Plan-view slices from the 3D ANT shear-wave velocity model at approximately 500, 900, 1,500 and 1,900 metres below surface. Black contours show the previously interpreted salt isopachs derived from active-seismic modelling, while solid and dashed black lines show mapped and inferred faults, respectively. The spatial association between the pre-existing salt interpretations and lower-velocity zones is approximate, and the ANT model did not independently resolve the boundaries of the interpreted salt structures. Source: CAUR Technologies Inc., Vortex Energy - Robinsons River Salt, CAU-25-023 - Ambient Noise Tomography Survey, Final Report.
Plan-view slices from the 3D ANT shear-wave velocity model at approximately 500, 900, 1,500 and 1,900 metres below surface. Black contours show the previously interpreted salt isopachs derived from active-seismic modelling, while solid and dashed black lines show mapped and inferred faults, respectively. The spatial association between the pre-existing salt interpretations and lower-velocity zones is approximate, and the ANT model did not independently resolve the boundaries of the interpreted salt structures. Source: CAUR Technologies Inc., Vortex Energy - Robinsons River Salt, CAU-25-023 - Ambient Noise Tomography Survey, Final Report.