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Geochemical Constraints on the Genesis Phosphorites of Chhattisgarh Basin, Durg District, M.P., India


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1 School of Studies in Geology, Ravishankar University, Raipur 492010 (M.P.), India
     

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This paper documents the geochemical and mineralogical characters of the phosphorite of Charmuria Formation (Chhattisgarh Basin). X-ray diffraction studies have revealed presence of carbonate fluorapatite as the only apatite mineral in this phosphorite, along with quartz as major gangue, and kaolinite-illite, calcite and pyrite in subordinate amounts. Structural formula of this apatite closely resembles carbonate fluorapatite. Further, CaO/P2O5 ratio (1.37 - 1.99) suggests that this phosphorite has not been affected by weathering. Quartz dominance over clay minerals and low CIA (24.79 - 46.87) is attributed to the tuffaceous nature of siliceous clays (lithofacies-A). The depletion of Sr, and trace elements of organic association in siliceous clays, phosphorite and phosphatic siliceous clays point to a common provenance.

Keywords

Geochemistry, Phosphorite, Carbonate Fluorapatite, Chhattisgarh Basin.
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  • Geochemical Constraints on the Genesis Phosphorites of Chhattisgarh Basin, Durg District, M.P., India

Abstract Views: 183  |  PDF Views: 1

Authors

M. W. Y. Khan
School of Studies in Geology, Ravishankar University, Raipur 492010 (M.P.), India
A. Mukherjee
School of Studies in Geology, Ravishankar University, Raipur 492010 (M.P.), India

Abstract


This paper documents the geochemical and mineralogical characters of the phosphorite of Charmuria Formation (Chhattisgarh Basin). X-ray diffraction studies have revealed presence of carbonate fluorapatite as the only apatite mineral in this phosphorite, along with quartz as major gangue, and kaolinite-illite, calcite and pyrite in subordinate amounts. Structural formula of this apatite closely resembles carbonate fluorapatite. Further, CaO/P2O5 ratio (1.37 - 1.99) suggests that this phosphorite has not been affected by weathering. Quartz dominance over clay minerals and low CIA (24.79 - 46.87) is attributed to the tuffaceous nature of siliceous clays (lithofacies-A). The depletion of Sr, and trace elements of organic association in siliceous clays, phosphorite and phosphatic siliceous clays point to a common provenance.

Keywords


Geochemistry, Phosphorite, Carbonate Fluorapatite, Chhattisgarh Basin.