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GEODISC Environmentally Sustainable Sites For Carbon Dioxide Injection WFS
This web service depicts potential geological sequestration sites and has been compiled as part of the Australian Petroleum Cooperative Research Centre's GEODISC program (1999-2002).
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Department of State Development - Mineral Drillholes, Petroleum and Geothermal Wells
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Location of South Australian mineral drillholes, petroleum and geothermal wells. Available format: ESRI Shape, MAPINFO Tab, Google Earth KMZ and WMS/WFS. Download Instructions: From SARIG http://map.sarig.sa.gov.au/Shortcut/DrillholesWells select 'Active Layers' and click the download icon.
GSQOpenData@resources.qld.gov.au - ESPERANZA SOUTH SD629
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URL: https://geoscience.data.qld.gov.au/dataset/bh077074
GSQOpenData@resources.qld.gov.au - EPM 13505, SELWYN 2, ANNUAL REPORT FOR PERIOD 6/2/2006 TO 5/2/2007
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URL: https://geoscience.data.qld.gov.au/dataset/cr049209 EPM 13505, SELWYN 2, ANNUAL REPORT FOR PERIOD 6/2/2006 TO 5/2/2007
GSQOpenData@resources.qld.gov.au - EUROMBAH EAST 1
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URL: https://geoscience.data.qld.gov.au/dataset/bh062017
GSQOpenData@resources.qld.gov.au - WESTMORELAND 2
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URL: https://geoscience.data.qld.gov.au/dataset/bh001245
GSQOpenData@resources.qld.gov.au - BALGOWNIE WEST 1
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URL: https://geoscience.data.qld.gov.au/dataset/bh000099
GSQOpenData@resources.qld.gov.au - GALILEE NS2502
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URL: https://geoscience.data.qld.gov.au/dataset/bh009979
Hydrocarbon and Geothermal Prospectivity of Sedimentary Basins in Central Australia; Warburton, Cooper, Pedirka, Galilee, Simpson and Eromanga Basins
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Within the Central Australian region, nominally constrained by 22.5oS 134oE and 31.5oS 144oE for this study, lie several systems of stacked basins beneath the extensive Mesozoic Eromanga Basin. Remnants of Proterozoic basins are largely inferred from gravity, unexplored, and are not everywhere differentiated from an extensive cover of the lower Palaeozoic Warburton Formation. This sequence is the central link between the contiguous Amadeus, Officer and Georgina Basins, and the Thomson Fold Belt. Since the Carboniferous, the region has largely experienced intracratonic sag and has accumulated continental sediments, including thick coal measures, with intermittent tectonism and uplift. In late Early Cretaceous, marine conditions briefly invaded this subsiding region, but continental sedimentation resumed in the Late Cretaceous. Tectonism occurred in the Tertiary with basin inversion and subsequent formation of the Great Artesian Basin. In the Cainozoic, the region is again in subsidence and accommodating fluvial and aeolian sediment slowly into the Eyre Basin. The preserved depocentres of the Carboniferous-Permian-Triassic Cooper, Pedirka-Simpson, and Galilee Basins are spatially separate, although all contain comparable, largely organically-mature continental coal measure sequences.
GSQOpenData@resources.qld.gov.au - GALILEE NS120
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URL: https://geoscience.data.qld.gov.au/dataset/bh007595
GSQOpenData@resources.qld.gov.au - GALILEE NS2400
공공데이터포털
URL: https://geoscience.data.qld.gov.au/dataset/bh009877