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  • Glaciation of Mauna Kea, Hawaii in Quaternary glaciations in the Northern Hemisphere.
  • Comparative uranium-thorium and thermoluminescence dating of weathered Quaternary alluvium in the tropics of Northern Australia
  • Geomorphology and Quaternary history of the Australian continental dune fields
  • Lithospheric deformation in French Polynesia (Pacific Ocean) as deduced from Quaternary shorelines in Proceedings. Volume 3. Symposia and seminars.
  • Late Quaternary shorelines give evidence of an elastic flexuring of the lithosphere in relation to the volcanic load of Tahiti and Moorea islands. Elastic models are however insufficient to explain all the sea-level data: thermal variations
  • Recent morphostratigraphic studies of the Australian Quaternary in Australian physical geography.
  • Prehistory and palaeoecology of Torres Strait in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
  • The Woakwine Terrace in the south east of South Australia and indications of the very early presence of man in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
  • Toward a comprehensive Upper Quaternary tephra and ignimbrite stratigraphy in New Zealand using electron microprobe analysis of glass shards
  • The supposed Javan affinities of the Tula adze-flake from Australia in Modern Quaternary research in southeast Asia.
  • Deformation of the North Queensland continental shelf in the late Quaternary in Shorelines and isostasy.
  • Geomorphological significance of late quaternary deposits of the Lake George Area, N. S. W.
  • Contemporary and palaeo channels patterns and the late Quaternary stratigraphy of Cooper Creek, Southwest Queensland, Australia
  • Alluvial terrace distributions and profiles drawn using the terrace heights provide the main evidence of the captures, and also evidence of the time when the captures occurred. The AA. have worked on late Quaternary deposits and climatic history
  • that sclerophyll vegetation developed largely from a Late Cretaceous/Early Tertiary immigrant flora in response to drier climatic conditions in the Late Tertiary and to a dramatic increase in burning with the arrival of aboriginal man in the Late Quaternary