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  5. 3D tomographic imaging of the southern Apennines (Italy): A statistical approach to estimate the model uncertainty and resolution
 
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3D tomographic imaging of the southern Apennines (Italy): A statistical approach to estimate the model uncertainty and resolution

Author(s)
De Matteis, R.  
GeDipartimento di Studi ologici e Ambientali, Università degli Studi del Sannio, Benevento,Italy  
Romeo, A.  
Dipartimento di Scienze Fisiche (RISSC-Lab), Università degli Studi di Napoli Federico II, Napoli, Italy  
Pasquale, G.  
Dipartimento di Studi Geologici e Ambientali, Università degli Studi del Sannio, Benevento,Italy  
Iannaccone, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Zollo, A.  
Dipartimento di Scienze Fisiche (RISSC-Lab), Università degli Studi di Napoli Federico II, Napoli, Italy  
Language
English
Obiettivo Specifico
4.1. Metodologie sismologiche per l'ingegneria sismica
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Stud. Geophys. Geod.  
Issue/vol(year)
/54 (2010)
Publisher
SPRINGER
Pages (printed)
367-387
Date Issued
2010
DOI
10.1007/s11200-010-0022-x
URI
https://www.earth-prints.org/handle/2122/6776
Subjects
04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy  
Subjects

error analysis

seismic tomography

southern Apennines

Abstract
A new dataset of first P-wave arrival times is used to derive the 3D tomographic
model of the Campania-Lucania region in the southern Apennines (Italy). We address the
issue related to the non-uniqueness of the tomographic inversion solution through massive
numerical experimentation based on the global exploration of the model parameter space
starting from a large variety of physically plausible initial models. The average of all the
realizations is adopted as the best-fit solution and the uncertainty of the model parameters
is studied using a statistical approach based on a Monte Carlo-type analysis. How the
uncertainty in the initial model, earthquake locations, and data influences the inversion
result is studied by considering separately the individual effects. Checkerboard tests are
performed to estimate the resolving power of the dataset. Re-located seismicity in
a reliable new 3D tomographic model allows us to correlate the earthquake distribution
with the main seismogenic structures present in the area.
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