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Basin-scale fluid flow in the Gippsland Basin: implications for geological carbon storage.

Authors :
O'Brien, G.W.
Tingate, P.R.
Goldie Divko, L.M.
Miranda, J.A.
Campi, M.J.
Liu, K.
Source :
Australian Journal of Earth Sciences. Feb2013, Vol. 60 Issue 1, p59-70. 12p. 2 Color Photographs, 1 Diagram, 5 Maps.
Publication Year :
2013

Abstract

Petroleum systems analysis has been carried out to better understand the geological CO2storage potential of the Gippsland Basin. From a regional perspective, the hydrocarbon migration architecture of the basin is interpreted to be dominated by two highly connected, filled-to-spill, hydrocarbon fairways; the northern (gas-dominated) and southern (oil-dominated) fill-spill chains, forming a convergent system that extends onshore along the Golden Beach Fill-Spill Chain (GBFSC). A separate oil-dominated Fill-Spill Chain, the Dolphin-Perch Fill-Spill Chain (DPFSC), is identified offshore to the southwest. Two broad flanking provinces, the Northerly Migration Province (NMP) and Southerly Migration Province (SMP), are also identified. Both provinces have broadly ramp-like geometries and relatively low dips. Migration across these provinces is not focused, and hence multiple pathways are present across a wide area. An understanding of the hydrocarbon systems in the basin can be used for characterising the potential for CO2storage. Previous studies have shown that the top seal potential of the offshore Gippsland Basin is suited to geological carbon storage and that large areas are prospective as storage regions. However, the linked nature of the fluid flow systems and the focused fluid flow fairways between areas of high storage potential and leaky systems onshore will require both a good regional geological understanding and informed resource management. [ABSTRACT FROM PUBLISHER]

Details

Language :
English
ISSN :
08120099
Volume :
60
Issue :
1
Database :
Academic Search Index
Journal :
Australian Journal of Earth Sciences
Publication Type :
Academic Journal
Accession number :
85924388
Full Text :
https://doi.org/10.1080/08120099.2013.755567