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Minerals 2022, 12, x FOR PEER REVIEW 14 of 21 Minerals 2022, 12, 1236 14 of 21 Figure 11. Apparent resistivity (left) and phase (right) vs. time plots for ST-02 for different (color- Figure 11. Apparent resistivity (left) and phase (right) vs. time plots for ST-02 for different (color- coded) sampling rate frequencies (top) and the calculated average (bottom). coded) sampling rate frequencies (top) and the calculated average (bottom). Generally speaking, the aforementioned processing steps produced the impedance, Generally speaking, the aforementioned processing steps produced the impedance, tipper, and spectral density matrix in EDI files following the standard SEG format. The EDI tipper, and spectral density matrix in EDI files following the standard SEG format. The files can be imported to several commercial or academic software programs for further pro- EDI files can be imported to several commercial or academic software programs for fur- cessing, such as Interpex IX1D, WinGlink, Geotools, ZondMT2D, EMUPLUS, ModEM3D, ther processing, such as Interpex IX1D, WinGlink, Geotools, ZondMT2D, EMUPLUS, Mo- and others. dEM3D, and others. One dimensional (1D) analyses for each sounding for both MT and CSEM (LOTEM) One dimensional (1D) analyses for each sounding for both MT and CSEM (LOTEM) data were performed. Based on the average resistivity of the study area of 0.7 Ohm.m and data were performed. Based on the average resistivity of the study area of 0.7 Ohm.m and the frequency of the injected current (max of 100 s), a skin depth of 4.1 km was estimated the frequency of the injected current (max of 100 s), a skin depth of 4.1 km was estimated and used for all of our 1D inversions [46]. The 1D inversion for MT data was performed and used for all of our 1D inversions [46]. The 1D inversion for MT data was performed using Interpex IX1D software for XY, YX, and the invariant of both datasets using OCCAM’s using Interpex IX1D software for XY, YX, and the invariant of both datasets using OC- inversion technique. The different number of layers and various models such as Bostick and CAM’s inversion technique. The different number of layers and various models such as Niblett were also tested during the 1D analysis process. To apply an uncertainty analysis, Bostick and Niblett were also tested during the 1D analysis process. To apply an uncer- the model equivalence was used by indicating the range (thicknesses and resistivities) of tainty analysis, the model equivalence was used by indicating the range (thicknesses and models that could fit the acquired data. The 1D inversion results for MT data can be seen resistivities) of models that could fit the acquired data. The 1D inversion results for MT in Figure 12, with RMS varying between 1.2 to 4.9. data can be seen in Figure 12, with RMS varying between 1.2 to 4.9.PDF Image | First High-Power CSEM
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