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J C PATTERSON INTERNATIONAL PETROLEUM INVESTMENT WHY AUSTRALIA?
P TIES R D SHAW and THE PETROLEUM PROSPECTIVITY OF THE CLARENCEMORETON
W G TOWNSON THE SUBSURFACE GEOLOGY OF THE WESTERN OFFICER BASIN
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aeolianites anticline APEA Journal Barrow Group Barrow Island Barrow Sub-basin basal basement Bass Basin Bass Strait borehole Callovian Carynginia Limestone cent Claystone Coal Measures Cooper Basin core Dampier Sub-basin delta deposition depth Dingo Claystone drilled Dupuy Member Early Cretaceous environment Eromanga Basin extensional facies field Figure flow Fortescue gas lift Geological Hussar hydrocarbon indicate interpreted interval Jurassic located lower margin maturity migration Muderong Shale Murta Member Naccowlah Block Naccowlah-Jackson Trend normal faults Officer Basin oil and gas organic matter overlying Palm Valley permeability Permian Petroleum pipeline porosity potential pressure production Proterozoic Rankin Platform reservoir Roma Shelf samples sand Sandstone sedimentary sediments seismic seismic data seismic sections sequence Shale shallow siltstone source rocks South Pepper stratigraphic structural tectonic thick tion transfer faults Triassic Trough unconformity unit Upper vitrinite Western Australia Woodada Yowalga zone