NDLI: Investigating the seismic cycle in Italy by multitemporal analysis of ALOS and ERS/ENVISAT DInSAR data sets

Content Provider	IEEE Xplore Digital Library
Author	Tolomei, C. Atzori, S. Merryman, J.P. Pezzo, G. Salvi, S.
Copyright Year	2011
Description	Author affiliation: Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy (Tolomei, C.; Atzori, S.; Merryman, J.P.; Pezzo, G.; Salvi, S.)
Abstract	In this study, we performed a detailed survey of surface deformations occurred in two different regions in Italy. The first, located in Southern Italy, takes into consideration the causative fault of the 1908 Messina earthquake (Mw 7.1), that is an east-dipping normal-oblique fault lying under water along the Straits of Messina. The second site is the L'Aquila area (Central Italy), where a Mw 6.3 earthquake occurred on 6th, April 2009. The subsequent studies demonstrated that the best-fit solution for the main shock, retrieved by DInSAR data, is represented by a normal fault ∼16 km long and ∼12 km wide, with a small right-lateral component, dipping 47°SW with a maximum slip of ∼90 cm (Atzori et al., 2009) [1]. This study is completely carried out within the SiGRiS project, funded by the Italian Space Agency (ASI).
Starting Page	2492
Ending Page	2495
File Size	952408
Page Count	4
File Format	PDF
ISBN	9781457710032
ISSN	21537003
e-ISBN	9781457710056
DOI	10.1109/IGARSS.2011.6049717
Language	English
Publisher	Institute of Electrical and Electronics Engineers, Inc. (IEEE)
Publisher Date	2011-07-24
Publisher Place	Canada
Access Restriction	Subscribed
Rights Holder	Institute of Electrical and Electronics Engineers, Inc. (IEEE)
Subject Keyword	Time series analysis Interferometry Synthetic aperture radar Earthquakes Orbits L-band Cities and towns
Content Type	Text
Resource Type	Article

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