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Australian Energy Producers Journal Australian Energy Producers Journal Society
Journal of Australian Energy Producers
RESEARCH ARTICLE (Non peer reviewed)

Geoscience Australia seismic survey 310: revealing stratigraphy and structure of the outer northern Perth Basin margin

George Bernardel A and Chris Nicholson A
+ Author Affiliations
- Author Affiliations

Geoscience Australia.

The APPEA Journal 53(2) 481-481 https://doi.org/10.1071/AJ12092
Published: 2013

Abstract

Geoscience Australia acquired seismic survey GA 310 in 2008–09, across the southwest margin of Australia, as part of the Australian government’s Energy Security Program. Deep reflection seismic and potential field data were recorded across sparse 2D grids located on the Wallaby Plateau in the north, Mentelle Basin in the south, and the intervening Houtman and Zeewyck sub-basins of the northern Perth Basin.

The offshore northern Perth Basin extends for about 700 km along the Western Australia margin, from the towns of Carnarvon in the north to Cervantes in the south. The largely Paleozoic-Mesozoic tectonostratigraphic framework is dominated by Permian and Early-Middle Jurassic rifting, followed by Late Jurassic-Early Cretaceous rifting leading to Valanginian breakup between Australia and Greater India. Underlying Precambrian Pinjarra Orogen structuring, in conjunction with rifting, has resulted in the development of several complex depocentres and basement highs.

A recent re-evaluation of the offshore northern Perth Basin well-based lithostratigraphy into a new chronostratigraphic sequence framework has been carried outboard, on the GA 310 seismic lines, into the margin bounding the Zeewyck and northern Houtman sub-basins. The main sequences hosting source rocks—Kockatea and Cattamarra—are widely present in the expansive northern Houtman Sub-basin, and are likely to be present in the deep Zeewyck Sub-basin. The mapping of a thick Late Jurassic Yarragadee Sequence in the Zeewyck Sub-basin indicates a major pre-breakup locus of relatively rapid deposition. The structural interpretation across the sub-basin highlights breakup-drift unconformities and strike-slip faulting and suggests a probable along-margin sheared crustal sliver; tectonic elements commensurate with an evolving rift-shear breakup margin.

George Bernardel is a geoscientist in Geoscience Australia’s Basin Resources Group. He has a BSc (Hons) and BEng. He has worked at Geoscience Australia since 1988 after a short period at Bridge Oil NL. In the past few years, he has been researching about the architecture and evolution of Australia’s Southwest Margin. Member: PESA and EAGE.

Chris Nicholson is a geoscientist in Geoscience Australia’s Basin Resources Group. He graduated from ANU with a BSc (Hons) (2000). His research has focused the hydrocarbon prospectivity of frontier basins on Australia’s continental margin. Recently, he worked with a multi-disciplinary team to re-assess the hydrocarbon prospectivity of the offshore northern Perth Basin. Previously, he undertook similar research on the Mentelle, Vlaming, and Bremer basins. He is leading a regional integrated assessment of petroleum prospectivity and CO2 storage potential in the Browse Basin. Member: PESA and EAGE.


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