کتابنگاری
داودی، ز. و یساقی،ع.،1390تأثیر فعالیت پهنه گسلی عرضی ایذه بر دگرریختیهای پوشش رسوبی در زاگرس چینخورده-رانده.فصلنامه علوم زمین دوره 20، 71-88.doi:
10.22071/GSJ.2011.55222
نجفی، م. و یساقی،ع.، 1388-شواهد ساختاری از عملکرد گسل عرضی نظام آباد بر پیشانی کمربند چین خورده-رانده زاگرس.فصل نامه زمین شناسی ایران سال3،37-45.
References
Agard, P., Omrani, J., Jolivet, L., Whitechurch, H., Vrielynck, B., Spakman, W. and Wortel, R. 2011- Zagros orogeny: a subduction-dominated process. Geological Magazine, 148(5-6), 692-725.
doi:10.1017/S001675681100046X.
Anderson, E., 1951- The dynamics of faulting. Oliver and Boyd, Ltd., London.
Angelier, J., 1989- From orientation to magnitudes in paleostress determinations using fault slip data. Journal of structural geology, 11(1-2), 37-50.
doi: 10.1016/0191-8141(89)90034-5.
Hessami, K., Koyi, H. A., Talbot, C. J., Tabasi, H., and Shabanian, E., 2001- Progressive unconformities within an evolving foreland fold–thrust belt, Zagros Mountains. Journal of the Geological Society, 158(6), 969-981.
doi: 10.1144/0016-764901-007.
Lacombe, O., Mouthereau, F., Kargar, S., Meyer, B., 2006- Late Cenozoic and modern stress fields in the western Fars (Iran): Implications for the tectonic and kinematic evolution of central Zagros TECTONICS, VOL. 25. doi.org/10.1029/2005TC001831.
McQuarrie, N., and Van Hinsbergen, D. J., 2013- Retrodeforming the Arabia-Eurasia collision zone: Age of collision versus magnitude of continental subduction. Geology, 41(3), 315-318.doi:10.1130/G33591.1.
McQuarrie, N., Stock, J. M., Verdel, C., and Wernicke, B. P., 2003- Cenozoic evolution of Neotethys and implications for the causes of plate motions. Geophysical research letters, 30(20). doi:10.1029/2003GL017992, 2003.
Mohajjel, M., and Fergusson, C. L., 2000- Dextral transpression in Late Cretaceous continental collision, Sanandaj–Sirjan zone, western Iran. Journal of Structural geology, 22(8), 1125-1139.
doi:10.1016/S0191-8141(00)00023-7.
Mohajjel, M., Fergusson, C. L., and Sahandi, M. R., 2003- Cretaceous–Tertiary convergence and continental collision, Sanandaj–Sirjan zone, western Iran. Journal of Asian Earth Sciences, 21(4), 397-412.
doi:10.1016/S1367-9120(02)00035-4.
Mouthereau, F., Lacombe, O., and Vergés, J., 2012- Building the Zagros collisional orogeny timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics, 532, 27-60.
doi: 10.1016/j.tecto.2012.01.022.
Navabpour, P., Angelier, J., and Barrier, E., 2007- Cenozoic post-collisional brittle tectonic history and stress reorientation in the High Zagros Belt (Iran, Fars Province). Tectonophysics, 432(1), 101-131.
doi:10.1016/j.tecto.2006.12.007.
Sadeghi, S., and Yassaghi, A., 2016- Spatial evolution of Zagros collision zone in Kurdistan, NW Iran: Constraints on Arabia-Eurasia oblique convergence. Solid Earth, 7(2), 659-672.
doi:10.5194/se-7-659-2016
Storti, F., Rossetti, F., Lufer, A. L., and Salvini, F., 2006- Consistent kinematic architecture in the damage zones of intraplate strike-slip fault systems in North Victoria Land, Antarctica and implications for fault zone evolution: Journal of Structural Geology, v. 28, no. 1, p. 50-63.
doi:10.1016/j.jsg.2005.09.004.
Yassaghi, A., 2006- Integration of Landsat imagery interpretation and geomagentic data on verification of deep-seated transverse fault lineaments in SE Zagros, Iran. International Journal of Remote Sensing. 27(20): 4529-4544,
doi:10.1080/01431160600661283.