Fig. 8. Gravity forward model along the seismic profile. A 2D gravity forward model is suggested by using all available constraints from gravity field (A, B), geologic map (A), rock type with densities (C), and spatial distribution of seismic reflectivities (Malehmir et al., 2022). The final model indicates that the prominent gravity lows (DF, SF1~SF3 in B) are mainly affected by the fault cores, which are characterized by low densities about 15% less than surroundings.

Econ. Environ. Geol. 2022;55:633-48 https://doi.org/10.9719/EEG.2022.55.6.633

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