
TY  - JOUR
A1  - Hillis, R.R. 
A1  - Williams, A.F. 
T1  - THE STRESS FIELD OF THE NORTH WEST SHELF AND WELLBORE STABILITY
JF  - The APPEA Journal
JO  - The APPEA Journal
Y1  - 1993
VL  - 33
IS  - 1
SP  - 373
EP  - 385
KW  - 
UR  - https://doi.org/10.1071/AJ92028 
N2  - Boreholes drilled in the search for hydrocarbons in the Barrow-Dampier Sub-Basin (North West Shelf, Australia) commonly exhibit an elliptical cross-section believed to be due to stress-induced wellbore failure known as borehole breakout. The azimuths of the long axes of 138 discrete breakouts identified in nine different wells in the Barrow-Dampier show a consistent 010&#xb0;&#x2212;030&#xb0;N trend implying that maximum horizontal compressive stress is oriented 100&#xb0;&#x2212;12G&#xb0;N.The orientation of horizontal stress determined in this study (and that from the Timor Sea area which is rotated some 50&#xb0;&#x2212;60&#xb0; with respect to the Barrow-Dampier) is consistent with that derived from theoretical modelling of the stress within the Indo-Australian plate based on the plate tectonic forces acting on its boundaries. The rotation of the horizontal stress orientations along the North West Shelf, between the Barrow-Dampier and the Timor Sea, is a reflection of the present-day complex plate convergence system at the north-eastern boundary of the Indo-Australian Plate.Vertical stress magnitudes, Sv, in the Barrow-Dampier were determined from density and sonic log data. Minimum and maximum horizontal stress magnitudes, Shmin and Shmax, were determined from mini-hydraulic fracture (or modified leak-off) test results. These data suggest that the fault condition of the Wanaea/Cossack area is on the boundary between normal faulting (extension) and strike-slip, i.e. Sv &#x2248; Shmax > Shmin. However, in other parts of the Barrow-Dampier the evidence suggests a strike-slip fault condition, i.e. Shmax > Sv > Shmin.Given the orientation of the stress field and the fault condition, inferences can be drawn regarding the stability of horizontal wells. Furthermore, experience from vertical wells can be utilized to determine the upper and lower bounds to the mud-weight envelope as functions of deviation and wellbore orientation. Since a horizontal well will see Sv and a horizontal stress, stress anisotropy around a wellbore in the Wanaea/Cossack area (and hence wellbore instability) will be minimized by drilling in the Shmin direction i.e. 010&#xb0;&#x2013;030&#xb0;N. 
ER  -

