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Authors
Affiliations
1 INSA Project, Department of Mines and Geology, Bangalore 560001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 22, No 6 (1981), Pagination: 258-265
Abstract
The Gurusiddapura and Hoskere conglomerates of Chitradurga schist belt belong to one continllolls stratigraphic unit. Deformational analysis indicates that the pebbles in both the conglomerates belong to one single population. Graded bedding and occurrence of pebbly and non-pebbly zones indicate turbidite environment of deposition in an unstable geosyncline. Since the conglomerates are interbedded with chlorite schist they do not mark any unconformity.
