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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 […]

    Read more of: Major paleogeographic and paleoclimatic changes during the late Paleozoic, Early Cretaceous and Cenozoic of central Australia and their influence on recycling of sediments
  2. Subglacial Conditions From Converted-Wave Seismic Reflection Amplitudes: Synthetic Experiments and Case Study Reveal a Frozen Bed at an Antarctic Ice Rise

    Understanding how an ice sheet slips at its base is an important part of ice sheet models; this requires knowledge of the geological materials underlying the ice. Controlled-source seismic surveys […]

    Read more of: Subglacial Conditions From Converted-Wave Seismic Reflection Amplitudes: Synthetic Experiments and Case Study Reveal a Frozen Bed at an Antarctic Ice Rise