Pliocene eustasy and the onset of sand barrier formation in Gippsland, Victoria


GIPPSLAND possesses a classical development of coastal lakes formed behind a sand barrier system which achieved its present form during the Quaternary. New evidence is assembled here, showing that a transgressive–regressive–transgressive cycle in the late Miocene–Pliocene ended in an earlier phase of barrier formation and lacustrine deposition. Another… (More)
DOI: 10.1038/280131a0


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