[ Up ] [ Introduction ] [ Seismic Expressions ] [ Results ] [ Bayu-Undan ] [ Tahbilk ] [ Skua ] [ Jabiru ] [ Cornea ] [ Anomaly1 ] [ Anomaly2 ] [ Anomaly3 ] [ North Rankin ] [ Enfield ] [ Macedon ] [ Chinook ] [ Carnarvon ] [ Novara NW ] [ Zeewulf ] [ Jupiter ] [ Scarborough ] [ Otway ] [ Kingfish ] [ Exploration ] [ Skua Detail ] [ Macedon Detail ] [ Implications ] [ Summary ] [ Acknowledgements ] [ References ] [ Authors ] [ Update ]
Kingfish
oil field, Gippsland Basin
Location:
Gippsland Basin, south-eastern
Pull-up:
Medium
Top of HRDZ: ~500 ms
Amplitude Anomalies: High
Intensity: Medium
Data Degradation: Low
The
giant Kingfish Field in the Gippsland Basin has a prominent HRDZ/gas chimney
associated with it (Fig. 23a). The anomaly is located between about 500 and 600
ms, near CDP 3250, and shows amplitude anomalies and pull-up of underling
reflectors (Fig. 23b). There is also some sign of pull-up near 300 ms. A column
of disrupted seismic data extends from near the sea floor down to about 1,200
ms.
Whilst
some of the shallow gas in the Gippsland Basin may be biogenic, large
thermogenic hydrocarbon seeps have also been documented in the basin (Heggie et
al, 1991a and b). In fact, no biogenic seeps have actually been detected during
any of the water column sniffer surveys carried out in the basin (O’Brien,
unpublished data). This observation, combined with the fact that the depth of
the disrupted data zone is consistent with leakage from the Kingfish
accumulation, leads us to favour a thermogenic, leakage-related origin for this
anomaly. Similarly, the Kingfish Field does not have a gas cap and the oil is
under-saturated with gas, as are the leaky Jabiru and Challis fields in the
Timor Sea.

a)

b)
Figure
23. a) An
HRDZ and gas chimney above the Kingfish oil
of
boxed area on Fig. 23a.

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APPEA Journal 2000. © This collection APPEA Limited 2000. Authors retain
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