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Kinematics and surface fracture pattern of the Anaran basement fault zone in NW of the Zagros fold–thrust belt

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Abstract

The preexisting north–south trending basement faults and their reactivation played an important role during the evolution of the Zagros fold–thrust belt. The Anaran Basement Fault (ABF) in the Lurestan region, NW of the Zagros, has been considered as a N–S trending basement lineament, although its surface structural expression is still debated. In this study, we use satellite images and field observations to identify and analyze the fractures in the sedimentary cover above the ABF. Fracture analysis demonstrates that approaching the ABF, the fracture pattern changes. The fractures association with reactivation of the deep-seated preexisting ABF can be categorized in four sets based on their directions. The mean direction for maximum compressional stress is different between the fault- and fold-related fractures within and around the ABF shear zone. We estimated an orientation of N30° ± 5° for the fault-related fractures and N45° ± 5° for the fold-related fracture sets outside of the ABF shear zone. This difference suggests that the fold-related and fault-related fracture sets have been formed in different two stages of deformation throughout the area. The axial traces of some folds, especially the Anaran anticline, demonstrate a right-lateral offset along the ABF, such that, in central part of the Anaran anticline, the fold axis of this anticline is changed from its original NW–SE trend to approximately north–south trend of the ABF.

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References

  • Agard P et al (2011) Zagros orogeny: a subduction-dominated process. Geol Mag 148:692–725

    Article  Google Scholar 

  • Ahmadhadi F, Lacombe O, Daniel J-M (2007) Early reactivation of basement faults in Central Zagros (SW Iran): evidence from pre-folding fracture populations in Asmari Formation and lower Tertiary paleogeography. In: Thrust belts and foreland basins. Springer, Berlin, pp 205–228

  • Ahmadhadi F, Daniel JM, Azzizadeh M, Lacombe O (2008) Evidence for pre-folding vein development in the Oligo–Miocene Asmari Formation in the Central Zagros Fold Belt, Iran. Tectonics. doi:10.1029/2006TC001978

    Google Scholar 

  • Alavi M (2007) Structures of the Zagros fold–thrust belt in Iran. Am J Sci 307:1064–1095

    Article  Google Scholar 

  • Allen MB (2010) Roles of strike-slip faults during continental deformation: examples from the active Arabia-Eurasia collision. Geol Soc Lond Spec Publ 338:329–344

    Article  Google Scholar 

  • Allen MB, Talebian M (2011) Structural variation along the Zagros and the nature of the Dezful Embayment. Geol Mag 148:911–924. doi:10.1017/S0016756811000318

    Article  Google Scholar 

  • Amrouch K, Lacombe O, Bellahsen N, Daniel JM, Callot JP (2010) Stress and strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain Anticline, Wyoming. Tectonics 29(TC1005):1–27. doi:10.1029/2009TC002525

    Google Scholar 

  • Anastasio DJ, Fisher DM, Messina TA, Holl JE (1997) Kinematics of décollement folding in the Lost River Range, Idaho. J Struct Geol 19:355–368

    Article  Google Scholar 

  • Aubourg C, Smith B, Bakhtari H, Guya N, Eshraghi A (2008) Tertiary block rotations in the Fars arc (Zagros, Iran). Geophys J Int 173:659–673

    Article  Google Scholar 

  • Authemayou C, Chardon D, Bellier O, Malekzadeh Z, Shabanian E, Abbassi MR (2006) Late Cenozoic partitioning of oblique plate convergence in the Zagros fold-and-thrust belt (Iran). Tectonics 25(TC3002):1–21. doi:10.1029/2005TC001860

    Google Scholar 

  • Bahroudi A, Koyi H (2003) Effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: an analogue modelling approach. J Geol Soc 160:719–733

    Article  Google Scholar 

  • Bahroudi A, Koyi HA (2004) Tectono-sedimentary framework of the Gachsaran Formation in the Zagros foreland basin. Mar Pet Geol 21:1295–1310

    Article  Google Scholar 

  • Bahroudi A, Talbot C (2003) The configuration of the basement beneath the Zagros basin. J Pet Geol 26:257–282

    Article  Google Scholar 

  • Baker C, Jackson J, Priestley K (1993) Earthquakes on the Kazerun line in the Zagros Mountains of Iran: strike-slip faulting within a fold-and-thrust belt. Geophys J Int 115:41–61

    Article  Google Scholar 

  • Bellahsen N, Fiore P, Pollard DD (2006) The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming. J Struct Geol 28:850–867

    Article  Google Scholar 

  • Berberian M (1995) Master “blind” thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics. Tectonophysics 241:193–224

    Article  Google Scholar 

  • Berberian M, King G (1981) Towards a paleogeography and tectonic evolution of Iran. Can J Earth Sci 18:210–265

    Article  Google Scholar 

  • Blanc E-P, Allen MB, Inger S, Hassani H (2003) Structural styles in the Zagros simple folded zone, Iran. J Geol Soc 160:401–412. doi:10.1144/0016-764902-110

    Article  Google Scholar 

  • Burberry CM (2015) The effect of basement fault reactivation on the Triassic—recent geology of Kurdistan, north Iraq. J Pet Geol 38:37–58

    Article  Google Scholar 

  • Carminati E et al (2013) Control of Cambrian evaporites on fracturing in fault-related anticlines in the Zagros fold-and-thrust belt. Int J Earth Sci 102:1237–1255

    Article  Google Scholar 

  • Casini G et al (2011) Sub-seismic fractures in foreland fold and thrust belts: insight from the Lurestan Province, Zagros Mountains, Iran. Pet Geosci 17:263–282. doi:10.1144/1354-079310-043

    Article  Google Scholar 

  • Chu HT, Lee J-C, Bergerat F, Hu J-C, Liang S-H, Lu C-Y, Lee T-Q (2013) Fracture patterns and their relations to mountain building in a fold–thrust belt: a case study in NW Taiwan. Bull Soc Géol Fr 184(4–5):485–500

    Article  Google Scholar 

  • Cooper SP, Goodwin LB, Lorenz JC (2006) Fracture and fault patterns associated with basement-cored anticlines: the example of Teapot Dome, Wyoming. AAPG Bull 90:1903–1920

    Article  Google Scholar 

  • Emami H (2008) Foreland propagation folding and structure of the Mountain Front Flexure in the Pusht-e Kuh arc (NW Zagros, Iran), PhD thesis. Universitat de Barcelona

  • Emami H et al (2010) Structure of the Mountain Front Flexure along the Anaran anticline in the Pusht-e Kuh Arc (NW Zagros, Iran): insights from sand box models. Geol Soc Lond Spec Publ 330:155–178

    Article  Google Scholar 

  • Falcon NL (1974) Southern Iran: Zagros Mountains. Geol Soc Lond Spec Publ 4:199–211

    Article  Google Scholar 

  • Farzipour-Saein A, Yassaghi A, Sherkati S, Koyi H (2009a) Mechanical stratigraphy and folding style of the Lurestan region in the Zagros fold–thrust belt, Iran. J Geol Soc 166:1101–1115

    Article  Google Scholar 

  • Farzipour-Saein A, Yassaghi A, Sherkati S, Koyi H (2009b) Basin evolution of the Lurestan region in the Zagros fold-and-thrust belt, Iran. J Pet Geol 32:5–19

    Article  Google Scholar 

  • Farzipour-Saein A, Nilfouroushan F, Koyi H (2013) 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 102:2117–2135

    Article  Google Scholar 

  • Friedman M (1969) Structural analysis of fractures in cores from Saticoy Field, Ventura County, California. AAPG Bull 53:367–389

    Google Scholar 

  • Gholipour AM (1998) Patterns and structural positions of productive fractures in the Asmari reservoirs, Southwest Iran. J Can Pet Technol 37:44–50

    Article  Google Scholar 

  • Hessami K, Koyi H, Talbot C (2001a) The significance of strike-slip faulting in the basement of the Zagros fold and thrust belt. J Pet Geol 24:5–28

    Article  Google Scholar 

  • Hessami K, Koyi HA, Talbot CJ, Tabasi H, Shabanian E (2001b) Progressive unconformities within an evolving foreland fold–thrust belt, Zagros Mountains. J Geol Soc 158:969–981

    Article  Google Scholar 

  • Homberg C, Hu J, Angelier J, Bergerat F, Lacombe O (1997) Characterization of stress perturbations near major fault zones: insights from 2-D distinct-element numerical modelling and field studies (Jura mountains). J Struct Geol 19:703–718

    Article  Google Scholar 

  • Homberg C, Angelier J, Bergerat F, Lacombe O (2004) Using stress deflections to identify slip events in fault systems. Earth Planet Sci Lett 217:409–424

    Article  Google Scholar 

  • Homke S, Vergés J, Garcés M, Emami H, Karpuz R (2004) Magnetostratigraphy of Miocene–Pliocene Zagros foreland deposits in the front of the Push-e Kush arc (Lurestan Province, Iran). Earth Planet Sci Lett 225:397–410

    Article  Google Scholar 

  • Jenness J (2014) Polar plots for ArcGIS Jenness Enterprises. http://www.jennessent.com/arcgis/polar_plotshtm

  • Khoshbakht F, Memarian H, Mohammadnia M (2009) Comparison of Asmari, Pabdeh and Gurpi formation’s fractures, derived from image log. J Pet Sci Eng 67:65–74

    Article  Google Scholar 

  • Khoshbakht F, Azizzadeh M, Memarian H, Nourozi G, Moallemi S (2012) Comparison of electrical image log with core in a fractured carbonate reservoir. J Pet Sci Eng 86:289–296

    Article  Google Scholar 

  • Koyi H (1988) Experimental modeling of role of gravity and lateral shortening in Zagros mountain belt. AAPG Bull 72:1381–1394

    Google Scholar 

  • Lacombe O, Bellahsen N, Mouthereau F (2011) Fracture patterns in the Zagros Simply Folded Belt (Fars, Iran): constraints on early collisional tectonic history and role of basement faults. Geol Mag 148:940–963

    Article  Google Scholar 

  • Mandl G (1988) Mechanics of tectonic faulting: models and basic concepts, vol 407. Elsevier, Amsterdam

    Google Scholar 

  • McClay K (1987) The mapping of geological structures. Geological Society of London Handbook Series. Open University Press, London

  • McQuarrie N (2004) Crustal scale geometry of the Zagros fold–thrust belt, Iran. J Struct Geol 26:519–535

    Article  Google Scholar 

  • McQuarrie N, van Hinsbergen DJ (2013) Retrodeforming the Arabia-Eurasia collision zone: age of collision versus magnitude of continental subduction. Geology 41:315–318. doi:10.1130/G33591.1

    Article  Google Scholar 

  • McQuillan H (1973) Small-scale fracture density in Asmari Formation of southwest Iran and its relation to bed thickness and structural setting. AAPG Bull 57:2367–2385

    Google Scholar 

  • McQuillan H (1974) Fracture patterns on Kuh-e Asmari anticline, southwest Iran. AAPG Bull 58:236–246

    Google Scholar 

  • Misra AA, Bhattacharya G, Mukherjee S, Bose N (2014) Near N-S paleo-extension in the western Deccan region, India: does it link strike-slip tectonics with India–Seychelles rifting? Int J Earth Sci 103:1645–1680

    Article  Google Scholar 

  • Misra AA, Sinha N, Mukherjee S (2015) Repeat ridge jumps and microcontinent separation: insights from NE Arabian Sea. Mar Pet Geol 59:406–428

    Article  Google Scholar 

  • Mobasher K, Babaie HA (2008) Kinematic significance of fold-and fault-related fracture systems in the Zagros mountains, southern Iran. Tectonophysics 451:156–169

    Article  Google Scholar 

  • Motiei H (1994) Stratigraphy of Zagros. Geological Survey of Iran Publications, Tehran (in Persion)

    Google Scholar 

  • Mouthereau F, Lacombe O, Tensi J, Bellahsen N, Kargar S, Amrouch K (2007a) Mechanical constraints on the development of the Zagros Folded Belt (Fars). In: Thrust belts and foreland basins. Springer, Berlin, pp 247–266

  • Mouthereau F, Tensi J, Bellahsen N, Lacombe O, De Boisgrollier T, Kargar S (2007b) Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: the Zagros Folded Belt (Fars, Iran). Tectonics 26(TC5006):28. doi:10.1029/2007TC002098

    Google Scholar 

  • Mouthereau F, Lacombe O, Vergés J (2012) Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics 532:27–60

    Article  Google Scholar 

  • Mukherjee S (2013a) Deformation microstructures in rocks. Springer, Berlin

    Book  Google Scholar 

  • Mukherjee S (2013b) Higher Himalaya in the Bhagirathi section (NW Himalaya, India): its structures, backthrusts and extrusion mechanism by both channel flow and critical taper mechanisms. Int J Earth Sci 102:1851–1870

    Article  Google Scholar 

  • Mukherjee S (2014) Atlas of shear zone structures in meso-scale. Springer, Berlin

    Book  Google Scholar 

  • Mukherjee S, Koyi HA (2010) Higher Himalayan Shear Zone, Sutlej section: structural geology and extrusion mechanism by various combinations of simple shear, pure shear and channel flow in shifting modes. Int J Earth Sci 99:1267–1303

    Article  Google Scholar 

  • Nemcok M, Schamel S, Gayer R (2009) Thrustbelts: structural architecture, thermal regimes and petroleum systems. Cambridge University Press, Cambridge

    Google Scholar 

  • Nilforoushan F et al (2003) GPS network monitors the Arabia-Eurasia collision deformation in Iran. J Geodesy 77:411–422

    Article  Google Scholar 

  • Nilfouroushan F, Pysklywec R, Cruden A, Koyi H (2013) Thermal-mechanical modeling of salt-based mountain belts with pre-existing basement faults: application to the Zagros fold and thrust belt, southwest Iran. Tectonics 32:1212–1226

    Article  Google Scholar 

  • Player RA, Hulstrand RF, Ghashghaie M (1966) The central Lurestan geological survey 1963–1964 IOOC Report, No. 1103 (Unpublished)

  • Pollard DD, Aydin A (1988) Progress in understanding jointing over the past century. Geol Soc Am Bull 100:1181–1204

    Article  Google Scholar 

  • Price NJ (1966) Fault and joint development in brittle and semi-brittle rock, vol 1. Pergamon Press, Oxford

    Google Scholar 

  • Ramsey LA, Walker RT, Jackson J (2008) Fold evolution and drainage development in the Zagros mountains of Fars province, SE Iran. Basin Res 20:23–48

    Article  Google Scholar 

  • Sepehr M, Cosgrove J (2004) Structural framework of the Zagros fold–thrust belt, Iran. Mar Pet Geol 21:829–843

    Article  Google Scholar 

  • Sepehr M, Cosgrove J (2005) Role of the Kazerun Fault Zone in the formation and deformation of the Zagros Fold–Thrust Belt, Iran. Tectonics 24(TC5005):13. doi:10.1029/2004TC001725

    Google Scholar 

  • Sharp I et al (2010) Stratigraphic architecture and fracture-controlled dolomitization of the Cretaceous Khami and Bangestan groups: an outcrop case study, Zagros Mountains, Iran. Geol Soc Lond Spec Publ 329:343–396

    Article  Google Scholar 

  • Sherkati S, Letouzey J (2004) Variation of structural style and basin evolution in the central Zagros (Izeh zone and Dezful Embayment), Iran. Mar Pet Geol 21:535–554

    Article  Google Scholar 

  • Snidero M, Amilibia A, Gratacos O, Blanc E-P, Muñoz J (2011) The 3D reconstruction of geological structures based on remote sensing data: example from the Anaran anticline, Lurestan province, Zagros fold and thrust belt, Iran. J Geol Soc 168:769–782. doi:10.1144/0016-76492010-107

    Article  Google Scholar 

  • Stearns DW, Friedman M (1972) Reservoirs in fractured rock: geologic exploration methods: the American Association of Petroleum Geologists reprinted from American Association of Petroleum Geologists Memoir Stratigraphic Oil and Gas Fields 16:82–106

  • Stephenson BJ, Koopman A, Hillgartner H, McQuillan H, Bourne S, Noad JJ, Rawnsley K (2007) Structural and stratigraphic controls on fold-related fracturing in the Zagros Mountains, Iran: implications for reservoir development. Geol Soc Lond Spec Publ 270:1–21

    Article  Google Scholar 

  • Stocklin J (1968) Structural history and tectonics of Iran: a review. AAPG Bull 52:1229–1258

    Google Scholar 

  • Stöcklin J (1974) Possible ancient continental margins in Iran. In: The geology of continental margins. Springer, Berlin, pp 873–887

  • Storti F, Salvini F (2001) The evolution of a model trap in the central Apennines, Italy: fracture patterns, fault reactivation and development of cataclastic rocks in carbonates at the Narni Anticline. J Pet Geol 24:171–190

    Article  Google Scholar 

  • Takin M (1972) Iranian geology and continental drift in the Middle East. Nature 235:147–150

    Article  Google Scholar 

  • Talbot C, Alavi M (1996) The past of a future syntaxis across the Zagros. Geol Soc Lond Spec Publ 100:89–109. doi:10.1144/GSL.SP.1996.100.01.08.1

    Article  Google Scholar 

  • Tavani S, Storti F, Fernández O, Muñoz J, Salvini F (2006) 3-D deformation pattern analysis and evolution of the Añisclo anticline, southern Pyrenees. J Struct Geol 28:695–712

    Article  Google Scholar 

  • Tavani S, Storti F, Soleimany B, Fallah M, Munoz JA, Gambini R (2011) Geometry, kinematics and fracture pattern of the Bangestan anticline, Zagros, SW Iran. Geol Mag 148:964–979

    Article  Google Scholar 

  • Tavani S, Snidero M, Muñoz J (2014) Uplift-induced residual strain release and late-thrusting extension in the Anaran mountain front anticline, Zagros (Iran). Tectonophysics 636:257–269

    Article  Google Scholar 

  • Tavani S, Storti F, Lacombe O, Corradetti A, Muñoz J, Mazzoli S (2015) A review of deformation pattern templates in foreland basin systems and fold-and-thrust belts: implications for the state of stress in the frontal regions of thrust wedges. Earth Sci Rev 141:82–104

    Article  Google Scholar 

  • Twiss RJ, Moores E (1992) Structural geology. WH Freeman, New York

    Google Scholar 

  • Vergés J, Goodarzi M, Emami H, Karpuz R, Efstathiou J, Gillespie P (2011) Multiple detachment folding in Pusht-e Kuh arc, Zagros: role of mechanical stratigraphy. AAPG Memoir 94:69–94

    Google Scholar 

  • Wennberg O, Svånå T, Azizzadeh M, Aqrawi A, Brockbank P, Lyslo K, Ogilvie S (2006) Fracture intensity vs. mechanical stratigraphy in platform top carbonates: the Aquitanian of the Asmari Formation, Khaviz Anticline, Zagros, SW Iran. Pet Geosci 12:235–246

    Article  Google Scholar 

  • Wibberley CAJ, Kurz W, Imber J, Holdsworth RE, Collettini C (2008) The internal structure of fault zones: implications for mechanical and fluid-flow properties. Geol Soc Lond Spec Publ 299:195–210

    Article  Google Scholar 

  • Zarifi Z, Nilfouroushan F, Raeesi M (2014) Crustal stress Map of Iran: insight from seismic and geodetic computations. Pure appl Geophys 170:1–18. doi:10.1007/s00024-013-0711-9

    Google Scholar 

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Acknowledgments

The authors are very grateful to Stefano Tavani and Soumyajit Mukherjee for careful and constructive reviews, which helped us to greatly improve this manuscript. We also acknowledge Wolf-Christian Dullo and Soumyajit Mukherjee for handling our manuscript and Katayoun Mobasher who introduced us some relevant articles. Moosarreza Toori is thanked for his help with the structural transect. AFS thanks the research and postgraduate office in University of Isfahan for their support. FN was funded by Swedish Research Council (VR).

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  1. Department of Geology, University of Isfahan, P.O. Code: 81746-73441, Isfahan, Iran

    M. Joudaki & A. Farzipour-Saein

  2. Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36, Uppsala, Sweden

    F. Nilfouroushan

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Joudaki, M., Farzipour-Saein, A. & Nilfouroushan, F. Kinematics and surface fracture pattern of the Anaran basement fault zone in NW of the Zagros fold–thrust belt. Int J Earth Sci (Geol Rundsch) 105, 869–883 (2016). https://doi.org/10.1007/s00531-015-1209-8

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