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Mosaboni Mine, Mosaboni, East Singhbhum District, Jharkhand, Indiai
| Regional Level Types | |
|---|---|
| Mosaboni Mine | Mine |
| Mosaboni | Census Area |
| East Singhbhum District | District |
| Jharkhand | State |
| India | Country |
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Latitude & Longitude (WGS84):
22° 33' 57'' North , 86° 26' 16'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
A copper mine owned by ICC (Indian Copper Co.). This mine has a capacity of 1 million tons/year ore.
Produces uranium as a by-product.
In the Mosaboni mine, operated by the Indian Copper Corporation Ltd., two roughly parallel lode zones dipping ENE are worked over a strike length of about 3 miles and to a depth of about 2,700 feet. In the early period of mining these lode zones were named West Lode and Main Lode. Later work has proved that the West Lode is richer and more persistent than the Main Lode, which pinched out near the 18th level (about 2,000 feet below surface) in the main shaft section of this mine. In this section, the distance of separation of the two lodes gradually diminishes with depth and they become almost parallel to each other near the 15th level. The average distance between the lodes is about 80 feet and they are generally 6 to'8 feet in width. Both the lodes are confined within the soda-granites and highly feldspathic schists. Three different types of sulfide ores are generally present within the lode zones, namely massive ore, braided ore, and disseminated ore. Massive ores have been formed by closely spaced veins, pockets, and lenses. In places the original structural controls are obliterated by ore. Braided ores are present where mineralization was controlled by closely spaced S• and Sa planes. In this type of ore, the feeder channels along the structural planes are preserved. Disseminated ores generally occur within sheared epidiorites and feldspathic schists away from the main lode zones.
Located about 6 miles from Moubhandar.
Produces uranium as a by-product.
In the Mosaboni mine, operated by the Indian Copper Corporation Ltd., two roughly parallel lode zones dipping ENE are worked over a strike length of about 3 miles and to a depth of about 2,700 feet. In the early period of mining these lode zones were named West Lode and Main Lode. Later work has proved that the West Lode is richer and more persistent than the Main Lode, which pinched out near the 18th level (about 2,000 feet below surface) in the main shaft section of this mine. In this section, the distance of separation of the two lodes gradually diminishes with depth and they become almost parallel to each other near the 15th level. The average distance between the lodes is about 80 feet and they are generally 6 to'8 feet in width. Both the lodes are confined within the soda-granites and highly feldspathic schists. Three different types of sulfide ores are generally present within the lode zones, namely massive ore, braided ore, and disseminated ore. Massive ores have been formed by closely spaced veins, pockets, and lenses. In places the original structural controls are obliterated by ore. Braided ores are present where mineralization was controlled by closely spaced S• and Sa planes. In this type of ore, the feeder channels along the structural planes are preserved. Disseminated ores generally occur within sheared epidiorites and feldspathic schists away from the main lode zones.
Located about 6 miles from Moubhandar.
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
17 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ 'Apatite' Formula: Ca5(PO4)3A |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ 'Chlorite Group' |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Mackinawite Formula: FeS |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Millerite Formula: NiS |
| ⓘ Molybdenite Formula: MoS2 |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Pentlandite Formula: (NixFey)Σ9S8 |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Pyrrhotite Formula: Fe1-xS |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Skutterudite Formula: CoAs3 |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ Tellurobismuthite Formula: Bi2Te3 |
| ⓘ Tetradymite Formula: Bi2Te2S |
| ⓘ Violarite Formula: Fe2+Ni3+2S4 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Millerite | 2.CC.20 | NiS |
| ⓘ | Mackinawite | 2.CC.25 | FeS |
| ⓘ | Violarite | 2.DA.05 | Fe2+Ni3+2S4 |
| ⓘ | Tellurobismuthite | 2.DC.05 | Bi2Te3 |
| ⓘ | Tetradymite | 2.DC.05 | Bi2Te2S |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Skutterudite | 2.EC.05 | CoAs3 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 9 - Silicates | |||
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Apatite' | - | Ca5(PO4)3A |
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 | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | Oxygen | |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| 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 | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| 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 | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| 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 | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| P | Phosphorus | |
| P | ⓘ Apatite | Ca5(PO4)3A |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Mackinawite | FeS |
| S | ⓘ Millerite | NiS |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pentlandite | (NixFey)Σ9S8 |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tetradymite | Bi2Te2S |
| S | ⓘ Violarite | Fe2+Ni23+S4 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| 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 | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Mackinawite | FeS |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Violarite | Fe2+Ni23+S4 |
| Co | Cobalt | |
| Co | ⓘ Skutterudite | CoAs3 |
| Ni | Nickel | |
| Ni | ⓘ Millerite | NiS |
| Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Ni | ⓘ Violarite | Fe2+Ni23+S4 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| As | Arsenic | |
| As | ⓘ Skutterudite | CoAs3 |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| Te | Tellurium | |
| Te | ⓘ Tellurobismuthite | Bi2Te3 |
| Te | ⓘ Tetradymite | Bi2Te2S |
| Bi | Bismuth | |
| Bi | ⓘ Tellurobismuthite | Bi2Te3 |
| Bi | ⓘ Tetradymite | Bi2Te2S |
Other Regions, Features and Areas containing this locality
AsiaContinent
India
- Jharkhand
- ⭔Kolhan DivisionDivision
Indian PlateTectonic Plate
- Singhbhum CratonCraton
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References
[1]Changkakoti, A., Gray, J., Morton, R. D., Sarkar, S. N. (1987) The Mosaboni copper deposit, India; a preliminary study on the nature and genesis of the ore-fluids. Economic Geology, 82 (6) 1619-1625 doi:10.2113/gsecongeo.82.6.1619
Nayak, B. K., Panchapakesan, V. (1990) Geothermic Control of Ore Assay in Mosaboni Mine, Singhbhum-Evidences from Fluid Inclusions. Journal Geological Society of India, 36 (2). 187-194 doi:10.17491/jgsi/1990/360209
Nayak, B. K., Panchapakesan, V. (1991) Thermodynamics and Oxygen-Sulpbur Fugacity Variations of Mosaboni Sulphide Mineralisation, Singhbhum, Bibar. Journal Geological Society of India, 37 (1). 39-46 doi:10.17491/jgsi/1991/370105