Ragon T., Sladen A., Bletery Quentin, Vergnolle M., Cavalié O., Avallone A., Balestra J., Delouis B. (2019). Joint inversion of coseismic and early postseismic slipto optimize the information content in geodetic data : application to the 2009 M w 6.3 L'Aquila earthquake, central Italy. Journal of Geophysical Research : Solid Earth, 124 (10), 10522-10543. ISSN 2169-9313.
Titre du document
Joint inversion of coseismic and early postseismic slipto optimize the information content in geodetic data : application to the 2009 M w 6.3 L'Aquila earthquake, central Italy
Ragon T., Sladen A., Bletery Quentin, Vergnolle M., Cavalié O., Avallone A., Balestra J., Delouis B.
Source
Journal of Geophysical Research : Solid Earth, 2019,
124 (10), 10522-10543 ISSN 2169-9313
When analyzing the rupture of a large earthquake, geodetic data are often critical. These data are generally characterized by either a good temporal or a good spatial resolution, but rarely both. As a consequence, many studies analyze the coseismic rupture with data that also include one or more days of early postseismic deformation. Here, we invert simultaneously for the coseismic and postseismic slip with the condition that the sum of the two models remains compatible with data covering the two slip episodes. We validate the benefits of this approach with a toy model and an application to the 2009 M w 6.3 L'Aquila earthquake, using a Bayesian approach and accounting for epistemic uncertainties. For the L'Aquila earthquake, we find that if early postseismic deformation is not an explicitly acknowledged coseismic signal, coseismic slip models may overestimate the peak amplitude while long-term postseismic models may largely underestimate the total postseismic slip amplitude. This example illustrates how the proposed approach could improve our comprehension of the seismic cycle, fault frictional properties, and the spatial and temporal relationship between seismic rupture, afterslip, and aftershocks.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020]
;
Géophysique interne [066]
