2009
DOI: 10.1016/j.marpetgeo.2008.05.001
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Regional study on potential CO2 geosequestration in the Collie Basin and the Southern Perth Basin of Western Australia

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Cited by 19 publications
(10 citation statements)
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“…A number of previous studies have made preliminary assessments in the South West, summarised in [1] . An appraisal of the geology around the town of Collie, a major emissions hub, by Varma et al, 2009) [2] showed no suitable storage locations proximal to Collie, and the study was geographically extended. The study then identified the current area (Lesueur; Figure 1) for investigation and work continues at present.…”
Section: Introductionmentioning
confidence: 94%
“…A number of previous studies have made preliminary assessments in the South West, summarised in [1] . An appraisal of the geology around the town of Collie, a major emissions hub, by Varma et al, 2009) [2] showed no suitable storage locations proximal to Collie, and the study was geographically extended. The study then identified the current area (Lesueur; Figure 1) for investigation and work continues at present.…”
Section: Introductionmentioning
confidence: 94%
“…Following on from these studies, the Western Australian Department of Mines and Petroleum then went on to fund a more detailed study (Varma et al 2007) 2). Areas investigated began within a 50 km radius of the town of Collie and included the Collie Basin sandstones and the coal measures of the Cardiff Subbasin.…”
Section: Co2crc Study (2007)mentioning
confidence: 99%
“…Salinity in the formation increases from 51500 to 425000 mg/L over a 250 m depth interval within the Eneabba Formation, and the associated lack of freshwater recharge suggests that the strata have low vertical hydraulic conductivity in that area ( Figure 6). Varma et al (2007Varma et al ( , 2009) used information from nearby Lake Preston-1 well log data to work out the downhole salinity and, by inference, estimate the permeability through the rest of the formations in the region of the Harvey Ridge structure ( Figure 5). Relative changes in the values of the induction and short-normal resistivity logs, at these depths, have been interpreted in this case as an increase in formation water resistivity relative to the resistivity of the mud, and are believed to be representing lower water salinity ( Figure 5).…”
Section: Evidence Of Injectivitymentioning
confidence: 99%
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