Stress field and tectonic regime of Central Iran from inversion of the earthquake focal mechanisms

Author:

Sheikholeslami Mohammad Reza,Mobayen Parisa,Javadi Hamid Reza,Ghassemi Mohammad R.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference116 articles.

1. Convergence history across Zagros (Iran): Constraints from collisional and earlier deformation;Agard;Int. J. Earth Sci.,2005

2. Zagros orogeny: a subduction-dominated process;Agard;Geol. Mag.,2011

3. Etude géologique de la région de Kalmard (W. Tabas);Aghanabati,1977

4. The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turanian active continental margin;Alavi;Geol. Soc. Am. Bull.,1997

5. Contrasting styles of convergence in the Arabia-Eurasia collision: why escape tectonics does not occur in Iran;Allen;Geol. Soc. Am. Spec. Pap.,2006

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