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180  4 Enhancing Geothermal Reservoirs
                              FMI (03.11.03)            FMI (03.11.03)            FMI (03.11.03)
                             Dynamic normalisation    Dynamic normalisation     Dynamic normalisation
                        N    E   S    W   N       N   E    S    W   N       N   E    S   W    N
                        Resistive     Conductive  Resistive     Conductive  Resistive    Conductive
                                             4151                     4199

























                                             4152                     4202
                               Figure 4.3  Formation MicroImaging mea-  opened by a massive waterfrac treatment.
                               surement in the borehole Groß Sch¨onebeck  The color scale runs from high electrical
                               3/90 exhibiting a ‘‘roll out’’ wall of the bore-  resistance (light) to low resistance (dark).
                               hole. The dark color shows a vertical fissure  (Please find a color version of this figure on
                               in the rough direction south-north which was the color plates.)

                               will help to clarify the structural controls on fold-related fracturing, which may
                               also comprise performing a fracture network modeling. All relevant upfront
                               investigations should be synoptically interpreted forming an integrated conceptual
                               3D subsurface model, which will ultimately build the base for the treatment design
                               and layout.



                               4.5
                               Definition and Description of Methods (Theoretical)

                               4.5.1
                               Hydraulic Stimulation

                               4.5.1.1 General
                               Since the early 1980s, research at various sites confirmed that shearing rather
                               than tensile fracturing is the dominant process (Pine and Batchelor, 1984; Baria
                               et al., 1999; Cornet, 1987). Natural joints, favorably aligned with the principal stress
                               directions, fail in shear. As a consequence, formations with high stress anisotropy
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