[ 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 ]
Enfield
oil and gas discovery, Carnarvon Basin
Location:
Carnarvon Basin
Top of HRDZ: 1300 ms
Pull-up: Strong
Intensity: High
Amplitude
Anomalies: Strong
Area:
Small
Data Degradation: High
Two HRDZs were identified in WA-271-P, prior to
the drilling of the Enfield–1 well by Woodside in 1999. Their significance was
highlighted when the Enfield–1 well discovered hydrocarbons in a stratigraphic
trap to the east of these anomalies. These HRDZs are small in extent but have
high intensity.
The
anomaly shown in Figure 13 is seen on only two closely spaced 2D lines—on a
wider grid spacing, the anomaly would be missed altogether. The presence of this
anomaly provides high confidence of hydrocarbon charge in this region.

Figure 13. An HRDZ lies to the
west of the Enfield discovery in the Carnarvon Basin. Left panel is by courtesy
of Schlumberger Geco-Prakla.

Field:
West of the Enfield oil and gas
discovery
Location:
Carnarvon Basin
Top of HRDZ: 1450 ms
Pull-up: Moderate
Intensity: Moderate
Amplitude Anomalies: Strong
Area: Small
Data Degradation: Moderate
The
second HRDZ to the west of the Enfield oil and gas discovery is shown on Figure
14. Cemented zones in the shallow section between 1,400 and 1,600 ms show
increased reflectivity, with some degradation in stack response evident below
this region. The strong reflector at 1,900 ms is affected by pull-up caused by
the overlying, high velocity, cemented zones. The presence of this anomaly
provides high confidence of hydrocarbon charge in this region.

Figure 14. A second HRDZ to the
west of the Enfield Discovery in the Carnarvon Basin.

The APPEA Journal 2000. © This collection APPEA Limited
2000. Authors retain © in respect of their own contribution.