افسری، ن.، تقی‌زاده فرهمند، ف.، قیطانچی، م. ر.، و سلیمانی، ا.، 1391. تغییرات عمق موهو در زیر زاگرس مرکزی (منطقه شیراز) با استفاده از امواج تبدیل یافته Ps: مجله علمی‌ ‌پژوهشی فیزیک زمین و فضا، شماره 38، جلد3. ص 13-1.

آقانباتی، س. ع.، 1383. زمین شناسی ایران: انتشارات سازمان زمین‌شناسی و اکتشاف معدنی کشور. 584 ص.

حسامی، خ.، جمالی، ف.، طبسی، ﻫ.، 1382. نقشه گسل های فعال ایران: پژوهشگاه بین المللی زلزله و مهندسی زلزله، گروه لرزه زمین ساخت، پژوهشکده زلزله شناسی.

فاطمی­زاده، آ. و تاتار، م.، 1385. تخمین ساختار سرعتی پوسته در ناحیه زاگرس مرکزی با استفاده از امواج شکست مرزی: فصلنامه علوم‌زمین، شماره60، ص 11-2.

Ajirlu, M. S., Moazzen, M., Hajialioghli, R., 2016. Tectonic evolution of the Zagros Orogen in the realm of the Neotethys between the Central Iran and Arabian Plates: An ophiolite perspective: Central European Geology, v. 59/x, p.1–27

Alavi, M., 1994. Tectonics of the Zagros orogenic belt of Iran: new data and interpretations: Tectonophysics, v229, p211-238.

Berberian, M., 1995. Master blind thrust faults hidden under the Zagros folds. Active basement tectonics and surface morphotectonics: Tectonophysics, v. 241, p.193-224.

Berberian, M. and Qorashi, M., 1986. General Geology and seismotectonics of the Chahar Mahal Bakhtiari Dam Site. Chahar Mahal Bakhtiari Dev. Proj., Plan and Budget Org. (in Persian).

Berberian, M. and King, G. C. P., 1981. Towards a paleogeography and tectonic evolution of Iran: Can. J. Earth Sci., v.18, p. 210–265.

Berberian, F., Muir, I. D., Pankhurst, R. J. and Berberian, M., 1982. Late Cretaceous and early Miocene Andean-type plutonic activity in northern Makran and Central Iran: J. Geol. Soc. London, v.139, p. 605-614.

Dehgani, G. A., and Makris, J., 1984. The Gravity field and crustal structure of Iran: N. Jb. GeoL. Palaont Abh., v.168, p. 215-229.

Faclon, N., 1974. Southern Iran: Zagros Mountain, in Mesozoic-Cenozoic Orogenic Belts: ed. Spencer, A. M., Spc. Publ. Geol. Soc. London, v. 4, p. 199-211.

Hatzfeld, D., Tatar, M., Priestley, K., and Ghafory-Ashtiany, M., 2003. Seismological constrains on the crustal structure beneath the Zagros mountain belt (Iran): Geophys. J. Int, v. 155, p. 403-410.

Jackson, J. A., McKenzi, D. P., 1984, Active tectonic of the Alpine- Himalayan belt between Western Turkey: Geophys. J. R. astr. Soc., v. 57, p. 209-229.

 Karasözen,  E.,  Nissen , E.,  Bergman E. A., Ghods, A., 2019, Seismotectonics of the Zagros (Iran) From Orogen‐Wide, Calibrated Earthquake Relocations: gir Solid Earth, v.124,p. 9109-9129.

Kaviani, A., Paul,, A., Bourova, E., Hatzfeld, D., Pederson, Mokhtari, M. A strong seismic velocity contrast in the shallow mantle across the Zagros collision zone (Iran): Geophys. J. Int., v. 171, p. 399–410

Kennett, B. L. N., and Engdahl, E. R., 1991. Travel times for global earthquake location and phase identification: Geophys. J. Int., v. 105, p. 429-465.

Laske, G., 2004. Map of the crustal thickness for Eurasia with1×1^◦resolution: http//mahi.uscd.edu/Gabi/rem.html.

http://www.irsc.ut.ac.ir

http://www.iiees.ac.ir

Molinaro, M., Zeyen, H., Laurencin, X., 2005. Lithospheric structure beneath the southeastern Zagros Mountains, Iran: recent slab break-off: Terra Nova, v. 17, p.1-6.

Nissen, E., Yamini-Fard, F., Tatar, M., Gholamzadeh, A., Bergman, E., Elliott, J.R., Jackson, J.A. & Parsons, B., 2010. The vertical separation of main shock rupture and Microseismicity at Qeshm Island in the Zagros Simply Folded Belt, Iran, Earth planet. Sci. Lett., 296, 181–194.

Paul, A., Kaviani, A., Hatzfeld, D., Vegne, J., and Mokhtari, M., 2006. Seismological evidence for crustal- scale thrusting in the Zagros mountain belt (Iran): Geophys. v. 166, p. 227–237.

Roustaei, M. et al., 2010. The 25 March 2006 Fin earthquakes (Iran) –insights into the vertical extents of faulting in the Zagros Simply Folded Belt, Geophys. J. Int., 181, 1275–1291.

Stocklin, J., 1968. Structural history and tectonics of Iran, A review: AAPG Bulletin v. 52, p.1229-1258.

Shad Manaman, N., Shomali, H., and Koyi, H., 2011. New constraints on upper-mantle S-velocity structure and crustal thickness of the Iranian plateau using partitioned waveform inversion: Geophys. J. Int., v. 184, p. 247–267.

Snyder, D. B. and Barazangi, M., 1986. Deep crustal structure and flexure of the Arbian Plate beneath the Zagros collisional mountain belt as inferred from gravity observations: Tectonics, v. 5, p. 361-373.

Taghizadeh-Farahmand, F., Sodoudi, F., and Afsari, N., 2015. Crustal thickness of Iran inferred from converted waves, 2014, Pure and Applied Geophysics journal, v. 172, p. 309–331.

Talebian, M. and Jackson, J., 2004. A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran, Geophys. J. Int., 156, 506–526.

Tatar, M., Hatzfeld, D., Ghafory-Ashtiany, M., 2004.  Tectonics of the Central Zagros (Iran) deduced from
microearthquake seismicity: Geophys. J. Int., v.156, p. 255–266.

Tatar, M., Nasrabadi et al., 2013. Crustal thickness variations in the Zagros continental collision zone (Iran) from joint inversion of receiver functions and surface wave dispersion: J. Seismol., v. 17, p. 1321–1337.

Vernant, Ph., Nilforoushan, F., Hatzfeld, D., Abbassi, M. R., Vigny. C., Masson, F., Nankali, H., Martinod, J., Ashtiani, A., Bayer, R., Tavakoli, F. and Chery, J., 2004. Present-day crustal deformation and plate kinematics in the   Middle East constrained by GPS measurements in Iran and northern Oman: Geophys. J. Int., v. 157, p. 381-398.

Vinnik, L. P., 1977.  Detection of waves converted from P to S_v in the mantle: Phys. Earth planet. Intre., v. 15, p. 39-45.

Yamini-Fard, F., Hatzfeld, D., Tatar, M. and Mokhtari, M., 2006. Microearthquake seismicity at the intersection between the Kazerun fault and the Main Recent Fault (Zagros, Iran): Geophys. J. Int., v. 166, p. 186-196.

Zhu, L., and Kanamori, H., 2000, Moho depth variation in southern California from teleseismic receiver functions, J. Geophys. Res., 105, 2969-2980.