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  1. Major paleogeographic and paleoclimatic changes during the late Paleozoic, Early Cretaceous and Cenozoic of central Australia and their influence on recycling of sediments

    During the late Paleozoic glacial ice extended from Antarctica across most of the Australian part of Gondwana. Maximum ice thickness over Antarctica was ∼5400–8000 m and over central Australia 2700–4000 […]

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