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Characteristics of Manganite (γ-MnOOH) in Manganese-Rich Gangpur Group of Rocks, Orissa


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1 Mineralogy and Metallography Division, Regional Research Laboratory, Bhubaneswar - 751 013, India
     

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Manganite γ-MnOOH, in the manganese-rich rocks of Precambrian Gangpur Group, Sundargarh district, Orissa, shows dissimilar fabrics and belongs to three generations but has more or less similar chemical composition. It occurs as patchy inclusions, accicular crystallites, egg-shaped micro-nodules, medium to coarse-grained mosaics, vein and fissure fillings and as wedge-shaped linings. The manganite is either formed froin Mn-oxide (jacobsite and vredenburgite) phases through retrogressive metamorphic transformation (Ma1) or generated through pseudomorphic replacement of Mn-sillicate (rhodonite and tcphroite) or Mn-carbonate (rhodochrosite) by chemical weathering under supergene conditions (Ma2). The vein filling type is the latest in its paragenesis (Ma3). Despite different mineral lineages, manganites are chemically similar though crystallites located in veins and fissures are relatively pure.

Keywords

Economic Geology, Manganite, Manganese, Gangpur Group, Orissa.
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  • Characteristics of Manganite (γ-MnOOH) in Manganese-Rich Gangpur Group of Rocks, Orissa

Abstract Views: 205  |  PDF Views: 2

Authors

B. K. Mohapatra
Mineralogy and Metallography Division, Regional Research Laboratory, Bhubaneswar - 751 013, India
B. R. Nayak
Mineralogy and Metallography Division, Regional Research Laboratory, Bhubaneswar - 751 013, India

Abstract


Manganite γ-MnOOH, in the manganese-rich rocks of Precambrian Gangpur Group, Sundargarh district, Orissa, shows dissimilar fabrics and belongs to three generations but has more or less similar chemical composition. It occurs as patchy inclusions, accicular crystallites, egg-shaped micro-nodules, medium to coarse-grained mosaics, vein and fissure fillings and as wedge-shaped linings. The manganite is either formed froin Mn-oxide (jacobsite and vredenburgite) phases through retrogressive metamorphic transformation (Ma1) or generated through pseudomorphic replacement of Mn-sillicate (rhodonite and tcphroite) or Mn-carbonate (rhodochrosite) by chemical weathering under supergene conditions (Ma2). The vein filling type is the latest in its paragenesis (Ma3). Despite different mineral lineages, manganites are chemically similar though crystallites located in veins and fissures are relatively pure.

Keywords


Economic Geology, Manganite, Manganese, Gangpur Group, Orissa.