High‐Resolution Seismic Profiling in the Hanging Wall of the Southern Fault Section Ruptured During the 2016 M w 6.5 Central Italy Earthquake
Author:
Affiliation:
1. Istituto Nazionale di Geofisica e Vulcanologia Rome Italy
2. Centro di Geotecnologie Università di Siena San Giovanni Valdarno Italy
3. Università degli Studi di Napoli Federico II Napoli Italy
4. Horizon Union LDT Derby UK
Funder
Dipartimento della Protezione Civile, Presidenza del Consiglio dei Ministri
Istituto Nazionale di Geofisica e Vulcanologia
Università degli Studi di Siena
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021TC006786
Reference146 articles.
1. Earthquake synchrony and clustering on Fucino faults (Central Italy) as revealed from in situ36Cl exposure dating
2. Geological model of the central Periadriatic basin (Apennines, Italy)
3. Fault‐generated mountain fronts and the identification of fault segments: Implications for seismic hazard assessment;Blumetti A. M.;Bollettino Società Geologica Italiana,2007
4. Defining a model of 3D seismogenic sources for Seismic Hazard Assessment applications: The case of central Apennines (Italy)
5. Testing Different Tectonic Models for the Source of the Mw6.5, 30 October 2016, Norcia Earthquake (Central Italy): A Youthful Normal Fault, or Negative Inversion of an Old Thrust?
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