Abstract
Systematic analog models are run to study the variation in deformation across basement steps in the Zagros fold-thrust belt. Our model results demonstrate that basement configuration/topography influences the sedimentation thickness and, hence, the kinematics and geometric evolution of the fold and thrust belt. The greater the difference in thickness between the adjacent cover units across a basement step, the sharper and clearer will be the offset of the deformation front. Based on model results, we conclude that in a fold-thrust belt, where basement step/topography is covered by a layer of ductile salt acting as a decollement, the effect of the salt decollement on the evolution of the belt is far greater than the effect of thickness variation of the cover units.
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References
Ala MA (1974) Salt diapirism in southern Iran. Am Assoc Pet Geol Bull 58:1758–1770
Allen MB, Talebian M (2011) Structural variation along the Zagros and the nature of the Dezful Embayment. Geol Mag 148:911–924
Ameen MS (1992) Effect of basement tectonics in hydrocarbon generation, migration and accumulation in northern Iraq. Am Assoc Pet Geol Bull 76(3):356–370
Bahroudi A, Koyi HA (2003) The effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: an analogue modeling approach. J Geol Soc Lond 160:719–733
Bahroudi A, Koyi HA (2004) Tectono-sedimentary framework of the Gachsaran formation in the Zagros foreland basin. Mar Pet Geol 21:1295–1310
Baker C, Jackson J, Priestley K (1993) Earthquakes on the Kazeroun line in the Zagros Mountains of Iran: strike-slip faulting within a fold and thrust belt. Geophys J Int 115:41–61
Barzegar F (1994) Basement fault mapping of E Zagros folded belt (SW Iran) based on space-born remotely sensed data. Proceeding of the 10th thematic conference on geologic remote sensing: exploration, environment and engineering 10:455–466, San Antonio, Texas, USA
Berberian M (1976) Contribution to the Seismo Tectonics of IRAN. Report II, Publication of Geological Survey of Iran No. 39, Tehran
Berberian M (1995) Master blind thrust faults hidden under the Zagros folds: active basement tectonics and surface morpho tectonics. Tectonophysics 241:193–224
Berberian M, King GCP (1981) Towards the paleogeography and tectonic evolution of Iran. Can J Earth Sci 18:210–265
Blanc EJP, Allen MB, Inger S, Hassani H (2003) Structural style in the Zagros simple folded zone, Iran. J Geol Soc London 160:401–412
Bonini M (2001) Passive roof thrusting and foreland-ward fold propagation in scaled brittle-ductile physical models of thrust wedges. J Geophys Res 106:2291–2311
Bourgeois F (1969) Kuh-e Bangestan: a model for cretaceous structures in Iran. Iranian Oil Operating Companies Report 89, Tehran
Buchanan PG, McClay KR (1991) Sandbox experiments of inverted listric and planar fault systems. Tectonophysics 188:97–115
Butler RWH, Coward MP, Harwood GM, Knipe R (1987) Salt: its control on thrust geometry, structural style and gravitational collapse along the Himalayan Mountain front in the salt range of northern Pakistan. In: Lerche I, O’Brien JJ (eds) Dynamical geology of salt and related structures. Academic Press, Orlando, pp 339–418
Chapple WM (1978) Mechanics of a thin-skinned fold-and-thrust belt. Geol Soc Am Bull 89:1189–1198
Cobbold PR, Rossello EA, Vendeville B (1989) Some experiments on interacting sedimentation and deformation above salt horizons. Bulleten de la Societe Geologique de France 8:453–460
Colman-Sadd SP (1978) Fold development in Zagros simply folded belt, Southwest Iran. Am Assoc Pet Geol Bull 62:984–1003
Costa E, Vendeville BC (2002) Experimental insights on the geometry and kinematics of fold-and-thrust belt above weak, viscous evaporatic decollement. J Struct Geol 24:1729–1739
Cotton JT, Koyi HA (2000) Modeling of thrust fronts above ductile and frictional detachments: application to structures in the salt range and Potwar Plateau, Pakistan. Geol Soc Am Bull 112:351–363
Davis DM, Engelder T (1985) The role of salt in fold-and-thrust belts. Techtonophysics 119:67–88
Davis DM, Engelder T (1987) Thin-skinned deformation over salt. In: Lerche I, O’Brien JJ (eds) Dynamical geology of salt and related structures. Academic Press, New York, pp 301–337
Davy P, Cobbold PR (1991) Experiments on shortening of 4-layer model of continental lithosphere. Tectonophysics 188:1–25
Dercourt J, Zonenshain LP, Ricou LE, Kazmin VG, Le Pichon X, Knipper AL, Grandjacquet C, Sbortshikov IM, Geyssant J, Lepvrier C, Pechersky DH, Boulin J, Sibuet JC, Savostin LA, Sorokhtin O, Westphal M, Bazhenov ML, Lauer JP, Biju-Duval B (1986) Geological evolution of the Tethys belt from the Atlantic to the Pamirs since the Lias. Tectonophysics 123:241–315
Dewey JF, Pitman WC, Ryan WBF, Bonnin J (1973) Plate tectonics and the evolution of the alpine system. Geol Soc Am Bull 84:3137–3180
Dixon JM, Liu S (1992) Centrifuge modeling of the propagation of thrust faults. In: McClay KR (ed) Thrust tectonicsm. Chapman and Hall, London, pp 53–69
Edgell HS (1996) Salt tectonism in the Persian Gulf basin. In: Alsop GI, Blundell DJ, Davison I (eds) Geological society of London, 100th edn. Special Publication, London, pp 129–151
Ellis S, Schreurs G, Panien M (2004) Comparisons between analogue and numerical models of thrust wedge development. J Struct Geol 26:1659–1675
Falcon NL (1961) Major earth-flexing in the Zagros Mountains of southwest Iran. Q J Geol Soc 117:367–376
Falcon NL (1969) Problems of relationship between surface structure and deep displacement illustrated by Zagros. In: Kent PE, Satterthawa GE, Spencer AM (eds) Time and place in orogeny, geological society of London, 2nd edn. Special Publication, London, pp 9–22
Falcon NL (1974) Southern Iran: Zagros Mountains. In: Spencer A (ed) Mesozoic-Cenozoic orogenic belts. Geological Society of London Special Publication 4:199–211
Farzipour Saein A, Yassagi A, Sherkati S, Koyi H (2009a) Basin evolution of the lurestan region in the zagros fold-and-thrust belt, Iran. J Petrol Geol 36:5–20
Farzipour Saein A, Yassagi A, Sherkati S, Koyi H (2009b) Mechanical stratigraphy and folding style of the Lurestan region in the Zagros fold thrust belt, Iran. J Geol Soc 166:1101–1115
Ghabeishavi A, Vaziri-Moghaddam H, Taheri A (2009) Facies distribution and sequence stratigraphy of the Coniacian–Santonian succession of the BangestanPalaeo-high in the Bangestan Anticline, SW Iran. Facies 55:243–257. doi:10.1007/s10347-008-0171-3
Harrison HL, Pattern BD (1995) Translation of salt sheets by basal shear, in Salt sediments and hydrocarbons: Gulf Coast section SEPM Foundation 16th annual conference, Dec 3–6, 99–107
Hart BB (1970a) The Kuh-e Bangestan Kuh-e Sawds Stratigraphical Survey. Iranian Oil Operating Companies, Report 1162, Tehran
Hart BB (1970b) Upper cretaceous palaeogeography, structural history and prospect of the Khuzestan Province. Iranian Oil Operating Companies, Report 1172, Tehran
Hart B B (1970c) Tectonic framework and paleogeography of the agreement area. Oil Service Company of Iran, Report 1179, Tehran
Hart BB, Setudehnia A (1969) The Kuh-e Mish. Geological Survey of Iranian Oil Operating Companies, Report 1143, Tehran
Haynes SJ, Mcquillan H (1974) Evolution of the Zagros suture zone, southern Iran. Geol Soc Am Bull 85:739–744
Henson FRS (1951) Observations on the geology and petroleum occurrences of the Middle East. Proceedings of the 3th World Petroleum Congress 1:118–140
Hessami K, Koyi HA, Talbot CJ (2001) The significance of strike-slip faulting in the basement of the Zagros fold-thrust belt. J Pet Geol 24:5–28
Hessami K, Nilforoushan F, Talbot CJ (2006) Active deformation within the Zagros Mountains deduced from GPS measurements. J Geol Soc London 163:143–148
Jackson J, Mckenzie DP (1984) Active tectonics of the alpine Himalayan belt between western Turkey and Pakistan. Geophys J Roy Astron Soc 77:185–264
Jackson J, Mckenzie DP (1988) The relationship between plate motions and seismic moment tensors, and the rates of active deformation in the Mediterranean and Middle East. Geophys J 93:45–73
Kent PE (1979) The emergent Hormuz salt plugs of southern Iran. J Pet Geol 2:117–144
Koop W, Stoneley R (1982) Subsidence history of the middle East Zagros Basin, Permian to recent. Philos Trans Royal Soc London 305:149–168
Koyi HA (1988) Experimental modeling of the role of gravity and lateral shortening in the Zagros mountain belt. Am Assoc Pet Geol Bull 72:381–1394
Koyi HA, Maillot B (2007) Quantifying the effect of ramp dip and friction on thickness change of hanging wall units. J Struct Geol 29:924–932
Koyi HA, Petersen K (1993) The influence of basement faults on the development of salt structures in the Danish Basin. Marin Petrol Geol 10:82–94
Koyi HA, Vendeville BC (2003) The effect of décollement dip on geometry and kinematics of model accretionary wedges. J Struct Geol 25(9):1445–1450
Koyi HA, Hessami K, Teixell A (2000) Epicenter distribution and magnitude of earthquakes in fold-thrust belts: insights from sandbox models. Geophys Res Lett 27:273–276
Koyi HA, Sans M, Bahroudi A (2004) Modeling the deformation front of fold-thrust belts containing multiple weak horizons. Bollettino di Geofisica Teorica ed Applicata 45:101–103
Letouzey J, Colletta B, Villay R, Chermette JC (1995) Evolution of salt related structures in compressional setting. In: Jackson MPA, Roberts DG, Snelson S (eds), Salt tectonic: a global perspective. American Association of Petroleum Geologists Bulletin Memoir 65:41–60
Liu H, McClay KR, Powell D (1992) Physical models of thrust wedges. In: McClay KR (ed) Thrust tectonics. Chapman and Hall, London, pp 71–81
Maillet B, Koyi HA (2006) Thrust dips and refraction in fault-bend faults: analogue experiments and theoretical predictions. J Struct Geol 28:36–49
Manafi M, Arian M (2008) Basement tectonic investigation of the Dezful embayment, between Kazeroun and Hendijan faults, Ph.d. thesis, research and science division of the Islamic Azad University, Tehran
Mann CD, Vita-Finzi C (1988) Holocene serial folding in the Zagros. In: Audley-Charles MT, Hallam A, Gondwana and Tethys. Geological Society of London, Special Publications 37:51–59
Marques FO, Cobbold PR (2002) Topography as a major factor in the development of arcuate thrust belts: insights from sandbox experiments. Tectonophysics 348:247–268
Marshak S, Wilkerson MS, Hsui AT (1992) Generation of curved fold-thrust belt: insight from simple and analytical models. In: McClay KR (ed) Thrust tectonics. Chapman and Hall, London, pp 83–92
McClay KR (1989) Analogue models of inversion tectonics. In: Cooper MA, Williams GD (eds) Inversion tectonics, Geological Society of London, Special Publication 44:41–59
McQuillan H (1973) A geological note on the Qir earthquake, SW Iran, April 1972. Geol Mag 110:243–248
Mcquillan H (1991) The role of basement tectonics in the control of sedimentary facies, structural patterns and salt plug emplacement in the Zagros fold belt of southwest Iran. J Southeast Asian Earth Sci 5(4):453–463
Molinaro M, Guezou JC, Leturmy P, Eshraghi SA, Frizon deLamotte D (2004) The origin of changes in structural style across the Bandar Abbas syntaxis, SE Zagros (Iran). Marin Petrol Geol 21(6):735–752
Molinaro M, Leturmy P, Guezou JC, Frizon Delamotte D, Eshraghi SA (2005) The structure and kinematics of the south-eastern Zagros fold-thrust belt, Iran: From thin skinned to thick skinned tectonics. Tectonics. doi:10.1029/2004Tc001633
Motiee H (1994) Stratigraphy of Zagros. Geological survey of Iran publications (in Farsi), Tehran
Motiee H (1995) Petroleum geology of Zagros. Geological survey of Iran Publications (in Farsi), Tehran
Mourgues R, Cobbold PR (2006) Sandbox experiments on gravitational spreading and gliding in the presence of fluid overpressures. J Struct Geol 28:887–901
Mouthereau F, Lacombe O, Meyer B (2006) The Zagros folded belt (Fars, Iran): constraints from topography and critical wedge modeling. Geophys J Int 165:336–356
Nilforoushan F, Koyi HA (2007) Displacement fields and finite strains in a sandbox model, simulating a fold-thrust belt. Geophys J Int 169:1341–1355. doi:10.1111/j.1365-246X.2007.03341.x
Nilforoushan F, Masson F, Vernant P, Vigny C, Martinod J, Abbassi M, Nankali H, Hatzfeld D, Bayer R, Tavakoli F, Ashtiani A, Doerflinger E, Daignières M, Collard P, Chéry J (2003) GPS network monitors the Arabia–Eurasia collision deformation in Iran. J Geodesy 77:411–422
Nilforoushan F, Koyi HA, Swantesson JOH, Talbot CJ (2008) Effect of basal friction on surface and volumetric strain in models of convergent settings measured by laser scanner. J Struct Geol 30:366–379
Nilfouroushan F, Pysklywec R, Cruden AR (2012) Sensitivity analysis of numerical scaled models of fold-and-thrust belts to granular material cohesion variation and comparison with analogue experiments. Tectonophysics 526:196–206. doi:10.1016/j.tecto.2011.06.022
Price NJ, Cosgrove JW (1990) Analysis of geological structures. Cambridge University Press, Cambridge
Sepehr M, Cosgrove JW (2004) Structural framework of the Zagros fold-thrust belt, Iran. Marine Petrol Geol 21:829–843
Sherkati S, Letouzey J (2004) Variation of structural style and basin evolution in the central Zagros (Izeh zone and Dezful Embayment), Iran. Marine Petrol Geol 21:535–554
Sherkati S, Molinaro M, Frizon de Lamotte D, Letouzey J (2005) Detachment folding in the Central and Eastern Zagros fold-belt (Iran): salt mobility, multiple detachments and late basement control. J Struct Geol 27:1680–1696
Stocklin J (1968) Structural history and tectonics of Iran, a review. Am Assoc Pet Geol Bull 52:1229–1258
Stockmal GS, Beaumont C, Nguyen M, Lee B (2007) Mechanics of thin-skinned fold and thrust belts: insights from numerical models. In: Sears JW, Harms TA, Evenchick CA (eds) Whence the Mountains? Inquiries into the Evolution of Orogenic Systems: A Volume in Honor of Raymond A, Price. Geological Society of America Special Paper. 433:63–98. doi:10.1130/2007.2433(04)
Storti F, McClay KR (1995) Influence of syntectonic sedimentation on thrust wedges in analogue models. Geology 23:999–1002
Szabo F, Kheradpir A (1978) Permian and triassic stratigraphy, Zagros basin, southwest Iran. J Pet Geol 1(2):57–82
Tabatabayi H (1991) The basement contour map of the South–East Iran. National Iranian Oil Company (in Farsi), Tehran
Tabatabayi H (2005) Satellite gravimetry of the persian golf, National Iranian Oil Company (in Farsi), Tehran
Talbot CJ (1992) Centrifuge models of Gulf of Mexico profiles. Marin Petrol Geol 9:412–432
Talbot CJ, Alavi M (1996) The past of a future syntaxis across the Zagros. In: Alsop GI, Blundell DJ, Davison I (eds) Salt tectonics. Geological Society of America, Special Publication 100:89–109
Thomas WA (1977) Evolution of Appalachian-Ouachita salients and recesses from reentrants and promontories in the continental margin. Am J Sci 277:1233–1278
Vernant Ph, Nilforoushan F, Hatzfeld D, Abbassi MR, Vigny C, Masson F, Nankali H, Martinod J, Ashtiani A, Bayer R, Tavakoli F, Chéry 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 157:381–398
Vidal-Royo O, Koyi HA, Munoz JA (2009) Formation of orogen-perpendicular thrusts due to mechanical contrasts in the basal décollement in the central external sierras (Southern Pyrenees, Spain). J Struct Geol 31(5):523–539
Vita finzi C (2001) Neotectonics at the Arabian plate margins. J Struct Geol 23:521–530
WalpersdorfA Hatzfeld D, Nankali H, Tavakoli F, Nilforoushan F, Tatar M, Vernant P, Chery J, Masson F (2006) Difference in the GPS deformation pattern of North and Central Zagros (Iran). Geophys J Int 167:1077–1088
Watson JF (1950) Preliminary note on the micropaleontology of the upper cretaceous marls of the central area Mountain Front, SE Iran. Iranian Oil Operating Companies, Report 791, Tehran
Weijermars R (1986) Flow behavior and physical chemistry of bouncing putties and related polymers in view of tectonic laboratory applications. Tectonophysics 124:325–358
Weijermars R, Jackson MPA, Vedeville BC (1993) Rheological and tectonic modeling of salt provinces. Tectonophysics 217:143–174
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AFS thanks the research and postgraduate office in University of Isfahan and Uppsala University for their support and acknowledges his wife for her help and kindness during the stay in Uppsala. We acknowledge M. Vatandoust for her help in preparation of some figures. The editors, Wolf-Christian Dullo and Wenjiao Xiao, and the detailed and constructive reviews of Yunpeng Dong and anonymous reviewer are acknowledged. Swedish Research Council (VR) funds HK and FN.
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Farzipour-Saein, A., Nilfouroushan, F. & Koyi, H. The effect of basement step/topography on the geometry of the Zagros fold and thrust belt (SW Iran): an analog modeling approach. Int J Earth Sci (Geol Rundsch) 102, 2117–2135 (2013). https://doi.org/10.1007/s00531-013-0921-5
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DOI: https://doi.org/10.1007/s00531-013-0921-5