Seismic swarms and diffuse fracturing within Triassic evaporites fed by deep degassing along the low‐angle Alto Tiberina normal fault (central Apennines, Italy)

Author:

Piana Agostinetti Nicola1ORCID,Giacomuzzi Genny2,Chiarabba Claudio3

Affiliation:

1. Geophysics Section, School of Cosmic PhysicsDublin Institute for Advanced Studies Dublin Ireland

2. Istituto Nazionale di Geofisica e Vulcanologia Trento Italy

3. Centro Nazionale TerremotiIstituto Nazionale di Geofisica e Vulcanologia Rome Italy

Funder

Science Foundation Ireland Marie-Curie Action COFUND

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference65 articles.

1. Creep and locking of a low-angle normal fault: Insights from the Altotiberina fault in the Northern Apennines (Italy)

2. Fluid flow and seismicity pattern: Evidence from the 1997 Umbria-Marche (central Italy) seismic sequence

3. Balanced sections and seismic reflection profiles across the Central Apennines;Bally A. W.;Mem. Soc. Geol. Ital.,1986

4. Geometria delle deformazioni estensionali recenti nel bacino dell' Alta Val Tiberina fra S.Giustino Umbro e Perugia: Evidenze geofisiche e considerazioni geologiche;Barchi M.;Boll. Soc. Geol. Ital.,1999

5. Seismic images of an extensional basin, generated at the hangingwall of a low-angle normal fault: The case of the Sansepolcro basin (Central Italy)

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