Implicating the Origin and Depositional Environment of Banded Iron Formation (BIF) of Bonai-Keonjhar Iron Ore Belt in Eastern India from its Petrography and Geochemistry

[1] Alexander B. W.(2008)Bau, M., Andersson, P., and Dulski, P., Continentally-derived solutes in shallow Archean sea water: Rare earth element and Nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa Geochim. Cosmochim. Acta 72 378-394

[2] Appel P.(1983)Rare earth elements in the early ArcheanIsua iron-formation, W.Greenland J. Precambrian Geol. 20 243-258

[3] Banerji A. K.(1977)On the Precambrian banded iron formation and manganese ores of Singhbhum region, Eastern India Econ. Geol. 72 90-98

[4] Basta F. F.(2011)Petrology and geochemistry of banded iron formation (BIF) of WadiKarim and Um Anab, Eastern Desert, Egypt: implications for the origin of Neoproterozoic BIF Precambrian Res. 187 277-292

[5] Maurice A. E.(1996)Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa Precambrian Res. 79 37-55

[6] Fontbote L.(1999)Comparing yttrium and rare earths in hydrothermal fluids from Mid-Atlantic Ridge; implications for Y and REE behaviour during near vent mixing and for the Y/Ho ratio of Proterozoic seawater Chem. Geol. 155 77-90

[7] Favarger P.(2016)Field Relationship among the three iron ore groups of iron ore super group encircling the North Odisha iron ore craton, India: a comparison study J. Geosci. Geomat. 4 53-60

[8] Bau M.(2007)Geochemistry of some banded iron-formations of the Archean supracrustals, Jharkhand–Orissa region, India J. Earth System Sci. 3 245-259

[9] Dulski P.(2004)Characterization of Early Archean chemical sediments by trace element signatures Earth Planet. Sci. Lett. 222 43-60

[10] Bau M.(1975)Metallogenesis at oceanic spreading centers Annu.Rev.Earth Planet.Sci. 3 401-433

[1] Alexander B. W.(2008)Bau, M., Andersson, P., and Dulski, P., Continentally-derived solutes in shallow Archean sea water: Rare earth element and Nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa Geochim. Cosmochim. Acta 72 378-394

[2] Appel P.(1983)Rare earth elements in the early ArcheanIsua iron-formation, W.Greenland J. Precambrian Geol. 20 243-258

[3] Banerji A. K.(1977)On the Precambrian banded iron formation and manganese ores of Singhbhum region, Eastern India Econ. Geol. 72 90-98

[4] Basta F. F.(2011)Petrology and geochemistry of banded iron formation (BIF) of WadiKarim and Um Anab, Eastern Desert, Egypt: implications for the origin of Neoproterozoic BIF Precambrian Res. 187 277-292

[5] Maurice A. E.(1996)Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa Precambrian Res. 79 37-55

[6] Fontbote L.(1999)Comparing yttrium and rare earths in hydrothermal fluids from Mid-Atlantic Ridge; implications for Y and REE behaviour during near vent mixing and for the Y/Ho ratio of Proterozoic seawater Chem. Geol. 155 77-90

[7] Favarger P.(2016)Field Relationship among the three iron ore groups of iron ore super group encircling the North Odisha iron ore craton, India: a comparison study J. Geosci. Geomat. 4 53-60

[8] Bau M.(2007)Geochemistry of some banded iron-formations of the Archean supracrustals, Jharkhand–Orissa region, India J. Earth System Sci. 3 245-259

[9] Dulski P.(2004)Characterization of Early Archean chemical sediments by trace element signatures Earth Planet. Sci. Lett. 222 43-60

[10] Bau M.(1975)Metallogenesis at oceanic spreading centers Annu.Rev.Earth Planet.Sci. 3 401-433