silicon | |
| Si | ⓘ Aegirine | NaFe3+Si2O6 |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Si | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Fayalite | Fe22+(SiO4) |
| Si | ⓘ Genthelvite | Be3Zn4(SiO4)3S |
| Si | ⓘ Orthoclase | K(AlSi3O8) |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Riebeckite | ◻Na2(Fe32+Fe23+)Si8O22(OH)2 |
| Si | ⓘ Thorite | Th(SiO4) |
| Si | ⓘ Titanite | CaTiO(SiO4) |
| Si | ⓘ Zircon | Zr(SiO4) |
| S | Sulfur | |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Galena | PbS |
| S | ⓘ Genthelvite | Be3Zn4(SiO4)3S |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| K | Potassium | |
| K | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Orthoclase | K(AlSi3O8) |
| Ca | Calcium | |
| Ca | ⓘ Fluorite | CaF2 |
| Ca | ⓘ Titanite | CaTiO(SiO4) |
| Ti | Titanium | |
| Ti | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Titanite | CaTiO(SiO4) |
| Fe | Iron | |
| Fe | ⓘ Aegirine | NaFe3+Si2O6 |
| Fe | ⓘ Arfvedsonite | NaNa2(Fe42+Fe3+)Si8O22(OH)2 |
| Fe | ⓘ Astrophyllite | K2NaFe72+Ti2[Si4O12]2O2(OH)4F |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Fayalite | Fe22+(SiO4) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Riebeckite | ◻Na2(Fe32+Fe23+)Si8O22(OH)2 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Zn | Zinc | |
| Zn | ⓘ Genthelvite | Be3Zn4(SiO4)3S |
| Zn | ⓘ Sphalerite | ZnS |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Nb | Niobium | |
| Nb | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| Sn | Tin | |
| Sn | ⓘ Cassiterite | SnO2 |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
| Th | Thorium | |
| Th | ⓘ Thorite | Th(SiO4) |
Localities in this Region
- Plateau
- Jos Plateau
Other Regions, Features and Areas containing this locality
AfricaContinent
African PlateTectonic Plate
- Tuareg Shield
- LATEA MetacratonVolcanic Arc
West AfricaUN Subregion
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References
[1]Kamaunji, Vandi Dlama; Ahmed, Hafizullah Abba; Wang, Lian-Xun; Sanislav, Ioan V.; Girei, Musa Bala; Zhu, Yu-Xiang; Liang, Xin-xin; Chen, Xin; Sami, Mabrouk (2026) Progressive mantle melting and crust–mantle–fluid hybridization in fluorite-bearing Sn–Nb ± Mo-rich alkaline granites of the Jos Plateau, central Nigeria. Ore Geology Reviews, 195. p.107405. doi:10.1016/j.oregeorev.2026.107405




Kigom, Jos Plateau, Plateau, Nigeria