Tectonic Evolution of the Southern Negros Geothermal Field and Implications for the Development of Fractured Geothermal Systems

Figure 9

Stereonet of the combined slip and dilation tendencies. Fracture planes are represented as poles. Regions of higher slip and dilation tendencies are shown in warm colors whilst areas with the lowest tendencies are in cold colours. Present-day stress conditions are based on the orientations in Rangin et al. [34]. For complete results on the various scenarios, refer to Pastoriza [27].