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Numerical modeling and GPS bring unexpected extension to light in the NW Iran. Philippe Vernant. GPS velocity field in Iran with respect to Eurasia. IIEES. NCC. Ph. Vernant - GSI – June 2007. GPS velocity field in Iran with respect to the Central Iranian Block. IIEES. NCC.
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Numerical modeling and GPS bring unexpected extension to light in the NW Iran Philippe Vernant
GPS velocity field in Iran with respect to Eurasia IIEES NCC Ph. Vernant - GSI – June 2007
GPS velocity field in Iran with respect to the Central Iranian Block IIEES NCC Ph. Vernant - GSI – June 2007
GPS velocity field in Iran with respect to Eurasia IIEES NCC
Linear increase of the velocities from the Black Sea to the Caspian Sea WNW ESE IIEES NCC
GPS, seismic cycle and fault slip rate Interseismic Coseismic Geologic + =
Interseismic modeling vl vl = (Vp /π) arctan (x/P) Savage and Burford, 1973 x
Block modeling of the NW Iranian deformation Ph. Vernant - GSI – June 2007
Block modeling of the NW Iranian deformation Ph. Vernant - GSI – June 2007
Equilibrium equations Boundary conditions Constitutive laws Initial conditions Numerical modeling of the earth dynamic
GPS velocity field with respect to Arabia McClusky et al. (2000; 2003), Vernant et al. (2004)
The Arabian plate motion seems constant since at least 10 Ma
Ph. Vernant - GSI – June 2007 Strain rate and velocity field Instrumental seismicity (Engdahl et al. 1998)
Two end member models Ph. Vernant - GSI – June 2007 Ph. Vernant - GSI – June 2007
Slab pull effects could explain the GPS and geological observations, but more work is needed … Ph. Vernant - GSI – June 2007 Ph. Vernant - GSI – June 2007
Thank you Ph. Vernant - GSI – June 2007