[1] حسامی، خ.، جمالی، ف.، طبسی، ه (1382) نقشه گسلهای فعال ایران، پژوهشگاه بینالمللی زلزلهشناسی و مهندسی زلزله.
[2] علیپور، ر.، پورکرمانی، م.، زارع، م.، اسپندار، ر (1389) استخراج اتوماتیک خطوارههای مرتبط با زون گسلی جوان اصلی زاگرس در جنوب لرستان و مقایسه آن با برداشتهای صحرایی، مجله علوم پایه دانشگاه آزاد اسلامی(JSIAU) ، جلد 20، شماره 77، ص 184-173.
[3] Agard, P., Omrani, J., Jolivet, L., Mouthereau, F (2005) Convergence history across Zagros (Iran): constraints from collisional and earlier deformation. International Journal of Earth Sciences. 94, 401– 419.
[4] Alavi, M (1980) Tectonostratigraphic evolution of the Zagrosides of Iran. Geology. 8, 144–149.
[5] Alavi, M (1994) Tectonics of the Zagros orogenic belt of Iran: new data and interpretations. Tectonophysics. 229, 211-238.
[6] Allen, M.B., Ghassemi, M.R., Shahrabi, M., Qorashi, M (2003) Accommodation of late Cenozoic oblique shortening in the Alborz range, northern Iran. Journal of Structural Geology 25, 659–672.
[7] Allen, M.B., Jackson, J., Walker, R (2004) Late Cenozoic reorganization of the Arabia– Eurasia collision and comparison of the short-term and long-term deformation rates. Tectonics. 23, TC2008, doi: 10.1029/2003TC001530.
[8] Alipoor, R., Poorkermani, M., Zare, M., El Hamdouni, R (2012) Active tectonic assessment around Rudbar Lorestan dam site, High Zagros Belt (SW of Iran). Geomorphology, 128, 1–14.
[9] Axen, G.J., Lam, P.J., Grove, M., Stockli, D.F., Hassanzadeh, J (2001) Exhumation of the west‐central Alborz Mountains, Iran, Caspian subsidence, and collision‐related tectonics. Geology 29, 559–562.
[10] Berberian, M., King, G.C.P (1981) Toward a paleogeography and tectonic evolution of Iran, Canad. J. Earth Sci. 18, 210-265.
[11] Berberian, M (1995) Master blind thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics. Tectonophysics. 241, 193–224.
[12] Blanc, E.J.P., Allen, M.B., Inger, S., Hassani H (2003) Structural styles in the Zagros Simple Folded Zone. Iran. Journal of the Geological Society of London. 160, 401–412.
[13] Corgne, S., Magagi, R., Yergeau, M., Sylla, D (2010) An integrated approach to hydro-geological lineament mapping of a semi-arid region of West Africa using Radarsat-1 and GIS. Remote Sensing of Environment, 114, p. 1863–1875.
[14] Dercourt, J., Ricou, L.E., Vrielynck, B (1993) Atlas Tethys Palaeo environmental maps, 14 maps, 1 pl. Paris: Gauthier-Villars.
[15] Dercourt, J., Zonenshain, L.P., Ricou, L.E., Kazmin, V.G., Le pichon, X., Knipper, A.L., Grandjacquet, C., Sbortshikov, I.M., Geyssant, J., Lepvrier, C., Pechersky, D.H., Boulin, J., Sibuet, J.C., Savostin, L.A., Sorokhtin, O., Westphal, M., Bazhenov, M.L., Lauer, J.P., BijuDuval, B (1986) Geological evolution of the Tethys belt from the Atlantic to the Pamirs since the LIAS. Tectonophysics. 123, 241–315.
[16] Dewey, J.F., Pitman III, W.C., Ryan, W.B.F., Bonini, J (1973) Plate tectonics and the evolution of the Alpine System. In: Geological Society of America Bulletin. 84, 3137–3180.
[17] Falcon, N.L (1974) Southern Iran: Zagros Mountains. Mesozoic–Cenozoic Orogenic Belts, Data for Orogenic Studies: Geol. Soc. Spec. Publ. London, 4, pp. 199–211.
[18] Hafkenscheid, E., Wortel, M.J.R., Spakman, W (2006) Subduction history of the Tethyan derived seismic tomography and tectonic reconstruction. Journal of Geophysical Research 111, B08401, doi:10.1029/2005JB003791, 26 p.
[19] Jackson, J.A., McKenzie, D.P (1984) Active tectonics of Alpine–Himalayan belt between western Turkey and Pakistan. Geophysical. Journal of the Royal Astronomical Society. 77, 185–264.
[20] Koop, W.J., Stoneley, R (1982) Subsidence history of the Middle East Zagros Basin, Permian to Recent. Philosophical Transactions of the Royal Society of London. Series A. 305, 149–168.
[21] Kim, Y.S., Peacock, D.C.P., Sanderson, D.J (2002) Fault damage zones. Journal of Structural Geology. 26, 503–517
[22] Koike, K., Nagano, S., Ohmi, M (1995) Lineament analysis of satellite image using a Segment Tracing Algorithm [STA]. computer and geosciences. 21, 1091-1104.
[23] Koike, K., Nagano, S., Kawaba, K (1998) Constraction and analysis of interpreted fracture plans through combination of satellite image derived lineaments and digital elevation model date. Computer and geosciences. 24, 573-583.
[24] Masoud, A., Koike, K (2006) Tectonic architecture through Landsat-7 ETM⁺/SRTM DEM-derived lineaments and relationship to the hydrogeologic setting in Siwa region, NW Egypt. African Earth Sciences. 45, 467-477.
[25] McClay, K.R., Whitehouse, P.S., Dooley, M., Richards, M (2004) 3D evolution of fold and thrust belts formed by oblique convergence. Marine and Petroleum Geology. 21, 857–877
[26] Mohajjel, M., Fergusson, C.L (2000) Dextral transpression in Late Cretaceous continental collision, Sanandaj- Sirjan zone, western Iran. Journal of Structural Geology 22, 1125-1139.
[27] Molinaro, M., Leturmy, P., Guezou, J.C., Frizon de Lamotte, D (2005) The structure and kinematics of the southeastern Zagros fold-thrust belt; Iran: from thin-skinned to thick-skinned tectonics. Tectonics. 24, TC3007, doi: 10.1029/2004TC001633.
[28] Navabpour, P., Angelier, J., Barrier, E (2007) Cenozoic post‐collisional brittle tectonic history and stress reorientation in the High Zagros Belt [Iran, Fars Province]. Tectonophysics 432, 101–131.
[29] Regard, V., Bollier, O., Thomas, J.C., Abbasi, M.R., Mercier, J., Shabanian, E., Feghhi, K., Soleymani, S (2004) Accommodation of Arabia–Eurasia convergence in the Zagros-Makran transfer zone, SE Iran: a transition between collision and Subduction through a young deformation system. In: Tectonics. 23, doi: 10.1029/2003TC001599 TC4007.
[30] Sarkarinejad, K (2007) Quantitative finite strain and kinematic flow analyses along the Zagros transpression zone. Iran Tectonophysics 442, 49e65.
[31] Sarkarinejad, K., Azizi, A (2008) Slip partitioning and inclined dextral transpression along the Zagros Thrust System, Iran. Journal of Structural Geology. 30, 116–136.
[32] Sarkarinejad, K., Faghih, A., Grasemann, B (2008) Transpressional deformations within the Sanandaj – Sirjan metamorphic belt (Zagros mountains, Iran). Journal of Structural Geology. 30, 818–826.
[33] Sarkarinejad, K., Partabian, A., Faghih, A., Kusky, T.M (2012) Usage of strain and vorticity analyses to interpret large-scale fold mechanisms along the Sanandaj - Sirjan metamorphic belt, SW Iran. Geological Journal 47, 99-110.
[34] Sengör, A.M.C., Altiner, D., Cin, A., Ustaömer, T., Hsü, K.J (1988) The origin and assembly of the Tethyside orogenic collage at the expense of Gondwana land. In Gondwana and Tethys (eds M. G. Audley-Charles & A. Hallam). Geological Society of London, Special Publication no. 37, 119-181.
[35] Sepehr, M., Cosgrove, J.W (2005) Role of the Kazerun fault zone in the formation and deformation of the Zagros Fold-Thrust Belt, Iran. Tectonics 24, TC5005, doi: 10.1029/2004TC001725.
[36] Stampfli, G.M., Borel, G. D (2002) A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. Earth and Planetary Science Letters. 196, 17–33.
[37] Stocklin, J (1968) Structural history and tectonics of Iran. A review. American Association of Petroleum Geologists Bulletin. 52, 1229–1258.
[38] Stöcklin, J (1977) Structural correlation of the Alpine ranges between Iran and Central Asia. Mém. Soc. géol. France. 8: 333-353.
[39] Takin, M (1972) Iranian Geology and Continental Drift in the Middle East. Nature. 235, 147–50.
[40] Talebian, M., Jackson, J (2002) Offset on the main recent fault of NW Iran and implications on the late Cenozoic tectonics of the Arabia–Eurasia collision zone. Geophysical Journal International. 150, 422–439.
[41] Tatar, M., Hatzfeld, D., Ghafory-Ashtiyani, M (2004) Tectonics of the Central Zagros (Iran) deduced from microearthquake seismicity. Geophysical Journal International. 156, 255–266.
[42] Tchalenko, J.S (1970) similarities between shear zones of different magnitudes. Bull. Ceol. Am. 81, 1625-1640
[43] 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. 277, 1–25.
[44] Turcotte. D.L (1997) Fractals and Chaos in Geology and Geophysic. Cambridge Univ. Press.
[45] Vernant, P., Nilforoushan, F., Hatzfeld, D., Abbassi, M., Vigny, C., Masson, F., Nankali, HMartinod, J., Ashtiani, A., Bayer, R., Tavakoli, F., Chéry, J (2004) Present‐day crustal deformation and plate kinematics in the Middle East constrained by GPS measurementsin Iran and northern Oman. Geophysical Journal International. 157, 381–398.
[46] Wellman, H.W (1966) Active wrench faults of Iran, Afghanistan and Pakistan. Geologische Rundschau. 55, 716–735.
[47] Ziegler, P.A., Stampfli, G.M (2001) Late Paleozoic-Early Mesozoic plate boundary reorganization: collapse of the Variscan orogen and opening of Neotethys. In: Cassinis, R. (Ed.), the Continental Permian of the Southern Alps and Sardinia (Italy) Regional Reports and General Correlations, Ed. 25. Annali Museo Civico Science Naturali, Brescia. 17–34.