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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=22462"><dc:title>Mineralogy, geochemistry and genesis of low-grade manganese ores of Anujurhi area, Eastern Ghats, India</dc:title><dc:creator>Pattnaik,	Sujata	(Avtor)
	</dc:creator><dc:creator>Majhi,	Satrughan	(Avtor)
	</dc:creator><dc:subject>Eastern Ghats Mobile Belt (EGMB)</dc:subject><dc:subject>Anujurhi</dc:subject><dc:subject>manganese ore</dc:subject><dc:subject>supergene enrichment</dc:subject><dc:description>The  Anujurhi  manganese  ores  occur  in  the  high-grade  gneisses  of  the  Precambrian  Eastern  Ghats  Supergroup  in  Odisha,  India.  They  are  characterized  by  conformable  lenses  containing  minerals  such  as  cryptomelane,  romanechite,  pyrolusite, todorokite, and pyrophanite, along with other opaque minerals like graphite, goethite and ilmenite. The gangue minerals associated with these ores include quartz, feldspar, garnet, kaolinite, apatite, sillimanite, zircon, biotite, alunite, and gorceixite. The primary elements present in the ore, Si, Mn, Fe, and Al, average at 16.20 %, 15.06 %, 11.94 %, and 6.6  %  respectively.  Additionally,  trace  amounts  of  P,  K,  Ti,  Mg,  Ca,  and  Na  were  detected.  The  average  Fe/Mn  ratio  of  0.81  and  the  Si  versus  Al  plot  of  the  Anujurhi  manganese  ores  suggest  a  hydrogenous-hydrothermal  mixed  source  for  the ferromanganese sediments. The characteristics of the manganese ore bands, absence of carbonate facies of ore, and geochemical association of Mn-Ba together with Na/Mg ratios and CaO-Na2O-MgO ternary plot of the manganese ores strongly  indicate  that  the  mineralization  is  a  metamorphosed  shallow  marine-lacustrine  deposit.  Following  deposition  and diagenesis, the manganese minerals underwent at least two phases of Ultra High Temperature (UHT) and granulite facies metamorphism along with the host rocks. Tectonic uplift, erosion, extended exposure to atmospheric oxygen and percolation of meteoric water led to the supergene alteration and remobilization of the primary manganese minerals in a colloidal state, followed by epigenetic replacement along the structural weak planes of the granulite facies rocks, resulting in the formation of the current deposits. This is evidenced by the observed secondary replacement and colloidal textures in the Mn oxides.</dc:description><dc:date>2024</dc:date><dc:date>2025-05-21 09:20:11</dc:date><dc:type>Neznano</dc:type><dc:identifier>22462</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
