
TY  - JOUR
A1  - Nelson, E. 
A1  - Hillis, R. 
A1  - Sandiford, M. 
A1  - Reynolds, S. 
A1  - Mildren, S. 
T1  - PRESENT-DAY STATE-OF-STRESS OF SOUTHEAST AUSTRALIA
JF  - The APPEA Journal
JO  - The APPEA Journal
Y1  - 2006
VL  - 46
IS  - 1
SP  - 283
EP  - 306
KW  - 
UR  - https://doi.org/10.1071/AJ05016 
N2  - There have been several studies, both published and unpublished, of the present-day state-of-stress of southeast Australia that address a variety of geomechanical issues related to the petroleum industry. This paper combines present-day stress data from those studies with new data to provide an overview of the present-day state-of-stress from the Otway Basin to the Gippsland Basin. This overview provides valuable baseline data for further geomechanical studies in southeast Australia and helps explain the regional controls on the state-of-stress in the area.Analysis of existing and new data from petroleum wells reveals broadly northwest&#x2013;southeast oriented, maximum horizontal stress with an anticlockwise rotation of about 15&#xb0; from the Otway Basin to the Gippsland Basin. A general increase in minimum horizontal stress magnitude from the Otway Basin towards the Gippsland Basin is also observed. The present-day state-of-stress has been interpreted as strike-slip in the South Australian (SA) Otway Basin, strike-slip trending towards reverse in the Victorian Otway Basin and borderline strike-slip/reverse in the Gippsland Basin. The present-day stress states and the orientation of the maximum horizontal stress are consistent with previously published earthquake focal mechanism solutions and the neotectonic record for the region. The consistency between measured present-day stress in the basement (from focal mechanism solutions) and the sedimentary basin cover (from petroleum well data) suggests a dominantly tectonic far-field control on the present-day stress distribution of southeast Australia. The rotation of the maximum horizontal stress and the increase in magnitude of the minimum horizontal stress from west to east across southeast Australia may be due to the relative proximity of the New Zealand segment of the plate boundary. 
ER  -

