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Basin Evolution Study of the Machundri River, Southern Saurashtra Coast, Gujarat
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The Neogene/Quaternary boundary is reported to be erosional. The Pleistocene miliolite limestone shows the development of a sequence of palaeo-beach-dune complexes with the gradual fall of sea level. The late Pleistocene-Holocene stratigraphic units comprise different generations of deltaic sediments aggrading older tidal marshes and backswarnps. The late Holocene sea-level fall helped in delta progradation and the development of different accretionary units all along the coast.
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