Recognition, Correlation and Age of Erosion Surfaces in the Iron Ore Ranges of Bihar and Orissa
Abstract
In the Iron Ore Ranges of Bihar and Orissa, three erosion surfaces have been recognised around 3000-2700 feet, 2300-2000 feet and 1600-1400 feet above M.S.L., based on model studies in the laboratory, and the relative positions in the field of the residual deposits of laterites and lateritic iron and manganese ores. These have been correlated with those in the neighbouring areas in the southeastern Chota Nagpur and the Simlipal massif in Bihar and Orissa respectively. Based on the study of sedimentary record in the adjoining Bengal Basin, the tentative ages assigned to them from the top are Upper Jurassic to Lower Cretaceous, Upper Eocene and Upper Miocene.
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References
DUNN, J. A., (l937) The mineral deposits of eastern Singhbhum and surrounding areas. Mem. Geol. Surv. Ind, Vol. 69, Pt. 1.
DUNN, J. A., (1938) Post-Mesozoic movements in Chota Nagpur. Abs. Proc. 25th Ind. Sc. Congr., p.125.
JONES, H. C., (1934) Iron ore deposits of Bihar and Orissa. Mem. Geol. Surv. Ind., Vol. 32, Pt. 2.
KING, L. C., (1962) The Morphology of the Earth. Oliver and Boyd., Edinburgh.
PRIDER, R. T., (1966) The lateritised surface of Western Australia. Australian Jour. Sc., Vol. 28 (12), pp. 443-451.
SENGUPTA, S., (1966) Geological and geophysical studies in western part of Bengal Basin, India. Bull. Am. Assoc. Petroleum. Geol., Vol. 50 (5), pp. 1001-1017.
VAIDYANADHAN, R., (l964) Recognition and correlation of erosion surfaces in and around the southern part of Cuddapah Basin. Jour. Geol. Soc. Ind., Vol. 5, pp. 121-127.
VAIDYANADHAN, R., (1967) An outline of the geomorphic history of India south of N. Latitude 18°. Proc. Seminar on Geomorphological studies in India (1965), Centre of Adv. Study in Geology, Saugor, pp. 121-130.