A Study of Banded Hematite Quartzite (BHQ) in Mallasamudra Area, Gadag Schist Belt, Karnataka, India

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Authors

  • Department of Civil Engineering, BMS Institute of Technology and Management, Yelahanka, Bangalore - 560064, Karnataka ,IN
  • Department of Geology, School of Earth Sciences, Central University of Karnataka, Kalaburagi - 585367, Karnataka ,IN
  • Department of Civil Engineering, Government Engineering College Raichur - 584135, Karnataka ,IN
  • Department of Civil Engineering, Vijaya Vittala Institute of Technology, Bangalore - 560077, Karnataka ,IN ORCID logo https://orcid.org/0009-0005-4280-7050

DOI:

https://doi.org/10.18311/jmmf/2023/35225

Keywords:

Banded Hematite Quartzite (BHQ), Banded Iron Formation (BIF), Gadag Schist Belt (GSB), Geochemistry, Low-Grade Iron Ore, Mallasamudra

Abstract

Mineral raw material plays a very important role in the manufacturing industry as well as the country's economic growth. The iron ore, especially the Banded Iron Formations (BIFs) are unique rock formations in geological history. The Mallasamudra area, Gadag Schist Belt (GSB), is having good exposures of iron ores. Most of the outcrops of BHQ are located on the top of the hills whereas metabasalts occur on either side of the hills in the area. The BHQ were delineated during field mapping. In the Banded Hematite Quartzite (BHQ) of Mallasamudra area, SiO2 varies from 48.22% to 52.12% and Fe2O3 varies from 29.23% to 33.21% indicating that the BHQ is of low-grade.

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Published

2023-12-01

How to Cite

Agasnalli, C., Lakkundi, T. K., Natikar, R. D., & Nerlikar, D. (2023). A Study of Banded Hematite Quartzite (BHQ) in Mallasamudra Area, Gadag Schist Belt, Karnataka, India. Journal of Mines, Metals and Fuels, 71(12), 2426–2432. https://doi.org/10.18311/jmmf/2023/35225
Received 2023-09-28
Accepted 2024-01-10
Published 2023-12-01

 

References

Naqvi SM, Rogers JJW. Precambrian Geology of India. Oxford Monographs on Geology and Geophysics No.6. New York: Oxford University Press; 1987. p. 223.

Rajamani V, Shivkumar K, Hanson, GN, Shirey SB. Geochemistry and Petrogenesis of Amphibolites, Kolar Schist Belt, South India: Evidence for Komatiitic Magma Derived by Low Percentages of Melting of the Mantle. Journal of Petrology. 1985; 26(1):92-123. https://doi.org/10.1093/petrology/26.1.92 DOI: https://doi.org/10.1093/petrology/26.1.92

Ramachandran TV, Beeraiah MB, Sengupta S. Exploration for Auriferous Ore Zones in Gadag Schist Belt, Karnataka. Some aspects of mineral development in India. Visakhapatnam: Geological Society of India and Geology Department, Andhra University; 2001. p. 53-66.

Beeraiah MB, Sengupta S, Venkateswamy, Ramachandran TV. Exploration for Gold in Sulphidic Banded Magnetite Chert of Nagavi-Mallasamudra area, Gadag Schist Belt. Special Publication Series - Geological Survey of India. 2001; 58:339-43.

Puranik SC. Primary Sedimentary Structures in Banded Iron Formations from Gadag Schist Belt, Karnataka, India. International Journal of Earth Science and Engineering. 2011; 4(2):111-21.

Agasnalli C, Basavanna M, Lakkundi TK. Geochemistry of Banded Iron Formations and associated Gold Mineralisation of Nagavi, Gadag Schist Belt, Karnataka. International Journal of Earth Sciences and Engineering. 2015; 8(4):1880-6.

Gross GA. Primary Features in Cherty Iron-Formations, Sedimentary Geology. 1972; 7(4):241-61. https://doi.org/10.1016/0037-0738(72)90024-3 DOI: https://doi.org/10.1016/0037-0738(72)90024-3

Ramadass G, Ramaprasada Rao IB, Himabindu D, Srinivasulu N. Pseudo-surface Velocities (densities) and Pseudo-depth Densities (velocities) along selected parts in the Dharwar Craton, India. Current Science. 2002; 82(2):197-202. https://www.currentscience.ac.in/Volumes/82/02/0197.pdf

Agasnalli C, Ramalingam J, Lakkundi TK, Deepak MS. A Study of Structural Controls on Gold Mineralisation in Nagavi area, Gadag Schist Belt, Karnataka, India. Journal of Mines, Metals and Fuels. 2022; 70(11).

Naqvi SM, Rana Prathap JG. Geochemistry of Adakites from Neoarchean Active Continental Margin of Shimoga Schist Belt, Western Dharwar Craton, India: Implications for the Genesis of TTG. Precambrian Research. 2007; 156(1-2):32-54. https://doi.org/10.1016/j.precamres.2007.03.003. DOI: https://doi.org/10.1016/j.precamres.2007.03.003

Naqvi SM. Comment on “The Sandur Schist Belt and its adjacent Plutonic Rocks: Implications of Late Archaean Crustal Evolution in Karnataka. Journal of Geological Society of India.1997; 49(4):459-60

Chkrabarti C., Reddy US, Natarman WK. Sedimentary Structures in the Archean Sediments of Gadag Schist Belt, Karnataka. Journal of Geological Society of India. 1993; 41(6).

Agasnalli C, Deepak MS, Lakkundi TK, Ajey Kumar VG. An Integrated Study of Landsat ETM and Cartosat DEM Data in Identification of Banded Iron Formations (BIFs) associated with Sulphide Mineralisation. Acta Geodynamica et Geomaterialia. 2022; 19(205):35-44. https://doi.org/10.13168/AGG.2021.0041. DOI: https://doi.org/10.13168/AGG.2021.0041

Ugarkar AG, Devaraju TC. Ore Mineralogy of Western Auriferous Zone of Gadag Greenstone Belt, Karnataka. Journal of Geological Society of India. 1994; 43:549-55.

Ugarkar AG, Panaskar DB, Gowda RG. Geochemistry, Petrogenesis and Tectonic Setting of Metavolcanics and their Implications for Gold Mineralisation in Gadag Gold Field, Southern India. Gondwana Research. 2000; 3(3):371-84. https://doi.org/10.1016/S1342-937X(05)70295-1. DOI: https://doi.org/10.1016/S1342-937X(05)70295-1