Publication Date:
2017-04-04
Description:
The Gargano promontory is a ENE-WSW topographical and structural high located
at the inner border of the Apulia foreland. The post-Miocene tectonics of the Gargano
area is characterized mainly by E-W strike-slip and NW-SE normal faults, whose
present state of activity is debated, since there have been no large earthquakes in the
instrumental era. Still, the Gargano is well known as a seismically active zone: destructive
earthquakes (and even a tsunami) have occurred in historical times, with felt
effects up to XI MCS, although the exact location of the seismogenic sources is uncertain.
The level of background seismicity is low, with a maximum magnitude Mw=5.4
occurring in the central part of the promontory. We have investigated the surface deformation
in the area using the PS-InSAR processing technique. We have analysed 83
descending, and 31 ascending images, obtaining good coherence over about 200.000
Permanent Scatterers. We have modeled the ground velocity field using elastic dislocation
models and a non-linear inversion scheme. The modeling preliminary results
suggest that the area is presently accumulating strain along the E-W Mattinata fault,
with locking depths in the range 10 to 15 km
Description:
Published
Description:
Vienna, Austria
Description:
open
Keywords:
SAR
;
Inteferometry
;
Permanent Scatterers
;
Gargano
;
04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
;
04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring
;
04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy
;
04. Solid Earth::04.03. Geodesy::04.03.08. Theory and Models
;
04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques
Repository Name:
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Type:
Poster session
Format:
3064034 bytes
Format:
image/png
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