Active deformation in Zagros-Makran transition zone inferred from GPS measurements
نویسندگان
چکیده
منابع مشابه
Active deformation in Zagros–Makran transition zone inferred from GPS measurements
R. Bayer,1,∗ J. Chery,1 M. Tatar,2 Ph. Vernant,1,†M. Abbassi,2 F. Masson,1 F. Nilforoushan,3 E. Doerflinger,1 V. Regard4 and O. Bellier4 1Laboratoire Dynamique de la lithosphere, University of Montpellier II-CNRS , Pl. E. Bataillon, 34095 Montpellier Cedex 05, France 2International Institute of Earthquake Engineering and Seismology, Farmenieh, Dibaji, Arghavan St., n◦ 27, 19531, Tehran, Iran 3G...
متن کاملCrustal deformation along the Dead Sea Transform and the Carmel Fault inferred from 12 years of GPS measurements
[1] Large-scale crustal deformation in the Levant is mainly related to the DST and the CFS. The former is an active left lateral transform, bounding the Arabian plate and the Sinai sub-plate, and the latter branches out of the former and separates the Sinai sub-plate into two tectonic domains. In this study we obtain the velocities of 33 permanent GPS stations and 145 survey stations that were ...
متن کاملViscoelastic deformation from North Anatolian Fault Zone earthquakes and the eastern Mediterranean GPS velocity field
[1] We have modeled linear viscoelastic relaxation of a uniformviscosity asthenosphere following large earthquakes in the AegeanAnatolian region during the 20th century to evaluate whether this process contributes significantly to the regional velocity field. We address in particular whether southward motion of the Aegean Sea region relative to central Anatolia (and thus extension of western Tu...
متن کاملDeformation in the Jura Mountains (France): First results from semi-permanent GPS measurements
New GPS estimates of relative motion across the Jura Mountain Belt with respect to the Eurasian Plate indicate less than 1 mm/ yr of convergence, considerably less than previous estimates. Velocity uncertainties have been evaluated by several methods and range from 0.2 to 0.5 mm/yr for the semi-permanent stations. The major, statistically-significant strain feature inferred by the Jura GPS meas...
متن کاملCoseismic Deformation from the 1999 Mw 7.1 Hector Mine, California, Earthquake as Inferred from InSAR and GPS Observations
We use interferometric synthetic aperture radar (InSAR) and Global Positioning System (GPS) observations to investigate static deformation due to the 1999 Mw 7.1 Hector Mine earthquake, that occurred in the eastern California shear zone. Interferometric decorrelation, phase, and azimuth offset measurements indicate regions of surface and near-surface slip, which we use to constrain the geometry...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Geophysical Journal International
سال: 2006
ISSN: 0956-540X,1365-246X
DOI: 10.1111/j.1365-246x.2006.02879.x