This study presents an integrated 3D crustal model of the Southern Apennines, a key area within this region, developed at a spatial resolution of 5x5x1 km3. The model synthesizes a wide array of geological and geophysical datasets, including stratigraphic well logs, lithological maps, seismic tomography, gravity and magnetic data, and thermal-petrophysical constraints. These inputs were rigorously processed to ensure spatial consistency and to capture depth-dependent properties such as thermal gradients and P-wave velocity variations. The model delineates major lithological units, from sedimentary covers and carbonate platforms to the crystalline basement, and identifies key intra-crustal discontinuities, extending down to the Moho. Validation against independent borehole and geophysical data confirms its accuracy. Beyond its scientific value, the model supports thermo-rheological analysis to investigate brittle-ductile transitions relevant to seismic risk, contributing to the TRHAM project (PRIN2022 PNRR).
An Integrated 3D Geological Model of Southern Italy: Insights from the TRHAM Project / Perrini, M.; Accomando, F.; Landro, G. De; Gola, G.; Tizzani, P.; Carafa, M.; Fedi, M.; Zollo, A.; Kastelic, V.; Lorenzo, C. Di; Naccio, D. Di; Taroni, M.; Castaldo, R.. - (2025), pp. 1-5. ( 31st Meeting of Environmental and Engineering Geophysics, Held at Near Surface Geoscience Conference and Exhibition, NSG 2025 ita 2025) [10.3997/2214-4609.202520267].
An Integrated 3D Geological Model of Southern Italy: Insights from the TRHAM Project
Perrini, M.;Accomando, F.;Landro, G. De;Carafa, M.;Fedi, M.;Zollo, A.Membro del Collaboration Group
;Castaldo, R.
2025
Abstract
This study presents an integrated 3D crustal model of the Southern Apennines, a key area within this region, developed at a spatial resolution of 5x5x1 km3. The model synthesizes a wide array of geological and geophysical datasets, including stratigraphic well logs, lithological maps, seismic tomography, gravity and magnetic data, and thermal-petrophysical constraints. These inputs were rigorously processed to ensure spatial consistency and to capture depth-dependent properties such as thermal gradients and P-wave velocity variations. The model delineates major lithological units, from sedimentary covers and carbonate platforms to the crystalline basement, and identifies key intra-crustal discontinuities, extending down to the Moho. Validation against independent borehole and geophysical data confirms its accuracy. Beyond its scientific value, the model supports thermo-rheological analysis to investigate brittle-ductile transitions relevant to seismic risk, contributing to the TRHAM project (PRIN2022 PNRR).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.


