A model for the hydrothermal tremor source of the Mefite d’Ansanto (Italy) CO2 non-volcanic emissions in the intermediate frequency band (1–15 Hz)

Author:

Morabito Simona,Cusano Paola,Nardone Lucia,Petrosino Simona

Publisher

Springer Science and Business Media LLC

Reference60 articles.

1. Chiodini, G. et al. Non-volcanic CO2 Earth degassing: Case of Mefite d’Ansanto (southern Apennines). Italy. Geophys. Res. Lett. 37, L11303 (2010).

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3. Patacca, E. & Scandone, P. Post-Tortonian mountain building in the Apennines. The role of the passive sinking of a relic lithospheric slab. In The Lithosphere in Italy: Advances in Earth Science Research (eds. Boriani, A., Bonafede, M., Piccardo, G.B. & Vai, G.B.), Atti dei Convegni Lincei 80, 157–176 (Accademia Nazionale dei Lincei, Rome, 1989).

4. Roure, F., Casero, P. & Vially, R. Growth processes and mélange formation in the southern Apennines accretionary wedge. Earth Planet. Sci. Lett. 102, 395–412 (1991).

5. Improta, L., Bonagura, M., Capuano, P. & Iannaccone, G. An integrated geophysical investigation of the upper crust in the epicentral area of the 1980, MS = 69, Irpinia earthquake (Southern Italy). Tectonophysics 361, 139–169. https://doi.org/10.1016/S0040-1951(02)00588-7 (2003).

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