This paper has the aim to show a geological and
structural Meso-Cenozoic carbonatic bedrock below the
AAB obtained by 3D gravity model. Subsidence phenomena
occurrences along the western edge of the basin only, it is
the southern end of Tiberian Gravity Ridge detected in low
depth. The distribution of the phenomena of collapse and
sulfur springs are recognized along the NNE-SSW, NE-SW
and N-S gravity discontinuities where the seismicity of the
January 2001 shows the distribution of the areas with higher
macroseismic effects.Published267 - 2727A. Geofisica per il monitoraggio ambientale e geologia medicaN/A or not JC