Page 202 - Reservoir Geomechanics
P. 202

184    Reservoir geomechanics







                                 X-STRUCTURE




                       Z-STRUCTURE
                                                      Y-STRUCTURE














                0       5       10 mi
                0            5            10 km

              Figure 6.10. A detailed stress map of an oil field in an area of active faulting as determined with
              four-arm caliper data. The length of the arrow corresponds to the quality of the data as explained in
              the text. Note that while the stress field shows many local variations due to the processes associated
              with active faulting and folding, these variations are straightforwardly mappable (courtesy
              D. Castillo).



              orthogonal pair measures a larger diameter. The logging tool does not rotate with depth
              in the breakouts. Washouts represent essentially complete failure of the wellbore such
              that both sets of arms of the four-arm caliper are larger than the diameter of the drill
              bit. Keyseats are an asymmetrical notching of the well caused by mechanical wear of
              the borehole at its top or bottom (or on the side of the well if there is a rapid turn in the
              well trajectory). It is also useful to use a wellbore deviation criterion to help distinguish
              keyseats from breakouts. Even in near-vertical wells, great care needs to be taken when
                                                                                     ◦
              considering enlargements of the wellbore that are essentially parallel (within 10–15 )
              to the well deviation direction as indicators of wellbore breakouts.
                Figure 6.10 is a detailed stress map of an oil field in central California constructed
              through analysis of breakouts with four-arm caliper data. The lengths of the individual
              wells correspond to the quality ranking (A, B or C) described in the next section. There
              are distinct variations in the direction of maximum horizontal stress from one part of
              the field to another due to the fact that this is an area of active reverse and strike-slip
              faulting (and folding). Nonetheless, the consistency of the stress measurements in each
              well (and between wells) is quite remarkable.
   197   198   199   200   201   202   203   204   205   206   207