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The deviation pattern between SYNPRK-path and SYNPRK responses is similar to the differences between observed and modelled field data (arrows in Figs 10a and b). This suggests that a CP linking the HCZ with surface could exists but this feature is not recovered by 3-D inversion given the specified error bounds and chosen regularization. In the 3-D inversions the HCZ exhibits a similar across-strike extent of 10–15 km beneath all profiles at approximately 15–20 km depth (Fig. 12d). This is consistent with the synthetic studies for which we observed similarly narrower low-resistive zones for the SYNPRK and SYPRK-path data when compared to 2-D results ( cf. Fig. 11). For 3-D, along-strike variability is suppressed, as a relatively strong smoothing is applied. Applying a lower regularization parallel to the SAF, however, leads to a generally feebler expression of the deep structures, but not more pronounced along-strike variations. As 3-D MT inversion is strongly ill-posed, inversion parameters should be systematically investigated. Appropriate choices for model and data parameters are interrelated and specific for each data set. Seja o primeiro a avaliar ofertas beta “Eclipse Master – Linha Master” Cancelar resposta.
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