[1] بلورچی م. ح (1978) نقشه زمینشناسی 100000/1 ورقه آوج، سازمان زمینشناسی و اکتشافات معدنی کشور.
[2] بلورچی م. ح (1358) پژوهش زمینشناسی 250000/1 چهارگوش کبودرآهنگ، سازمان زمینشناسی و اکتشافات معدنی کشور.
[3] مجیدزاده ، ر.، حسینزاده م م.، اسماعیلی، ر (1390) ارزیابی کمی مورفوتکتونیک فعال در حوضههای البرزشمالی (حد فاصل شهرهای بهشر تا نکاء)، سیامین گردهمایی علوم زمین.
[4] Alipoor, R., Poorkermani, M., Zare, M., El Hamdouni, R (2011) Active tectonic assessment around Rudbar Lorestan dam site, High Zagros Belt (SW of Iran), Geomorphology, 128, p. 1–14.
[5] Berberian, M., King, G.C (1981) Towards a Paleogeography and Tectonic Evolution of Iran, Canadian Journal of Earth Sciences, 18, p. 210.
[6] Bull, W.B., McFadden, L.D (1977) Tectonic geomorphology north and south of the Garlock fault, California. In: Doehring, D.O. (Ed.), Geomorphology in Arid Regions. Proceedings of the Eighth Annual Geomorphology Symposium. State University of Nsew York, Binghamton, p.115–138.
[7] Byrd, J.O.D., Smith, R.B., Geissman, J.W (1994) The Teton fault, Wyoming: neotectonics, and mechanisms of deformation. J. Geophys. Res. 99 (B10), 20095–20122.
[8] Chen, Y.C., Sung, Q., Cheng, K.Y (2003) Along-strike variations of morphotectonic features in the Western Foothills of Taiwan: tectonic implications based on stream-gradient and hypsometric analysis. Geomorphology 56, 109–137.
[9] Chorowicz, J., Dhont, D., Gundogdu, N (1999) Neotectonics in the eastern North Anatolian fault region (Turkey) advocates crustal extension: mapping from SAR ERS imagery and Digital Elevation Model, J. Struct. Geol. 21, p. 511-532.
[10] Florinsky, I.V (1998) Combined analysis of digital terrain models and remotely sensed data in landscape investigations, Prog. Phys. Geogr. 22, p. 33–60.
[11] Hack, J.T (1973) Stream-profile analysis and stream-gradient index, Journal of Research of the U.S. Geological Survey 1 (4), p. 421–429.
[12] Hamdouni، R.El. Iriggaray، C. Fernandez، T. Chacon، J. Keller، E.A (2008) Assessment of relative active tectonics ، southwest border of the Sierra Nevada (Southern Spain), Geomorphology. 96, p.150-173.
[13] Hessami, K., Nilforoushan, F., Talbot, C.J (2006) Active deformation within the Zagros Mountains deduced from GPS measurements, Journal of the Geological Society of London 163, p. 143–148.
[14] Ioannis،M.T. Ioannis،K.K. Pavlides،S (2006) Tectonic geomorphology of the easternmost extension of the Gulf Corinth (Beotia، cnteral Greece), Tectonophysics Vol453 (2008) ، p. 211-232.
[15] Keller, E.A., Pinter, N (1996) Active Tectonic, Earthquake, Uplift and Landscape, Prentic Hall.
[16] Keller, E.A., Pinter, N (2002) Active Tectonics: Earthquakes, Uplift and Landscape, Second ed. Prentice Hall, NJ. 362.
[17] Keller, E.A., Gurrola, L., Tierney, T.E (1999) Geomorphic criteria to determine direction of lateral propagation of reverse faulting and folding, Geology 27, p .515–518.
[18] Koike. K, S. Nagano, 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, 573.
[19] Morisawa. M., and Hack, J.T (1985) Tectonic geomorphology. Boston, Unwin Hymen, P. 390.
[20] Rockweel, T.K., Keller, E.A., Johnson, D.L (1985) Tectonic geomorphology of alluvial fans and mountain fronts near Ventura, California. In: Morisawa, M. (Ed.), Tectonic Geomorphology. Proceedings of the 15th Annual Geomorphology Symposium. Allen and Unwin Publishers, Boston, MA, p. 183–207.
[21] Silva, P.G., Goy, J.L., Zazo, C., Bardajm, T (2003) Fault generated mountain fronts in Southeast Spain: geomorphologic assessment of tectonic and earthquake activity, Geomorphology 250, p. 203–226.
[22] Strahler, A.N (1952) Hypsometric (area-altitude) analysis of erosional topography. Geological Society of America Bulletin 63, 1117–1142.
[23] Troiani, F., Della Sata, M (2008) The use of the Stream Length–Gradient index in morphotectonic analysis of small catchments: A case study from Central Italy, Geomorphology, 102, p. 159-168.
[24] Verrios, S., Zygouri, V., Kokkalas, S (2004) Morphotectonic analysis in the Eliki fault zone (Gulf of Corinth, Greece). Bulletin of the Geological Society of Greece 36, 1706–1715.
[25] Yang، J.C (1985) Geomorphology (in Chinese), High Education press. Beijing, 320.
[26] Zovoili, E., Konstantinidi, E., Koukouvelas, I.K (2004) Tectonic geomorphology of escarpments: the cases of Kompotades and Nea Anchialos faults. Bulletin of the Geological Society of Greece 36, 1716–1725.