Reddy, Purushottam R and Raghavendra, N R and Sathyagangadharudu, A (2010) The study of banded iron formations of coppermountain belt near Torangal, Bellary District, Karnataka State (India). Journal of Metallurgy and Materials Science, 52 (2). pp. 161-168.
Purushottam_161-168.pdf
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Abstract
The banded iron formation (BIF), corresponding mostly to oxide facies, exposed
in north eastern parts of the Sandur greenstone belt has been studied with respect to their
field, Petro graphic, Mineralogical and Petrochemical Aspects. It is concluded that these
iron formations are essentially the results of chemical precipitation of iron and silica
derived from continental weathering of basic rocks under anaerobic, quiest, below-wave
base marine conditions. The banding is attributed to cyclic changes in climatic conditions.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | Banded Iron Formation (BIF), Facies, Greenstone Belt and Craton |
| Subjects: | Metallurgy |
| Divisions: | Metal Extraction and Forming |
| Depositing User: | Dr. A K Sahu |
| Date Deposited: | 14 Mar 2011 05:02 |
| Last Modified: | 02 Sep 2026 20:18 |
| URI: | http://eprints.nmlindia.org/id/eprint/2560 |

