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Economic Potential of the Heavy Minerals of the Beaches between Baruva and Bavanapadu, Andhra Pradesh


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1 Department of Geology, Andhra University, Visakhapatnam - 530 003, India
     

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The economic potentiality of the heavy minerals in the beaches between Baruva and Bavanapadu extending for about 45 km was examined. In the sub-surface sediments, the heavy minerals were studied at an interval of 1 m up to a maximum depth of 5.8m. In general the concentration of heavy minerals is high in dunes followed by backshore and foreshore regions. Heavy mineral content increases from surface to sub-surface in dunes, decreases in foreshore and does not vary much in backshore. The heavy minerals include mainly ilmenite, garnet, sillimanite and ortho-pyroxenes with minor amounts of amphiboles, zircon, monazite, rutile etc. Majority of the heavies such as ilmenite, monazite, zircon etc. are concentrated in finer fractions while some of the heavies like garnet and sillimanite are concentrated in coarser fractions. The inferred reserves estimated for the area indicate its economical potential.

Keywords

Heavy Minerals, Dunes, Backshore, Foreshore, Economic Potential.
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  • Economic Potential of the Heavy Minerals of the Beaches between Baruva and Bavanapadu, Andhra Pradesh

Abstract Views: 199  |  PDF Views: 2

Authors

D. Rajasekhara Reddy
Department of Geology, Andhra University, Visakhapatnam - 530 003, India
V. S. S. Prasad
Department of Geology, Andhra University, Visakhapatnam - 530 003, India
V. Malathi
Department of Geology, Andhra University, Visakhapatnam - 530 003, India
K. S. N. Reddy
Department of Geology, Andhra University, Visakhapatnam - 530 003, India
D. D. Varma
Department of Geology, Andhra University, Visakhapatnam - 530 003, India

Abstract


The economic potentiality of the heavy minerals in the beaches between Baruva and Bavanapadu extending for about 45 km was examined. In the sub-surface sediments, the heavy minerals were studied at an interval of 1 m up to a maximum depth of 5.8m. In general the concentration of heavy minerals is high in dunes followed by backshore and foreshore regions. Heavy mineral content increases from surface to sub-surface in dunes, decreases in foreshore and does not vary much in backshore. The heavy minerals include mainly ilmenite, garnet, sillimanite and ortho-pyroxenes with minor amounts of amphiboles, zircon, monazite, rutile etc. Majority of the heavies such as ilmenite, monazite, zircon etc. are concentrated in finer fractions while some of the heavies like garnet and sillimanite are concentrated in coarser fractions. The inferred reserves estimated for the area indicate its economical potential.

Keywords


Heavy Minerals, Dunes, Backshore, Foreshore, Economic Potential.