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  5. Did the September 2010 (Darfield) earthquake trigger the February 2011 (Christchurch) event?
 
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Did the September 2010 (Darfield) earthquake trigger the February 2011 (Christchurch) event?

Author(s)
Stramondo, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Kyriakopoulos, C.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Bignami, C.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Chini, M.  
Melini, D.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Moro, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Picchiani, M.  
Saroli, M.  
University of Cassino  
Boschi, E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia  
Language
English
Obiettivo Specifico
1.10. TTC - Telerilevamento
Status
Published
JCR Journal
N/A or not JCR
Peer review journal
Yes
Journal
Scientific Reports  
Issue/vol(year)
98/1 (2011)
Publisher
Nature
Pages (printed)
Article number:98
Date Issued
September 2011
DOI
10.1038/srep00098
URI
https://www.earth-prints.org/handle/2122/7439
Subjects
04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations  
Subjects

DInSAR

Coulomb Failure

Christchurch earthqua...

surface deformation

seismi source modelli...

Abstract
We have investigated the possible cause-and-effect relationship due to stress transfer between two
earthquakes that occurred near Christchurch, New Zealand, in September 2010 and in February 2011. The
Mw 7.1 Darfield (Canterbury) event took place along a previously unrecognized fault. The Mw 6.3
Christchurch earthquake, generated by a thrust fault, occurred approximately five months later, 6 km
south-east of Christchurch’s city center. We have first measured the surface displacement field to retrieve
the geometries of the two seismic sources and the slip distribution. In order to assess whether the first
earthquake increased the likelihood of occurrence of a second earthquake, we compute the Coulomb Failure
Function (CFF). We find that the maximum CFF increase over the second fault plane is reached exactly
around the hypocenter of the second earthquake. In this respect, we may conclude that the Darfield earthquake contributed to promote the rupture of the Christchurch fault.
Type
article
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2011_NatureSR_Stramondo_et_al.pdf

Size

2.77 MB

Format

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Checksum (MD5)

5bc1860a1d6c8009e7e1dd845ac3c764

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