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Marlagalla-Allapatna, Mandya District, Karnataka, Indiai
| Regional Level Types | |
|---|---|
| Marlagalla-Allapatna | Pegmatite Field |
| Mandya District | District |
| Karnataka | State |
| India | Country |
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Latitude & Longitude (WGS84):
12° 25' 0'' North , 76° 44' 30'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
The pegmatite field contains more than 50 pegmatites with variable size and mineralogy. Sarbajna & Krishnamurthy (1994) describes the following types:
Type I: Unzoned perthite-mica pegmatites.
These pegmatites are typically vein like (1-10m long and 0.1 to 1 m wide). They are unzoned with quartz, microcline perthite, biotite or muscovite with magnetite. This type is most common near Gudahalli-gananguru and in areas north of Chikkopal.
Type II: Partly zoned muscovite-beryl pegmatites.
These pegmatites are typically 10-50m long and 1-2m wide. They are partly zoned with a quartz core surrounded by intergrown quartz, feldspar and muscovite. Beryl and small amounts of columbite-tantalite occurs in the quartz/feldspar zone. This type occurs 150m north of Marlagalla.
Type III: Zoned muscovite-microcline pegmatites with spodumente
The pegmatites are larger lensoids. They are 10 to 80m long and 3-5 m wide. Zoning is fairly pronounced with a central quartz core which in most cases are surrounded by a well developed zone of spodumene crystals. Thereafter comes an intermediate intermediate zone of K-feldspar and albite, followed by an albite and muscovite zone. The border zone is weathered and not well preserved.
Type IV: Pegmatites with albite replacement of spodumene.
These pegmatites exhibit a complex zonation in which spodumene has partly been replaced by albite. The pegmatites also contains columbite and tantalite. They are emplaced in schistose rocks near Marlagalla.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) |
| ⓘ Beryl Formula: Be3Al2(Si6O18) References: Sarbajna, Chanchal; Sinha, R. P.; Krishnamurthy, P.; Krishna, K. V. G.; Viswanathan, R.; Banerjee, D. C. (1999) Mineralogy and Geochemistry of Alkali Beryl from the Rare Metal Bearing Pegmatites of Marlagalla-Allapatna, Mandya District, Karnataka. Journal Geological Society of India, 54 (6). 599-608 doi:10.17491/jgsi/1999/540603 |
| ⓘ Beryl var. Alkali-beryl Formula: Be3Al2(Si6O18) References: Sarbajna, Chanchal; Sinha, R. P.; Krishnamurthy, P.; Krishna, K. V. G.; Viswanathan, R.; Banerjee, D. C. (1999) Mineralogy and Geochemistry of Alkali Beryl from the Rare Metal Bearing Pegmatites of Marlagalla-Allapatna, Mandya District, Karnataka. Journal Geological Society of India, 54 (6). 599-608 doi:10.17491/jgsi/1999/540603 |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ Columbite-(Fe) Formula: Fe2+Nb2O6 Description: 6 of 8 columbite-tantalite samples analysed by Sarbajna et al. (2000) are dominantly columbite-(Fe), but the crystals are heavily zoned and the core or rim may be another mineral in the group. References: |
| ⓘ Columbite-(Mn) Formula: Mn2+Nb2O6 Description: Columbite-(Fe) is the dominant columbite-tantalite mineral at this locality, but 1 of 8 samples analysed by Sarbajna et al.(2000) has a distinct columbite-(Mn) core. References: |
| ⓘ 'Columbite-Tantalite' Description: Sarbajna et al. (2000) presents 79 analyses of 8 columbite-tantalite specimens and show that they are heavily zoned, with both Fe/Mn and Nb/Ta dominant zones. Their results indicate that columbite-(Fe) is the dominant mineral in this group with 62 of 79 analyses, 4 analyses corresponds to columbite-(Mn), 4 analyses corresponds to tantalite-(Mn) and 9 analyses corresponds to tantalite-(Fe). References: |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Microcline Formula: K(AlSi3O8) |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Spodumene Formula: LiAlSi2O6 References: |
| ⓘ Tantalite-(Fe) Formula: Fe2+Ta2O6 Description: Columbite-(Fe) is the dominant columbite-tantalite mineral at this locality, but 2 of 8 samples analysed by Sarbajna et al.(2000) show distinct tantalite-(Fe) zones. References: |
| ⓘ Tantalite-(Mn) Formula: Mn2+Ta2O6 Description: Columbite-(Fe) is the dominant columbite-tantalite mineral at this locality, but 2 of 8 samples analysed by Sarbajna et al.(2000) show distinct tantalite-(Mn) zones. References: |
| ⓘ 'Tourmaline' Formula: AD3G6(T6O18)(BO3)3X3Z |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Columbite-(Fe) | 4.DB.35 | Fe2+Nb2O6 |
| ⓘ | Tantalite-(Fe) | 4.DB.35 | Fe2+Ta2O6 |
| ⓘ | Columbite-(Mn) | 4.DB.35 | Mn2+Nb2O6 |
| ⓘ | Tantalite-(Mn) | 4.DB.35 | Mn2+Ta2O6 |
| Group 9 - Silicates | |||
| ⓘ | Beryl var. Alkali-beryl | 9.CJ.05 | Be3Al2(Si6O18) |
| ⓘ | 9.CJ.05 | Be3Al2(Si6O18) | |
| ⓘ | Spodumene | 9.DA.30 | LiAlSi2O6 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Columbite-Tantalite' | - | |
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 | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Li | Lithium | |
| Li | ⓘ Spodumene | LiAlSi2O6 |
| Be | Beryllium | |
| Be | ⓘ Beryl var. Alkali-beryl | Be3Al2(Si6O18) |
| Be | ⓘ Beryl | Be3Al2(Si6O18) |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Beryl var. Alkali-beryl | Be3Al2(Si6O18) |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Beryl | Be3Al2(Si6O18) |
| O | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
| O | ⓘ Tantalite-(Fe) | Fe2+Ta2O6 |
| O | ⓘ Columbite-(Mn) | Mn2+Nb2O6 |
| O | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Microcline | K(AlSi3O8) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Spodumene | LiAlSi2O6 |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| 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) |
| 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 | ⓘ Beryl var. Alkali-beryl | Be3Al2(Si6O18) |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Beryl | Be3Al2(Si6O18) |
| Al | ⓘ Microcline | K(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Spodumene | LiAlSi2O6 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Beryl var. Alkali-beryl | Be3Al2(Si6O18) |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Beryl | Be3Al2(Si6O18) |
| Si | ⓘ Microcline | K(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Spodumene | LiAlSi2O6 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Microcline | K(AlSi3O8) |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mn | Manganese | |
| Mn | ⓘ Columbite-(Mn) | Mn2+Nb2O6 |
| Mn | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
| Fe | ⓘ Tantalite-(Fe) | Fe2+Ta2O6 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Nb | Niobium | |
| Nb | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
| Nb | ⓘ Columbite-(Mn) | Mn2+Nb2O6 |
| Ta | Tantalum | |
| Ta | ⓘ Tantalite-(Fe) | Fe2+Ta2O6 |
| Ta | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
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References
Banerjee, D. C.; Krishna, K. V. G.; Murthy, G. V. G. K.; Srivastava, S. K.; Sinha, R. P. (1994) Occurrence of Spodumene in the Rare Metal-Bearing Pegmatites of Mariagalla-Allapatna Area, Mandya Dist., Karnataka. Journal Geological Society of India, 44 (2). 127-139 doi:10.17491/jgsi/1994/440203
Sarbajna, Chanchal; Sinha, R. P.; Krishnamurthy, P.; Krishna, K. V. G.; Viswanathan, R.; Banerjee, D. C. (1999) Mineralogy and Geochemistry of Alkali Beryl from the Rare Metal Bearing Pegmatites of Marlagalla-Allapatna, Mandya District, Karnataka. Journal Geological Society of India, 54 (6). 599-608 doi:10.17491/jgsi/1999/540603