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Before seismic data were made available, the subsurface setting of the Umbria-Marche area was mainly derived&#13; from the extrapolation of surface data and from models resulting from analogies with other mountain chains&#13; around the world. During the 90s industrial seismic data availability considerably increased, allowing the definition&#13; of new, previously unknown features. Beside the industrial seismic data availability, a deep crustal, near&#13; vertical seismic section trending E-W was acquired (CROP-03) across the Italian peninsula from the Tyrrhenian&#13; to the Adriatic coast. The subsurface data defined the compressional deformation style (thin- Vs thick- skinned)&#13; and the extensional deformation style. A set of east-dipping low-angle-normal faults, which dissect the previous&#13; compressional structures and which are the dominant features controlling the extension of the Apennines were&#13; recognised. The subsequent application of the seismic data interpretation to seismotectonic issues, defined in&#13; more detail the subsurface geometries of the active faults and the relationships between upper crust structure and&#13; seismicity

Seismic reflection data in the Umbria Marche Region: limits and capabilities to unravel the subsurface structure in a seismically active area