Seismic potential on the northwestern Main Recent Fault (Iran) revealed by InSAR
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Elsevier BV
Reference10 articles.
1. Partitioning of strike-slip and covergent motion between Eurasia and Arabia in eastern Turkey and the Caucasus;Jackson;Journal of Geophysical Research: Solid Earth,1992
2. Talebian M., Jackson J., 2002. Offset on the Main Recent Fault of NW Iran and implications for the late Cenozoic tectonics of the Arabia-Eurasia collision zone. Geophysical Journal International, 150.
3. Spatial evolution of Zagros collision zone in Kurdistan, NW Iran: Constraints on Arabia-Eurasia oblique convergence;Sadeghi;Solid Earth,2016
4. Tchalenko, J. S., & Braud, J., 1974. Seismicity and structure of the Zagros (Iran): the Main Recent Fault between 33 and 35 N. Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 277(1262), 1-25..
5. Aftershocks study of the 2006 Silakhur earthquake (Zagros, Iran): seismological evidences for a pull-apart basin along the Main Recent Fault, Doroud segments;Sepahvand;Journal of seismology,2012
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