آقانباتی، ع. (1383). زمین شناسی ایران. تهران: انتشارات سازمان زمین شناسی اکتشافات معدنی کشور. 589 صفحه.
درویش زاده، ع. (1370). زمین شناسی ایران. تهران: امیرکبیر، انتشارات ندا.
شیخ الاسلامی، م. ر.، جوادی، ح. ر.، اسدی سرشار، م.، آقا حسینی، ا.، کوه پیما، م.، وحدتی دانشمند، ب. (1392). دانشنامه گسله های ایران. تهران: پژوهشکده علوم زمین سازمان زمین شناسی و اکتشافات معدنی کشور، انتشارات رهی.
Allen, M. B., Jackson, J. A., & Walker, R. (2004). Late Cenozoic reorganization of the Arabia-Eurasia collision and comparison of short-term and long-term deformation rates. Tectonics, 23, TC2008. doi: 10.1029/2003TC001530.
Allen, M.B., Saville, C., Blanc, E.J.-P., Talebian, M., & Nissen, E. (2013). Orogenic plateau growth: Expansion of the Turkish-Iranian Plateau across the Zagros fold-and-thrust belt. Tectonics, 32, 171–190.
Al-Lazki, A.I., Al-Damegh, K.S., El-Hadidy, S.Y., Ghods, A., & Tatar, M. (2014). Pn-velocity structure beneath Arabia–Eurasia Zagros collision and Makran subduction zones. Geological Society, London, Special Publications, 392, 45–60.
Ambraseys, N. N., & Melville, C. (1982). A History of Persian Earthquakes. Cambridge: Cambridge University Press.
Angelier, J. (2002). Inversion of earthquake focal mechanisms to obtain the seismotectonic stress IV—a new method free of choice among nodal lines. Geophysical Journal International, 150, 588–609.
Arthaud, F. (1969). Méthode de détermination graphique des directions de raccourcissement d’allongement et intermédiare d’une population de failles. Bulletin de la Société Géologique de France, 11, 729–737.
Berberian, M. (1976). Contribution to the seismotectonics of Iran (Part II). Tehran: Ministry of Industry and Mines, Geological Survey of Iran, Tectonic and Seismotectonic Section.
Burg, J. P. (2018). Geology of the onshore Makran
accretionary wedge: Synthesis and tectonic interpretation. Earth-Science Reviews. https://doi.org/10.1016/j.earthscirev.2018.09.011
Bott, M.H.P. (1959). The mechanics of oblique slip faulting. Geological Magazine, 96, 109–117.
Byrne, D. E., Sykes, L. R., & Davis, D. M. (1992). Great thrust earthquakes and aseismic slip along the plate boundary of the Makran Subduction Zone. Journal of Geophysical Research, 97(B1), 449–478.
Casciello, E., Vergés, J., Saura, E., Casini, G., Fernández, N., Blanc, E., Homke, S., & Hunt, D.W. (2009). Fold patterns and multilayer rheology of the Lurestan Province, Zagros simply folded belt (Iran). Journal of the Geological Society, 166(5), 947–959.
Compton, R.R. (1966). Analysis of Pliocene-Pleistocene deformation and stresses in northern Santa Lucia Range, California. Geological Society of America Bulletin, 77, 1361–1380.
Dahlen, F. A. (1984). Noncohesive critical Coulomb wedges: An exact solution. Journal of Geophysical Research, 89, 10125–10133. https://doi.org/10.1029/JB089iB12p10125
Delogkos, E., Childs, C., Manzocchi, T., Walsh, J.J., & Pavlides, S. (2017). The role of bed-parallel slip in the development of complex normal fault zones. Journal of Structural Geology. https://doi.org/10.1016/j.jsg.2017.02.014.
Dolati, A., & Burg, J.P. (2013). Preliminary fault analysis and paleostress evolution in the Makran Fold‐and‐Thrust Belt in Iran. In Al Hosani, K., Roure, F., Ellison, R., & Lokier, S. (Eds.), Lithosphere dynamics and sedimentary basins: The Arabian Plate and analogues (pp. 261–277). Heidelberg, Germany: Springer. https://doi.org/10.1007/978‐3‐642‐30609‐9_13
Dziewonski, A., Chau, T. A., & Woodhouse, J. H. (1981). Determination of earthquake source parameters from waveform data for studies of global and regional seismicity. Journal of Geophysical Research, 86, 2825–2852.
Ellouz-Zimmermann, N., et al. (2007b). Offshore frontal part of the Makran Accretionary Prism (Pakistan): the Chamak survey. In Lacombe, O., Lavé, J., Roure, F., & Vergès, J. (Eds.), Thrust belts and foreland basins: from fold kinematics to hydrocarbon systems (pp. 349–364). Berlin: Springer.
Frohling, E., & Szeliga, W. (2016). GPS constraints on interplate locking within the Makran subduction zone. Geophysical Journal International, 205(1), 67–76.
Grando, G., & McClay, K. (2007). Morphotectonics domains and structural styles in the Makran accretionary prism, offshore Iran. Sedimentary Geology, 196, 157–179.
Hardebeck, J.L., & Michael, A. J. (2006). Damped regional-scale stress inversions: methodology and examples for southern California and the Coalinga aftershock sequence. Journal of Geophysical Research, 111, B11310.
Harms, J.C., Cappel, H.N., & Francis, D.C. (1984). The Makran coast of Pakistan: its stratigraphy and hydrocarbon potential. In Haq, B.U., & Milliman, J.D. (Eds.), Marine Geology and Oceanography of Arabian Sea and Coastal Pakistan (pp. 3–27). New York: Van Nostrand Reinhold Co.
Hasegawa, A., Yoshida, K., & Okada, T. (2011). Nearly complete stress drop in the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake. Earth, Planets and Space, 63, 703–707. https://doi.org/10.5047/eps.2011.06.007
Hatzfeld, D., Authemayou, C., Van der Beek, P., Bellier, O., Lavé, J., Oveisi, B., Tatar, M., Tavakoli, F., Walpersdorf, A., & Yamini-Fard, F. (2010). The kinematics of the Zagros Mountains (Iran). In P. Leturmy & C. Robin (Eds.), Tectonic and stratigraphic evolution of Zagros and Makran during the Mesozoic-Cenozoic, vol 330. Geological Society, Special Publications, London, pp. 19–42.
Hatzfeld, D. (1999). The present-day tectonics of the Aegean as deduced from seismicity. Geological Society, London, Special Publications, 156(1), 415–426.
Hessami, K., Koyi, H. A., & Talbot, C. J. (2001). The significance of strike-slip faulting in the basement of the Zagros fold and thrust belt. Journal of Petroleum Geology, 24, 5–28.
Jackson, J. A. (1980). Reactivation of basement faults and crustal shortening in orogenic belts. Nature, 283, 343–346.
Jacob, K. H., & Quittmeyer, R. L. (1979). The Makran region of Pakistan and Iran: Trench-arc system with active plate subduction. In A. Farah & K. A. de Jong (Eds.), Geodynamics of Pakistan (pp. 305–317).
Kidd, R. G. W., & McCall, G. J. H. (1985). Plate tectonics and the evolution of Makran. In G. J. H. McCall (Ed.), East Iran Project, Area No. 1. Geological Survey of Iran, Report, 1, 564–618.
King, G. C. P., Bilham, R. G., Campbell, J. W., Mckenzie, D. P., & Niazi, M. (1975). Detection of elastic strain fields caused by fault creep events in Iran. Nature, 253, 420–423.
Kirby, S., Engdahl, R. E., & Denlinger, R. (1996). Intermediate-depth intraslab earthquakes and arc volcanism as physical expressions of crustal and uppermost mantle metamorphism in subducting slabs. Subduction: Top to Bottom, 96, 195–214.
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. doi:10.1098/rsta.1982.0031.
Kopp, C., Fruehn, J., Flueh, E. R., Reichert, C., Kukowski, N., Bialas, J., & Klaeschen, D. (2000). Structure of the Makran subduction zone from wide-angle and reflection seismic data. Tectonophysics, 329, 171–191.
Kukowski, N., Schillhorn, T., Flueh, E. R., & Huhn, K. (2000). A newly identified strike slip plate boundary in the northeast Arabian Sea. Geology, 28, 355–358.
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, 25, TC1003.
Maggi, A., Priastley, K., Jackson, J., & Baker, C. (2002). Focal depths of moderate and large size earthquakes in Iran. Journal of Seismology and Earthquake Engineering, 4, 1–10.
Maggi, A., Jackson, J. A., Priestley, K., & Baker, C. (2000). A reassessment of focal depth distributions in southern Iran, the Tien Shan, and northern India: Do earthquakes really occur in the continental mantle? Geophysical Journal International, 143, 629–661.
McQuarrie, N., Stock, J. M., Verdel, C., & Wernicke, B. P. (2003). Cenozoic evolution of Neotethys and implications for the causes of plate motions. Geophysical Research Letters, 30, 2036. doi:10.1029/2003GL017992.
Michael, A. J. (1984). Determination of stress from slip data: faults and folds. Journal of Geophysical Research, 89, 11517–11526.
Mirahmadi, Sh., Sadidkhouy, A., Javan-Doloei, Gh., & Mohammadi, N. (2024). Crustal seismic anisotropy beneath the Zagros and Central Iran. Vol. 58, No. 1, pp. 134–147.
Mokhtari, M., et al. (2019). A review of the seismotectonics of the Makran Subduction Zone as a baseline for Tsunami Hazard Assessments. Geoscience Letters, 6(13). doi:10.1186/s40562-019-0143-1 (in Persian).
Mokhtari, M., Abdoulahi Fard, I., & Hessami, K. (2008). Structural elements of the Makran region, Oman Sea, and their potential relevance to tsunamigenesis. Natural Hazards, 47, 185–199.
Mokhtari, M., Amjadi, A. A., Mahshadnia, L., & Rafzadeh, M. (2019). A review of the seismotectonics of the Makran Subduction Zone as a baseline for Tsunami Hazard Assessments. Geoscience Letters, 6(1), 1-9. https://doi.org/10.1186/s40562-019-0143-1.
Molinaro, N., Leturmy, P., Guezou, J. C., & Frizon de Lamotto, D. (2005). The structure and kinematics of the south-eastern fold-thrust belt, Iran: From thin-skinned to thick-skinned tectonics. Tectonics, 24, TC3007. doi:10.1029/2004TC001633.
Mostafazadeh, M., Alptekin, O., & Osman Oncel, A. (2000). Body waveform modeling of five moderately earthquakes in the Zagros fold thrust. Journal of Seismology and Earthquake Engineering, 2(3), 1-10.
Movaghari, R., Javan Doloei, G., & Hessami, K. (2024). Azimuthal seismic anisotropy of the Iran plateau: Insights from ambient noise analysis. Physics of the Earth and Planetary Interiors, 357, 107280. https://doi.org/10.1016/j.pepi.2024.107280.
Nissen, E., Yamini-Fard, F., Tatar, M., Gholamzadeh, A., Bergman, E., Elliott, J., Jackson, J., & Parsons, B. (2010). The vertical separation of mainshock rupture and microseismicity at Qeshm island in the Zagros fold-and-thrust belt, Iran. Earth and Planetary Science Letters, 296(3-4), 181–194.
Normand, R., Simpson, G., & Bahroudi, A. (2019). Extension at the coast of the Makran subduction zone (Iran). Terra Nova, 31, 503–510.
Okal, E. A., & Synolakis, C. E. (2008). Far-field tsunami hazard from mega-thrust earthquakes in the Indian Ocean. Geophysical Journal International, 172(3), 995–1015.
Penney, C., Tavakoli, F., Saadat, A. R., Nankali, H. R., Sedighi, M., Khorrami, F., Sobouti, F., Ra, Z., Cople, A., Jackson, J., & Priestley, K. (2017). Megathrust and accretionary wedge properties and behaviour in the Makran subduction zone. The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 42(4/W4).
Rostam, G. G., Pakzad, M., Noorbakhsh Mirzaei, N., & Sakhaei, S. R. (2018). Analysis of the stress field and strain rate in Zagros-Makran transition zone. Journal of Seismology, 22, 287–301.
Ruh, J. B. (2017). Effect of fluid pressure distribution on the structural evolution of accretionary wedges. Terra Nova, 29, 202–210. https://doi.org/10.1111/ter.12263.
Sarkarinejad, K., & Zafarmand, B. (2017b). Stress state and movement potential of the Kar-e-Bas fault zone, Fars, Iran. Journal of Geophysics and Engineering, 14, 998–1009. doi:10.1088/1742-2140/aa6f2f.
Sarkarinejad, K., & Zafarmand, B. (2017a). Tectonic stress and kinematic analyses of the Ghir fault zone, Zagros, Iran. Persian Geosciences, 26(102), 185–196.
Seno, T., & Yoshida, M. (2004). Where and why do large shallow intraslab earthquakes occur? Physics of the Earth and Planetary Interiors, 141(3), 183–206. https://doi.org/10.1016/j.pepi.2003.11.002.
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.
Shan, Y., Li, Z., & Lin, G. (2004). A stress inversion procedure for automatic recognition of polyphase fault/slip data sets. Journal of Structural Geology, 26(5), 919–925.
Smith, G., McNeill, L., Henstock, I. J., & Bull, J. (2012). The structure and fault activity of the Makran accretionary prism. Journal of Geophysical Research: Solid Earth, 117, B01312. https://doi.org/10.1029/2012JB009312.
Sonder, L. J. (1992). Effects of density contrasts on the orientation of stresses in the lithosphere: Relation to principal stress directions in the Transverse Ranges, California. Tectonics, 9, 761–771.
Song, T.-R. A., & Simons, M. (2003). Large trench-parallel gravity variations predict seismogenic behavior in subduction zones. Science, 301, 630–633. doi:10.1126/science.1085557.
Strasser, F. O., Arango, M. C., & Bommer, J. J. (2010). Scaling of the source dimensions of interface and intraslab subduction-zone earthquakes with moment magnitude. Seismological Research Letters, 81(6), 941–950.
Talebian, M., & Jackson, J. (2004). A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran. Geophysical Journal International, 156, 506-526.
Tatar, M., Hatzfeld, D., & Ghafori-Ashtiany, M. (2004). Tectonics of the central Zagros (Iran) deduced from microearthquakes seismicity. Geophysical Journal International, 156, 255–266.
Tatar, M., Hatzfeld, D., Martinod, J., Walpersdorf, A., Ghafori-Ashtiany, M., & Chery, J. (2002). The present-day deformation of the central Zagros from GPS measurements. Geophysical Research Letters, 29(19), 1927. doi: 10.1029/2002GL015427.
Vergés, J., Saura, E., Casciello, E., Fernandez, M., Villaseñor, A., Jimenez‐Munt, I., & García‐Castellanos, D. (2011). Crustal‐scale cross‐sections across the NW Zagros belt: Implications for the Arabian margin reconstruction. Geological Magazine, 148(5-6), 739–761. https://doi.org/10.1017/S0016756811000331.
Vernant, Ph., Nilforoushan, F., Hatzfeld, D., Abbasi, M. R., Vigny, C., Masson, F., Nankali, H., Martinod, J., Ashtiani, A., Bayer, R., Tavakoli, F., & Chery, J. (2004). Present-day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and Northern Oman. Geophysical Journal International, 157, 381-398.
Vigny, C., Huchon, P., Ruegg, J., Khanbari, K., & Asfaw, L. M. (2006). Confirmation of Arabia plate slow motion by new GPS data in Yemen. Journal of Geophysical Research, 111, B02402. doi:10.1029/2004JB003229.
Wallace, R. E. (1951). Geometry of shearing stress and relation to faulting. Journal of Geology, 59, 118–130.
Walpersdorf, A., Hatzfeld, D., Nankali, H., Tavakoli, F., Nilforoushan, F., Tatar, M., Vernant, P., Ch´ery, J., & Masson, F. (2006). Difference in the GPS deformation pattern of North and Central Zagros (Iran). Geophysical Journal International, 167, 1077–1088.
Wang, K. (2000). Stress–strain ‘paradox’, plate coupling, and forearc seismicity at the Cascadia and Nankai subduction zones. Tectonophysics, 319, 321–338. https://doi.org/10.1016/S0040‐1951(99)00301‐7.
Wells, R. E., Blakely, R. J., Sugiyama, Y., Scholl, D. W., & Dinterman, P. A. (2003). Basin-centered asperities in great subduction zone earthquakes: A link between slip, subsidence, and subduction erosion? Journal of Geophysical Research, 108(B10), 2507. doi:10.1029/2002JB002072.
White, R. S., & Louden, K. E. (1982). The Makran continental margin: Structure of a thickly sedimented convergent plate boundary. In J. S. Watkins & C. L. Drake (Eds.), Studies in continental margin geology. AAPG Special Volumes, 34, 499–518.
White, R. S. (1982). Deformation of the Makran accretionary sediment prism in the Gulf of Oman (northwest Indian Ocean). In J. K. Leggett (Ed.), Trench-Forearc Geology: Sedimentation and Tectonics on Modern and Ancient Active Plate Margins (Geological Society Special Publication, 10, 69–84).
YaminiFard, F., Hatzfeld, D., Farahbod, A., Paul, A., & Mokhtari, M. (2007). The diffuse transition between the Zagros continental collision and the Makran oceanic subduction (Iran): Microearthquake seismicity and crustal structure. Geophysical Journal International, 170, 182–194.
YaminiFard, F., Hatzfeld, D., Tatar, M., & Mokhtari, M. (2006). Microseismicity at the intersection between the Kazerun fault and the Main Recent Fault (Zagros-Iran). Geophysical Journal International, 166, 186–196.
