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Active deformation in Zagros-Makran transition zone inferred from GPS measurements
Bayer R., Chery J., Tatar M., Vernant P., Abbassi M., Masson F., Nilforoushan F., Doerflinger E., Regard V., Bellier O.
Geophysical Journal International 165 (2006) 373-381 - http://hal.archives-ouvertes.fr/hal-00321128
Article in peer-reviewed journal
Sciences of the Universe/Earth Sciences
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. Regard 4, O. Bellier 5
1:  Laboratoire Dynamique de la Lithosphère (LDL)
http://www.dstu.univ-montp2.fr/GTS/index.html
CNRS : UMR5573 – INSU – Université Montpellier II - Sciences et techniques
Univ. Montpellier II - CC. 60 Place Eugène Bataillon 34095 MONTPELLIER CEDEX 5
France
2:  International Institute of Earthquake Engineering and Seismology (IIEES)
International Institute of Earthquake Engineering and Seismology
P O Box 19395/3913, Tehran, Iran
Iran, Islamic Republic Of
3:  National Cartographic Center of Iran (NCC)
National Cartographic Center of Iran
Azadi Square, Meraj Avenue, P.O.Box: 13185-1684, Tehran, Iran
Iran, Islamic Republic Of
4:  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
5:  Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE)
http://www.cerege.fr
CNRS : UMR6635 – Institut de recherche pour le développement [IRD] – INSU – Université de Provence - Aix-Marseille I – Université Paul Cézanne - Aix-Marseille III
CEREGE EUROPOLE MEDITERR. DE L'ARBOIS - BP 80 13545 AIX EN PROVENCE CEDEX 4
France
The Bandar Abbas-Strait of Hormuz zone is considered as a transition between the Zagros collision and the Makran oceanic subduction. We used GPS network measurements collected in 2000 and 2002 to better understand the distribution of the deformation between the collision zone and the Makran subduction. Analysing the GPS velocities, we show that transfer of the deformation is mainly accommodated along the NNW-SSE-trending reverse right-lateral Zendan-Minab-Palami (ZMP) fault system. The rate is estimated to 10 +/- 3 mm yr-1 near the faults. Assuming that the ZMP fault system transfers the motion between the Makran-Lut Block and the Arabian plate, we estimate to 15 mm yr-1 and 6 mm yr-1, respectively, the dextral strike-slip and shortening components of the long-term transpressive displacement. Our geodetic measurements suggest also a 10-15 km locking depth for the ZMP fault system. The radial velocity pattern and the orientation of compressive strain axes around the straight of Hormuz is probably the consequence of the subducting Musandam promontory. The N-S Jiroft-Sabzevaran (JS) fault system prolongates southwards the dextral shear motion of the Nayband-Gowk (NG) fault system at an apparent rate of 3.1 +/- 2.5 mm yr-1. The change from strong to weak coupling for underthrusting the Arabian plate beneath the Zagros (strong) and the Makran (weak) may explain the dextral motion along the ZMP, JS/NG and Neh-Zahedan fault systems which transfer the convergence from a broad zone in the western Iran (Zagros, Tabriz fault system, Alborz, Caucasus and Caspian sea surroundings) to Makran subduction.
English

Geophysical Journal International
Publisher Oxford University Press (OUP): Policy P - Oxford Open Option A
ISSN 0956-540X (eISSN : 1365-246X)
international
2006-04
165
373-381