The detectability of the deformation pattern produced by the June 15, 1995 Aigion Earthquake with DInSAR techniques is ensured by its magnitude (MW = 6.3), shallow depth and dip-slip mechanism. In this paper, stacking procedures are applied to a series of ERS interferograms in order to filter out from the differential phase field the atmospheric signal, and an a posteriori test is used to check the statistical properties of the atmospheric signal both in time and space. Based on the DInSARderived deformation pattern, a new fault model is proposed that takes into account the crustal layering of the western part of the Gulf of Corinth.
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|Titolo:||Refined InSAR derived fault model for the Mw=6.3, June 15, 1995 Aigion EQ (Greece)|
|Data di pubblicazione:||2006|
|Nome del convegno:||IEEE GOLD REMOTE SENSING CONFERENCE|
|Appare nelle tipologie:||4.1 Contributo in Atti di convegno|