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Birmania Phosphorites: Petro-Mineralogical Characters and Palaeogeological Implications


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1 Department of Geology, University of Delhi, Delhi 110 007, India
     

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The lower Palaeozoic (possibly Cambrian) phosphorites of Birmania in Western Rajasthan are pelletal as well as microcrystalline. Carbonate fluorapatite is the only mineral phase in these phosphorites. Petrodiagenetic and mineralogical studies indicate primary precipitation of apatite directly from the basinal waters. Suggestions have been made for an extensive Cambrian sea encompassing the phosphogenic provinces of Western Rajasthan, Hazara in Pakistan and Mussoorie hills of Kumaun Himalayas.
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  • Birmania Phosphorites: Petro-Mineralogical Characters and Palaeogeological Implications

Abstract Views: 180  |  PDF Views: 4

Authors

Viqar Husain
Department of Geology, University of Delhi, Delhi 110 007, India
D. M. Banerjee
Department of Geology, University of Delhi, Delhi 110 007, India

Abstract


The lower Palaeozoic (possibly Cambrian) phosphorites of Birmania in Western Rajasthan are pelletal as well as microcrystalline. Carbonate fluorapatite is the only mineral phase in these phosphorites. Petrodiagenetic and mineralogical studies indicate primary precipitation of apatite directly from the basinal waters. Suggestions have been made for an extensive Cambrian sea encompassing the phosphogenic provinces of Western Rajasthan, Hazara in Pakistan and Mussoorie hills of Kumaun Himalayas.