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Proterozoic Conglomerates of Bar, Debari, Umra and Jaisamand in South Central Rajasthan - A Study in Strain Analysis
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Dunnet's matching curve technique has been applied for evaluating the finite strain of basal conglomerate clasts occurring at the base of Delhi as well as Aravalli rock formations. The study revealed that deformation shown by the enclosing clasts are close to the theoretical values.
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