Articles | Volume 13, issue 3
https://doi.org/10.5194/se-13-553-2022
https://doi.org/10.5194/se-13-553-2022
Research article
 | 
17 Mar 2022
Research article |  | 17 Mar 2022

Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines

Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha

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Cited articles

Amato, V., Aucelli, P. P. C., Cesarano, M., Jicha, B., Lebreton, V., Orain, R., Pappone, G., Petrosino, P., and Russo Ermolli, E.: Quaternary evolution of the largest intermontane basin of the Molise Apennine (centralsouthern Italy), Rend. Lincei, 25, 197–216, https://doi.org/10.1007/s12210-014-0324-y, 2014. 
Amato, V., Aucelli, P. P. C., Bellucci Sessa, E., Cesarano, M., Incontri, P., Pappone, G., Valente, E., and Vilardo G.: Multidisciplinary approach for fault detection: integration of PS-InSAR, geomorphological, stratigraphic and structural data in the Venafro intermontane basin (Central–Southern Apennines, Italy), Geomorphology, 283, 80–101, https://doi.org/10.1016/j.geomorph.2017.01.027, 2017. 
Amato, V., Aucelli, P. P. C., Cesarano, M., Filocamo, F., Leone, N., Petrosino, P., Rosskopf, C. M., Valente, E., Casciello, E., Giralt, S., and Jicha, B. R.: Geomorphic response to late Quaternary tectonics in the axial portion of the Southern Apennines (Italy): A case study from the Calore River valley, Earth Surf. Proc. Land., 43, 2463–2480, https://doi.org/10.1002/esp.4390, 2018. 
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Ascione, A., Ciotoli, G., Bigi, S., Buscher, J., Mazzoli, S., Ruggiero, L., Sciarra, A., Tartarello, M. C., and Valente, E.: Assessing mantle versus crustal sources for non-volcanic degassing along fault zones in the actively extending southern Apennines mountain belt (Italy), Geol. Soc. Am. Bull., 130, 1697e1722, https://doi.org/10.1130/B31869.1, 2018. 
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Short summary
We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
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