2000
DOI: 10.1029/2000jb900148
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Active deformation of the Corinth rift, Greece: Results from repeated Global Positioning System surveys between 1990 and 1995

Abstract: Abstract.Between 1990 tectonic observations shows that these two earthquakes occurred on low-angle (_< 35 ø) north dipping normal faults located between 4.5 and 10 km depth in the inner part of the rift. Assuming that the deformation is concentrated in relatively narrow deforming zones, we use a simple model of a dislocation in an elastic half-space to study the implication of the localization. Using the geometry of the known seismogenic faults, our observations imply continuous aseismic deformation in the up… Show more

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Cited by 300 publications
(321 citation statements)
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“…In a similar way, from a corrected S R age estimate of 350-400 ka and GR ne twork values of 410-420 m in the central sector, we derive a minimum uplift rate of 1.05-1.2 mm year -1 for the penultimate uplift phase. (Backert et al, 2010;Briole et al, 2000).…”
Section: Synthesis Of the Resultsmentioning
confidence: 99%
“…In a similar way, from a corrected S R age estimate of 350-400 ka and GR ne twork values of 410-420 m in the central sector, we derive a minimum uplift rate of 1.05-1.2 mm year -1 for the penultimate uplift phase. (Backert et al, 2010;Briole et al, 2000).…”
Section: Synthesis Of the Resultsmentioning
confidence: 99%
“…show that most of present-day deformation is concentrated offshore in a narrow band (Briole et al, 2000;Avallone et al, 2004). In this area, the southern coast is bounded by the en-echelon Eliki-AigionKamarai-Psathopyrgos fault system (Fig.…”
Section: Introductionmentioning
confidence: 99%
“…Τελευταίες έρευνες με γεωδαιτικές μετρήσεις δείχνουν ότι η περιοχή του δυτικού Κορινθιακού διευρύνεται σε ΝΔ κατεύθυνση, με ρυθμό 1-1,5 cm/y, ενώ του ανατολικού με ρυθμό 0,5 cm/y (Billiris et al, 1991, Clarke et al, 1998, Briole et al, 2000. Στη περιοχή της βορείου Πελοποννήσου λόγω της νεοτεκτονικής παραμόρφωσης έχει διαπιστωθεί αναστροφή της ροής (ροή προς νότο), ορισμένων τμημάτων του άνω ρου του υδρογραφικού δικτύου (Zelilidis 2000).…”
Section: εισαγωγηunclassified