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  5. Uncovering deformation processes from surface displacements
 
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Uncovering deformation processes from surface displacements

Author(s)
Stramondo, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Trasatti, E.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Albano, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Moro, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Chini, M.  
Bignami, C.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Polcari, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Saroli, M.  
Università degli studi di Cassino e del Lazio meridionale  
Language
English
Obiettivo Specifico
1T. Geodinamica e interno della Terra
4T. Fisica dei terremoti e scenari cosismici
3V. Dinamiche e scenari eruttivi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Geodynamics   
Issue/vol(year)
/102 (2016)
Publisher
Elsevier
Pages (printed)
58-82
Date Issued
August 2016
DOI
10.1016/j.jog.2016.08.001
URI
https://www.earth-prints.org/handle/2122/10332
Subjects
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::04.03.09. Instruments and techniques  
04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics  
04. Solid Earth::04.06. Seismology::04.06.11. Seismic risk  
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics  
Subjects

SAR

InSAR

Earth observation

Surface displacements...

Satellite missions

Advanced InSAR

Earthquake studies

Volcanic studies

Tectonic process

Coseismic studies

Soil liquefaction

Post-seismic studies

Interseismic studies

Volcanic unrest

Pre-eruptive phase

Eruptive phase

Abstract
Today, satellite remote sensing has reached a key role in Earth Sciences. In particular, Synthetic ApertureRadar (SAR) sensors and SAR Interferometry (InSAR) techniques are widely used for the study of dynamicprocesses occurring inside our living planet. Over the past 3 decades, InSAR has been applied for mappingtopography and deformation at the Earth’s surface. These maps are widely used in tectonics, seismology,geomorphology, and volcanology, in order to investigate the kinematics and dynamics of crustal faulting,the causes of postseismic and interseismic displacements, the dynamics of gravity driven slope failures,and the deformation associated with subsurface movement of water, hydrocarbons or magmatic fluids.
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