The Australian Government, through the Department of Industry, Innovation and Science, routinely funds Geoscience Australia to acquire pre-competitive data to support prospectivity assessments of various offshore basins. As part of the Australian Government's National CO2 Infrastructure Plan (Carbon Storage Taskforce 2009), a marine seismic reflection survey, Gippsland Basin Infill 2D Marine Seismic Survey - GA0352, was undertaken in the offshore southern margin of the Gippsland Basin to investigate potential sites suitable for CO2 geological storage (Langford, 2016).

This product is a map of the major Australian petroleum fields and pipelines (2010).

Regular release of offshore acreage, part of the Australian Government's strategy to encourage investment in petroleum exploration. These data are currently used for display only within the Geoscience Australia website.

Package holding all available processed data and well completion reports relevant to the Carnarvon 2007Acreage Release in workstation format - Geoframe, Kingdom and Landmark.

The Major Carbon Dioxide Emitters of Australia is a combination of a two digital datasets 'source_top50' and 'min_source' from within the publication: Bradshaw, J., Bradshaw, B., Spencer, L., Wilson, P., Simon, G. & Mackie, V. 2001. GEODISC Project 1 - Regional analysis, stage 3 basins and emissions mapping, Geoscience Australia, GEODISC1-2001-006 (CD). The top 139 CO2 emitters as of 1998 are included, representing ~43% of net national GHG emissions and 54% of the net energy emissions from the 1998 National Greenhouse Gas Inventory. Each emitter has information containing the following attributes; Facility, Facil_Type, Facil_Name, State, Emissions, Emissions1, Emissions2, Emissions3, 20Yrs_Mt, 20Yrs_Tcf, DataSource, DataYear.

The Onshore Energy Systems Group have undertaken a regional study on the prospectivity of the southern Georgina Basin, and present here a synopsis of the initial results from this multidisciplinary project. The Georgina Basin is a Neoproterozoic to Lower Devonian sedimentary basin covering 325,000 km2 of western Queensland and the Northern Territory (Dunster et al., 2007; Kruse et al., 2013; Munson, 2014). It is a northwest-southeast-trending extensional basin, where thick marine Cambrian and Ordovician sediments are preserved in its two southern depocentres, the Dulcie and Toko synclines, and a thinner succession is present in the Undilla Sub-basin to the northeast. Within these depocentres, the Thorntonia Limestone and Arthur Creek Formation (Figure 1) contain potential source rocks (Ambrose et al., 2001; Boreham and Ambrose, 2012). Most of the southern Georgina Basin is under license for petroleum exploration, with explorers targeting the carbonate-dominated Arthur Creek Formation for both conventional and unconventional hydrocarbons. A data package that includes raw and reprocessed HyLogging data from 25 wells in the Georgina Basin was recently released (Smith and Huntington, 2014). The HyLogging data map the mineralogical variations within formations and were used in conjunction with wireline log and biostratigraphic data to refine stratigraphic correlation. The HyLogging data were re-processed using a common set of mineral scalars (i.e., spectroscopic indices) to create an internally-consistent, basin-wide dataset. Other datasets, including total organic carbon (TOC) content, X-ray diffraction (XRD) measurements and biostratigraphy were also integrated with the Hylogging data. The 'hot shale' of the Arthur Creek Formation has a characteristic spectral response of decreasing albedo and an increased short wave infra-red (SWIR) aspectral response with increasing depth to the base of the Arthur Creek Formation (Figure 2), which both appear to correlate with increasing core total gamma and TOC. These inter-relationships may be used to better characterise and identify potential source rock units in the basin. Recent biostratigraphic work has highlighted an age discrepancy in the prospective organic-rich `hot shale in the base of the middle Cambrian Arthur Creek Formation (Figure 1). This unit is present in the two major southern depocentres, the Dulcie and Toko synclines, where it has previously been considered as correlative. Recent results, however, suggest that the basal 'hot shale' is either significantly younger in the Toko Syncline than in the Dulcie Syncline, or represents a condensed section in the former. Middle Cambrian carbon isotope excursions have been correlated across a number of Australian basins and can be used to test correlative models across the Georgina depocentres. High resolution sampling across this middle Cambrian section has been carried out in a number of wells in the Dulcie Syncline and in the Undilla Sub-basin, where the age equivalent Inca Shale is penetrated. Carbon isotopes from organic carbon (kerogen) as well as carbon and oxygen isotope ratios of four carbonate mineral phases (calcite, ankerite, dolomite and siderite) were analysed and these data are compared with existing carbon isotope stratigraphy published from neighboring wells (Donnelly et al., 1988; Lindsay et al., 2005; Creveling et al., 2013). Initial results corroborate the new biostratigraphic interpretation.

Updated USB drive containing GA-reports, maps in digital format to be handed out as promotioanl material at APPEA conference

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No abstract available

Map of permits currently held by Silver Wave Energy (AC/P49 to 51). Paper size A0.