1887
ASEG2012 - 22nd Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

The objective of the recent Silvereye 1 exploration well in Bass Basin was to test Paleocene and Cretaceous sandstone reservoirs of the Eastern View Coal Measures (EVCM). The well was designed to test a faulted four-way dip closure and stratigraphic trap interpreted as a sand filled channel. Pre-drill analysis relied on a recent 3D marine seismic survey with well control provided by 2D seismic ties to wells located in adjacent exploration permits.

The pre-drill interpretation of a gas-bearing sandstone-filled channel was based on a brightening of seismic amplitude (a predominantly class 3 AVO anomaly) associated with the channel feature. The AVO behaviour was consistent with the response at the same gas-bearing stratigraphic level in the nearby White Ibis 1 well, hence the presence of hydrocarbons (gas) was considered likely.

The well intersected the predicted stratigraphy but failed to encounter hydrocarbons at any of the reservoir intervals. A channel sand was intersected within a thick claystone interval at the pre-drill proposed stratigraphic trap. The claystone is characterised by low-velocity and high density, while the sandstone has slightly higher porosity than sand typically encountered in this section. It was the contrasting characteristics of these lithologies that determined the class 3 AVO response and the mis-interpretation of the anomaly. We show that a close examination of the rock physics trends of reservoir and non-reservoir rocks in surrounding wells could have allowed this scenario to be recognised pre-drill.

Failure to recognise all possible lithological characteristics in the pre-drill AVO model meant that not all outcomes were analysed, and hence were not included in the risking of the prospect . The post drill evaluation has recognised that rock physics studies are an important tool for recognising all possible scenarios to aid in prospect evaluation.

Had a more comprehensive rock physics evaluation been conducted, the actual outcome would likely have been recognised as one of several possibilities, but would not necessarily have prevented drilling of the well.

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2012-12-01
2026-01-12
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References

  1. Boreham et al., 2003. Coal as a source of oil and gas: A case study from the Bass Basin, Australia: APPEA Journal, Vol. 43 (2003), p. 117-148
  2. Hall, A., 2011 Silvereye 1 Petrophysical Interpretation Report, Origin Energy Resources Ltd, unpublished,
  3. Hansen et al., 2011. Silvereye 1 Well Proposal T/44P, Bass Basin Tasmania. Origin Energy Resources Ltd, unpublished,
  4. Phillips H., 2011. Silvereye 1 T/44P Offshore Bass Basin Well Completion Report Basic Data. Origin Resources Ltd, unpublished,
  5. Rutherford, S.R., and Williams, R.H., 1989, Amplitude-versus- offset variations in gas sands: Geophysics, Vol. 54, p. 680-688.
  6. Smith, T. M., Sondergelz, C. H., and Rai, C. S., 2003 Gassmann fluid substitutions: A tutorial Geophysics, Vol. 68, P. 430–440,
  7. Williamson et al., 1987. Review of stratigraphy, structure, and hydrocarbon potential of Bass Basin, Australia: Bulletin of the American Association of Petroleum Geologists, Vol. 71, p. 253-280
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  • Article Type: Research Article
Keyword(s): AVO; Bass Basin; channel; rock physics
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