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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
fault
and cap rock seals
DOI:10.1306/1060756H23162
2005 by The American Association of Petroleum Geologists.
A Regional Analysis of
Fault
Reactivation and
Seal
Integrity Based on Geomechanical Modeling: An Example from the Bight Basin, Australia




S. D. Reynolds,1 E. Paraschivoiu,2 R. R. Hillis,1 G. W. O'Brien1
1Australian School of Petroleum, The University of Adelaide, Adelaide, South Australia, Australia
2Primary Industries and Resources of South Australia, Adelaide, South Australia, Australia
ACKNOWLEDGMENTS
Special thanks to Jennie Totterdell and Barry Bradshaw of Geoscience Australia for permission to use their fault
interpretation and for providing the digital
fault
files, to Peter Boult for valuable comments and suggestions, and to Primary Industries and Resources of South Australia Publishing Services for assistance with graphic files. Fugro Multi Client Services are thanked for permission to publish the seismic image in Figure 3. We thank David Castillo, Isabelle Moretti, and Signe Ottesen for their constructive comments regarding this manuscript.
ABSTRACT
The Bight Basin is a major frontier basin of Jurassic–Cretaceous age, which is currently undergoing renewed exploration interest. Although only limited data is available for understanding the petroleum systems in the basin, several observations indicate that poor fault
seal
integrity may represent a key exploration risk. The presence of a paleo-oil column in the Jerboa-1 well, interpreted gas chimneys, oil slicks, and asphaltite strandings indicate that
seal
failure caused by
fault
reactivation is potentially a significant issue in the Bight Basin. Thus, in this study, we investigated the likelihood that faults in the Bight Basin will undergo sufficient structural reactivation to induce
fault
seal
failure, under the regional in-situ stress field.
Fault
reactivation risk was assessed for two sets of faults that represent extensional events of Late Jurassic (Sea Lion faults) and Late Cretaceous age (Tiger faults).
Analysis of in-situ stress data suggests that the region is currently under a strike-slip or normal stress regime. Interpretation of borehole breakouts from six wells indicates the average maximum horizontal stress orientation is 130N. Although the magnitudes of the three principal stresses could not be unequivocally constrained, plausible ranges of values were determined based on well data. Pore pressure in wells in the region is hydrostatic except in Greenly-1, where moderate overpressure occurs.
This study assesses the risk of fault
reactivation using the
fault
analysis
seal
technology (FAST) technique. The FAST technique evaluates the increase in pore pressure (
P) required to cause reactivation as a measure of
fault
reactivation risk. In all cases investigated, faults striking 40(
15)
N of any dip are the least likely to be reactivated. Thus, traps requiring such faults to be sealing are the least likely to be breached.
Fault
reactivation risk for the strike-slip and normal stress regimes have been plotted in map view on a series of
fault
orientations for the Sea Lion and the Tiger faults using a range of hypothetical dips. The results for these hypothetical dips clearly demonstrate the importance of knowing both the strike and dip of a particular
fault
when conducting a three-dimensional
fault
seal
analysis, because the risk can range from relatively low risk at 25
dip to relatively high risk at 70
dip, with differences being more significant for certain
fault
orientations.
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