The role of active strike-slip faults and opposite vertical axis rotations in accommodating eurasia-arabia shortening in central iran

Author:

Mattei MassimoORCID,Cifelli FrancescaORCID,Alimohammadian Habib,Rashid Hamideh

Funder

Italian Ministry of Education and Research

Roma TRE University

Dipartimento di Eccellenza

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference49 articles.

1. Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates;Allen;Tectonics,2004

2. Right-lateral shear across Iran and kinematic change in the Arabia-Eurasia collision zone;Allen;’Geophysical Journal International’184,2011

3. The Dasht-e-Bayaz (Iran) earthquake of August 31, 1968: a field report;Ambraseys;Bull. seism. Soc. Am.,1969

4. Textural and geochemical studies of detrital Fe–Ti oxides and test of their validity in provenance determination, a case study from central Iran;Amini;J. Afr. Earth Sci.,2015

5. Tectono‐sedimentary evolution of the northern Iranian Plateau: insights from middle–late Miocene foreland‐basin deposits;Ballato;Basin Res.,2017

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