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  5. High-Resolution Densely Spaced Wide-Aperture Seismic Profiling as a Tool to Aid Seismic Hazard Assessment of Fault-Bounded Intramontane Basins: Application to Vallo di Diano, Southern Italy
 
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High-Resolution Densely Spaced Wide-Aperture Seismic Profiling as a Tool to Aid Seismic Hazard Assessment of Fault-Bounded Intramontane Basins: Application to Vallo di Diano, Southern Italy

Author(s)
Bruno, P. P.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Castiello, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Villani, F.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Improta, L.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Language
English
Obiettivo Specifico
2T. Tettonica attiva
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Bullettin Seismological Society of America  
Issue/vol(year)
3/103(2013)
Pages (printed)
1969-1980
Date Issued
June 1, 2013
DOI
10.1785/0120120071
URI
https://www.earth-prints.org/handle/2122/9306
Subjects
04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methods  
04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution  
Subjects

seismic imaging of a ...

Abstract
Seismic hazards in extensional regions are mostly posed by high-angle
normal faults and deep hanging-wall basins that can promote significant groundmotion
amplifications. Characterized by strong lateral velocity variations, these structures
represent challenging targets for seismic exploration. In this paper, we show that
prestack depth migration of high-resolution seismic-reflection data, collected with
nonconventional dense wide-aperture arrays, can effectively assist deterministic
seismic-hazard assessment of fault-bounded basins. Our high-resolution 3.2 km long
seismic profile was acquired along Vallo di Diano, the largest fault-bounded intramontane
basin in the southern Apennines seismic belt (Italy). The imaging strategy combines
prestack depth migration with an iterative velocity-building technique that
utilizes results of multiscale refraction tomography. In particular, migration of steeply
dipping reflections is essential in imaging the complex morphology of the basement
rocks beneath the basin. By combining seismic-reflection and VP tomography results
we were able to evaluate (1) the structure of the Vallo di Diano basin along a representative
transect from near-surface to basement depths; (2) the shallow-depth geometry
of the Vallo di Diano fault system, which bounds the basin to the east; (3) the
structure of the sediment–basement interface; and (4) the velocity structure of basement
and sediments within the basin. These findings are valuable both for understanding
the tectonic evolution of the Vallo di Diano and for developing earthquake-shaking
scenario studies.
Type
article
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BSSA_padula_2013.pdf

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Size

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Format

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Checksum (MD5)

857da37c82713a1f5131c3c78e6b1b27

rome library|catania library|milano library|napoli library|pisa library|palermo library
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