The 2010-2011 Canterbury, New Zealand, seismic sequence: Multiple source analysis from InSAR data and modeling
The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a Mw7.1 earthquake and continued with large aftershocks with dramatic consequences, particularly for the city of Christchurch. We model the main earthquakes using InSAR data, providing displacement maps and the...
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| Published in | Journal of Geophysical Research: Solid Earth Vol. 117; no. B8 |
|---|---|
| Main Authors | , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Washington, DC
Blackwell Publishing Ltd
01.08.2012
American Geophysical Union |
| Subjects | |
| Online Access | Get full text |
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| Abstract | The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a Mw7.1 earthquake and continued with large aftershocks with dramatic consequences, particularly for the city of Christchurch. We model the main earthquakes using InSAR data, providing displacement maps and the respective modeling for the September 4th, 2010, February 22nd, 2011 and June 13th, 2011 events. Relocated aftershocks, field and GPS surveys are used to constrain models obtained by inversion of InSAR data; the fault slip distribution is retrieved with a variable patch size approach aimed at maximizing the spatial resolution on the fault plane. For the September 2010 earthquake we estimated significant slip values below 10 km depth; the calamitous February 2011 event in Christchurch is modeled with a double fault source with slip values less than 2 m down to 7 km depth; for the second June 13th event in Christchurch we identified a NW‐SE striking fault as responsible for the earthquake. Last, we introduce the use of InSAR coherence maps to quickly detect the areas subject to soil liquefaction in Christchurch, as shown for the two main events.
Key Points
We model with a full‐resolution approach the 2010‐2011 Canterbury sequence
We analyze the stress transfer between faults
We exploit coherence maps to detect soil liquefaction |
|---|---|
| AbstractList | The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a Mw7.1 earthquake and continued with large aftershocks with dramatic consequences, particularly for the city of Christchurch. We model the main earthquakes using InSAR data, providing displacement maps and the respective modeling for the September 4th, 2010, February 22nd, 2011 and June 13th, 2011 events. Relocated aftershocks, field and GPS surveys are used to constrain models obtained by inversion of InSAR data; the fault slip distribution is retrieved with a variable patch size approach aimed at maximizing the spatial resolution on the fault plane. For the September 2010 earthquake we estimated significant slip values below 10 km depth; the calamitous February 2011 event in Christchurch is modeled with a double fault source with slip values less than 2 m down to 7 km depth; for the second June 13th event in Christchurch we identified a NW‐SE striking fault as responsible for the earthquake. Last, we introduce the use of InSAR coherence maps to quickly detect the areas subject to soil liquefaction in Christchurch, as shown for the two main events.
Key Points
We model with a full‐resolution approach the 2010‐2011 Canterbury sequence
We analyze the stress transfer between faults
We exploit coherence maps to detect soil liquefaction The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a M w 7.1 earthquake and continued with large aftershocks with dramatic consequences, particularly for the city of Christchurch. We model the main earthquakes using InSAR data, providing displacement maps and the respective modeling for the September 4th, 2010, February 22nd, 2011 and June 13th, 2011 events. Relocated aftershocks, field and GPS surveys are used to constrain models obtained by inversion of InSAR data; the fault slip distribution is retrieved with a variable patch size approach aimed at maximizing the spatial resolution on the fault plane. For the September 2010 earthquake we estimated significant slip values below 10 km depth; the calamitous February 2011 event in Christchurch is modeled with a double fault source with slip values less than 2 m down to 7 km depth; for the second June 13th event in Christchurch we identified a NW‐SE striking fault as responsible for the earthquake. Last, we introduce the use of InSAR coherence maps to quickly detect the areas subject to soil liquefaction in Christchurch, as shown for the two main events. We model with a full‐resolution approach the 2010‐2011 Canterbury sequence We analyze the stress transfer between faults We exploit coherence maps to detect soil liquefaction |
| Author | Atzori, S. Pasquali, P. Tolomei, C. Trasatti, E. Merryman Boncori, J. P. Salvi, S. Antonioli, A. Bannister, S. |
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| Copyright | 2012. American Geophysical Union. All Rights Reserved. 2015 INIST-CNRS |
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| Keywords | models inverse problem maps Australasia interferometry Complex system surveys liquefaction cartography urban areas earthquakes faults Modeling Global Positioning System depth slip displacements Radar observation fault planes aftershocks spatial resolution soils Synthetic aperture radar |
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| Snippet | The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a Mw7.1 earthquake and continued with large aftershocks with dramatic... The 2010–2011 Canterbury sequence is a complex system of seismic events that started with a M w 7.1 earthquake and continued with large aftershocks with... |
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| SubjectTerms | Canterbury Earth sciences Earth, ocean, space Exact sciences and technology InSAR liquefaction modeling seismic sequence stress transfer |
| Title | The 2010-2011 Canterbury, New Zealand, seismic sequence: Multiple source analysis from InSAR data and modeling |
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