253 8. Seismic anisotropy applied to geothermal prospection The compatibility between the attributes is again observable from the Top Keuper Mid horizon and below (Figure 8.14). Figure 8.12 AVAZ anisotropy at Top Cretaceous (left), Top Kimmeridgian (middle) and Top Dogger (right). Figure 8.13 VVAZ anisotropy at Top Cretaceous (left), Top Kimmeridgian (middle) and Top Dogger (right). Figure 8.14 AVAZ (left) and VVAZ (right) anisotropy at Top Keuper Mid level.
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