2021
DOI: 10.1080/08120099.2021.1966836
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The Cooper–Eromanga petroleum province, Australia

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Cited by 3 publications
(1 citation statement)
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“…A rapid increase in subsidence rates, combined with globally high sea levels in the Early Cretaceous, resulted in a marine incursion across much of the Australian continent and deposition of marine sediments across the Eromanga Basin (Gallagher et al 2008). Open marine and marginal marine sedimentation continued until the Late Cretaceous when the basin returned to non-marine sedimentation during deposition of the Winton Formation before basin closure during an E-W Late Cretaceous compressional event (Cotton et al 2006;Kulikowski et al 2021). Rapid deposition of the Late Cretaceous Winton Formation was the critical event for hydrocarbon generation and expulsion from many Permian, Triassic and Jurassic source intervals (Lowe- Young et al 1997).…”
Section: Tectonostratigraphic Evolution Of the Eromanga Basinmentioning
confidence: 99%
“…A rapid increase in subsidence rates, combined with globally high sea levels in the Early Cretaceous, resulted in a marine incursion across much of the Australian continent and deposition of marine sediments across the Eromanga Basin (Gallagher et al 2008). Open marine and marginal marine sedimentation continued until the Late Cretaceous when the basin returned to non-marine sedimentation during deposition of the Winton Formation before basin closure during an E-W Late Cretaceous compressional event (Cotton et al 2006;Kulikowski et al 2021). Rapid deposition of the Late Cretaceous Winton Formation was the critical event for hydrocarbon generation and expulsion from many Permian, Triassic and Jurassic source intervals (Lowe- Young et al 1997).…”
Section: Tectonostratigraphic Evolution Of the Eromanga Basinmentioning
confidence: 99%