- Abstract:
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Seismological, GPS and historical data suggest that most of the 40 mm yr−1 convergence at the Hellenic Subduction Zone is accommodated through aseismic creep, with earthquakes of MW ≲ 7 rupturing isolated locked patches of the subduction interface. The size and location of these locked patches are poorly constrained despite their importance for assessment of seismic hazard. We present continuous GPS time-series covering the 2008 MW 6.9 Methoni earthquake, the largest earthquake on the subduct...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 11.5MB)
-
- Publisher copy:
- 10.1093/gji/ggw462
-
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- Publisher:
- Oxford University Press Publisher's website
- Journal:
- Geophysical Journal International Journal website
- Volume:
- 208
- Issue:
- 3
- Pages:
- 1592-1610
- Publication date:
- 2016-12-05
- Acceptance date:
- 2016-12-06
- DOI:
- EISSN:
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1365-246X
- ISSN:
-
0956-540X
- Pubs id:
-
pubs:687756
- URN:
-
uri:cd40df49-a164-4481-a356-46628a1dda90
- UUID:
-
uuid:cd40df49-a164-4481-a356-46628a1dda90
- Local pid:
- pubs:687756
- Copyright holder:
- England et al
- Copyright date:
- 2016
- Notes:
- © The Authors 2016. Published by Oxford University Press on behalf of The Royal Astronomical Society.
Journal article
The 2008 Methoni earthquake sequence: the relationship between the earthquake cycle on the subduction interface and coastal uplift in SW Greece
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