1887
Volume 24, Issue 3-4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

Studies of Amplitude Variations with [Versus] Offset (AVO) have been used in Australia and worldwide to evaluate possible hydrocarbon prospects. This study concentrates on modelling the effects of thin beds (carbonates, shales) above and within sandstones on AVO behaviour.

Forward modelling of synthetic gathers from the Campbell-2 well has confirmed that the strongly anomalous AVO response observable over the gas and oil field is due to the hydrocarbon column in the Flag Sandstone of the Barrow Group. Modelling presented here shows that a 5 m thick shale with its top 15 m below the top of the reservoir modified the AVO response of the top of the reservoir, but this response is still strongly anomalous. However, modelling a reservoir with two 5 m thick shale beds located 5 m and 15 m below the top of the reservoir modified the AVO response of the top of the reservoir to the extent that the AVO response is not significantly anomalous.

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/content/journals/10.1071/EG993847
1993-09-01
2026-01-18
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References

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  2. Micenko, M. (1992), ‘AVO and inversion mapping — Campbell Gas Field, Barrow Sub-Basin, W.A.’, Explor. Geophys.23, 213–218.
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  7. Ward, J. (1992), ‘AVO calibration — ideas based on a sandstone model’, In SEG/EAEG Summer Research Work-Shop, How Useful is Amplitude-Versus-Offset (AVO) Analysis?. Big Sky, Montana.
/content/journals/10.1071/EG993847
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  • Article Type: Research Article
Keyword(s): AVO; Campbell-2; Carnarvon Basin.; Flag Sandstone; thin beds

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