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Geological evolution of the Canning Basin, Western Australia
Underlying an area of 430 (lOO km2 onshore and 165000 km2 offshore in Western Australia the Canning Basin contains about 10 000 m of Palaeozoic, Mesozoic, and Cainozoic... -
Seascapes of the Australia Margin and Adjacent Sea Floor: Methodology and Results
This report describes the iterative methods used to create the seascapes, including a detailed appendix documenting the different datasets used in the different planning zones.... -
Some aspects of lagoon sedimentation and circulation at One Tree Reef,...
Observations of water movement at One Tree Reef under modal wind, wave, and tide conditions show that the lagoon currents are insufficient to entrain lagoon sediments and cannot... -
Regional variations in Australian heat flow
Twenty new heat-flow values from widely separated sites on the Australian continent are presented. These are combined with published land and marine data in the area 90-170°E,... -
Australia and the Ocean Drilling Program : Extended Abstracts from the 13th...
Legacy product - no abstract available -
Post Cruise Report, Prydz Bay and Mac. Robertson Shelf, Antarctica, January...
The Natural Variability Sub-program of the Co-operative Research Centre for Antarctic and Southern Ocean Environments aims to study past environmental change by examining ice... -
3D Gravity Models of the Capel and Faust Basins, Lord Howe Rise
This report is part of a set delivered by Geoscience Australia on interpretation of data acquired during the summer of 2006/07 on seismic reflection, refraction and potential... -
Examination of Samples from Cossigny No. 1, Flinders Shoal No. 1, Hampton...
Examination of samples from Cossigny No. 1, Flinders Shoal No. 1, Hampton No. 1 and Lawley 1, offshore Carnarvon Basin, Western Australia, for Triassic conodonts. -
pmd*CRC 40Ar/39Ar Geochronology and Halogen/Noble Gas Geochemistry of...
The principal objective of the H4 Project was to evaluate existing techniques and develop new enabling technologies in geochronology and isotope geoscience to significantly... -
Geology of the Stillwell Hills
The Stillwell Hills region comprises granulite facies gneisses which record evidence for multiple periods of deformation and metamorphism spanning more than 2500 Million years.... -
Towards a balanced future BMR marine program: new basins, new approaches, new ideas
Legacy product - no abstract available -
Vema cruise 33 leg 3 over the magnetic quiet zone south of Australia, 20...
Legacy product - no abstract available -
Using Himawari-8 SST data for the investigation of highly dynamic...
The high frequency (10 min) and resolution (~2km) of Himawari-8 data provides an enormous opportunity for the monitoring and investigation of highly dynamic oceanographic... -
Enhancing Marine Spatial Planning through Integrated Seabed Mapping and...
Pre-competitive geoscience information, including bathymetry compilations, seabed geomorphology and sediment stability maps and other spatial information is essential to support... -
Marine geology of the continental shelf off southeast Australia
The continental shelf of southeast Australia between Sugarloaf Point and Gabo Island, New South Wales, varies in width from 72 km east of Newcastle to 17 km east of Montague... -
The Geology of the Kenn Plateau Off Northeast Australia: Results of Southern...
In the Late Cretaceous, the Kenn Plateau was part of the Maryborough Basin to the west and the Capricorn Basin to the north. It separated from Australia from the earliest... -
Marine geophysical survey, Gulf of Papua and Bismarck Sea Field report,...
Legacy product - no abstract available -
Preliminary report of an underwater gravity survey, Cape Arnhem to Darwin, 1958
Legacy product - no abstract available -
Summaries of other papers presented
Abstracts: 'Models of sulphide ore formation in sedimentary rocks', Gustafson, L.B.; 'Metal sources and fixation in some stratiform deposits' Lambert, I.B.; 'addle dolomite... -
R/V 'Vema' crusie 33 leg 14, in the southwest Pacific Ocean, 21 January to...
Legacy product - no abstract available