[ 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 ]
Novara
North-West anomalies
Feature:
Novara NW (Undrilled)
Location: Carnarvon Basin
Top of HRDZ: 1100 ms
Pull-up: Moderate
Intensity: Low
Amplitude Anomalies: Small
Area: Small
Data Degradation: Low
Line
HE94-146 (Fig. 18) shows apparent shallow folding at around 1,500 ms which may
actually be caused by the pull-up effects below shallower HRDZs. It may be
possible to discriminate between tectonic/depositional and leakage causes for
the observed effects.
Figure 18. Possible HRDZs NW of
Novara-1.
The APPEA Journal 2000. © This collection APPEA Limited
2000. Authors retain © in respect of their own contribution.
