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Fracture patterns in the Zagros Simply Folded Belt (Fars, Iran): constraints on early collisional tectonic history and role of basement faults

Published online by Cambridge University Press:  14 April 2011

OLIVIER LACOMBE*
Affiliation:
UPMC Univ Paris 06, UMR 7193, ISTEP, F-75005, Paris, France CNRS, UMR 7193, ISTEP, F-75005, Paris, France
NICOLAS BELLAHSEN
Affiliation:
UPMC Univ Paris 06, UMR 7193, ISTEP, F-75005, Paris, France CNRS, UMR 7193, ISTEP, F-75005, Paris, France
FRÉDÉRIC MOUTHEREAU
Affiliation:
UPMC Univ Paris 06, UMR 7193, ISTEP, F-75005, Paris, France CNRS, UMR 7193, ISTEP, F-75005, Paris, France
*
Author for correspondence: [email protected]

Abstract

Pre-/early folding fracture patterns were recognized in several anticlines from three structural domains in the Simply Folded Belt of the Fars arc. These fracture sets were characterized in terms of opening mode and relative chronology and used to reconstruct the main compressional trends related to the early Zagros collisional history. The palaeostress reconstructions based on these fracture sets were further refined by combination with newly collected or already available fault-slip and calcite twin data. As an alternative to previous models of rigid block rotations or regional stress rotation, we propose that the complex pattern of pre-folding fractures and the contrasting palaeostress orientations through time in the different domains investigated are related to the presence of basement faults with N–S and WNW trends, above which basement and cover were variably coupled during stress build-up and early deformation of the Arabian margin. Beyond regional implications, this study draws attention to the need to carefully consider pre-existing fractures, possibly unrelated to folding, to build more realistic conceptual fold–fracture models.

Type
THE ZAGROS FOLD-THRUST BELT: FOLDS AND FRACTURES
Copyright
Copyright © Cambridge University Press 2011

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References

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, 401–19.CrossRefGoogle Scholar
Ahmadhadi, F., Daniel, J. M., 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 27, TC1016, doi:10.1029/2006TC001978, 22 pp.CrossRefGoogle 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 the Asmari Formation and Lower Tertiary paleogeography. In Thrust Belts and Foreland Basins; From fold kinematics to hydrocarbon systems, Frontiers in Earth Sciences (eds Lacombe, O., Lavé, J., Vergès, J. & Roure, F.), pp. 205–28. Springer-Verlag.CrossRefGoogle Scholar
Allen, M. B. & Armstrong, H. A. 2008. Arabia-Eurasia collision and the forcing of mid Cenozoic global cooling. Palaeogeography, Palaeoclimatology, Palaeoecology 265, 52–8.CrossRefGoogle Scholar
Allen, M., Jackson, J. & Walker, R. 2004. Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates. Tectonics 23, TC2008, doi:10.1029/2003TC001530, 16 pp.Google Scholar
Amrouch, K., Lacombe, O., Bellahsen, N., Daniel, J.-M. & Callot, J. P. 2010 a. Stress/strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain anticline (Wyoming, USA). Tectonics 29, TC1005, doi:10.1029/2009TC002525, 27 pp.CrossRefGoogle Scholar
Amrouch, K., Robion, P., Callot, J.-P., Lacombe, O., Daniel, J.-M., Bellahsen, N. & Faure, J.-L. 2010 b. Constraints on deformation mechanisms during folding provided by rock physical properties: a case study at Sheep Mountain anticline (Wyoming, USA). Geophysical Journal International 182, 1105–23.CrossRefGoogle Scholar
Anastasio, D. J., Fisher, D. M., Messina, T. A. & Holl, J. E. 1997. Kinematics of decollement folding in the Lost River Range, Idaho. Journal of Structural Geology 19, 355–68.CrossRefGoogle Scholar
Angelier, J. 1990. Inversion of field data in fault tectonics to obtain the regional stress III – a new rapid direct inversion method by analytical means. Geophysical Journal International 103, 363–76.CrossRefGoogle Scholar
Aubourg, C., Smith, B., Bakhtari, H., Guya, N. & Eshraghi, A. R. 2008. Tertiary block rotations in the Fars Arc (Zagros, Iran). Geophysical Journal International 173, 659–73.CrossRefGoogle Scholar
Aubourg, C., Smith, B., Eshrahi, A., Lacombe, O., Authemayou, C., Amrouch, K., Bellier, O. & Mouthereau, F. 2010. New magnetic fabric data and their comparison with stress/strain markers from the Western Fars arc (Zagros); tectonic implications. In Tectonic and Stratigraphic Evolution of Zagros and Makran During the Meso-Cenozoic (eds Leturmy, P. & Robin, C.), pp. 97120. Geological Society of London, Special Publication no. 330.Google Scholar
Authemayou, C., Chardon, D., Bellier, O., Malekzadeh, Z., Shabanian, E. & Abbassi, M. R. 2006. Late Cenozoic partitioning of oblique plate convergence in the Zagros fold-and-thrust belt (Iran). Tectonics 25, TC3002, doi:10.1029/2005TC001860, 21 pp.CrossRefGoogle Scholar
Bachmanov, D. M., Trifonov, V. G., Hessami, K. T., Kozhurin, A. I., Ivanova, T. P., Rogozhin, E. A., Hademi, M. C. & Jamali, F. H. 2004. Active faults in the Zagros and central Iran. Tectonophysics 380, 221–41.CrossRefGoogle Scholar
Bakhtari, H., Frizon De Lamotte, D., Aubourg, C. & Hassanzadeh, J. 1998. Magnetic fabric of Tertiary sandstones from the Arc of Fars (Eastern Zagros, Iran). Tectonophysics 284, 299316.CrossRefGoogle 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. Geophysical Journal International 115, 4161.CrossRefGoogle Scholar
Bellahsen, N., Fiore, P. & Pollard, D. D. 2006. The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming. Journal of Structural Geology 28, 850–67.CrossRefGoogle Scholar
Berberian, M. 1995. Master ‘blind’ thrust faults hidden under the Zagros folds; active basement tectonics and surface morphotectonics. Tectonophysics 241, 193224.CrossRefGoogle Scholar
Berberian, M. & King, G. C. P. 1981. Towards a paleogeography and tectonic evolution of Iran. Canadian Journal of Earth Sciences 18, 210–65.CrossRefGoogle Scholar
Bergbauer, S. & Pollard, D. D. 2004. A new conceptual fold-fracture model including prefolding joints, based on the Emigrant Gap Anticline, Wyoming. Geological Society of America Bulletin 116, 294307.CrossRefGoogle Scholar
Beydoun, Z. R., Clarke, M. W. H. & Stoneley, R. 1992. Petroleum in the Zagros Basin: a late Tertiary foreland basin overprinted onto the outer edge of a vast hydrocarbon-rich Paleozoic-Mesozoic passive-margin shelf. In Foreland Basins and Fold Belts (eds Macqueen, R. W. & Leckie, D. A.), pp. 309–39. American Association of Petroleum Geologists Memoir no. 55.Google Scholar
Colman-Sadd, S. 1978. Fold development in Zagros simply folded belt, Southwest Iran. American Association of Petroleum Geologists Bulletin 62, 9841003.Google Scholar
Couzens, B. A. & Dunne, W. M. 1994. Displacement transfer at thrust terminations: The Saltville Thrust and Sinking Creek Anticline, Virginia, U.S.A. Journal of Structural Geology 16, 781–93.CrossRefGoogle Scholar
Demets, C., Gordon, R. G., Argus, D. F. & Stein, S. 1990. Current plate motions. Geophysical Journal International 101, 425–78.CrossRefGoogle Scholar
Engelder, T. 1987. Joints and shear fractures in rock. In Fracture Mechanics of Rocks (ed. Atkinson, B. K.), pp. 2769. London: Academic Press.CrossRefGoogle Scholar
Erslev, E. A. & Mayborn, K. R. 1997. Multiple geometries and modes of fault-propagation folding in the Canadian thrust belt. Journal of Structural Geology 19, 321–35.CrossRefGoogle Scholar
Fakhari, M. D., Axen, G. J., Horton, B. K., Hassanzadeh, J. & Amini, A. 2008. Revised age of proximal deposits in the Zagros Foreland Basin and implications for Cenozoic evolution of the High Zagros. Tectonophysics 451, 170–85.CrossRefGoogle Scholar
Falcon, N. L. 1974. Southern Iran: Zagros Mountains. In Mesozoic–Cenozoic Orogenic Belts: Data for orogenic studies (ed. Spencer, A.), pp. 199211. Geological Society of London, Special Publication no. 4.Google Scholar
Fischer, M. P., Woodward, N. B. & Mitchell, M. M. 1992. The kinematics of break-thrust folds. Journal of Structural Geology 14, 451–60.CrossRefGoogle Scholar
Gholipour, A. M. 1998. Patterns and structural positions of productive fractures in the Asmari reservoirs, Southwest Iran. Journal of Canadian Petroleum Technology 37, 4450.CrossRefGoogle Scholar
Hancock, P. L. 1985. Brittle microtectonics; principles and practice. Journal of Structural Geology 7, 437–57.CrossRefGoogle Scholar
Hennings, P. H. 2000. Combining outcrop data and three-dimensional structural models to characterize fractured reservoirs: an example from Wyoming. American Association of Petroleum Geologists Bulletin 84, 830–49.Google Scholar
Hessami, K., Koyi, H. A., Talbot, C. J., Tabasi, H. & Shabanian, E. 2001. Progressive unconformities within an evolving foreland fold-thrust belt, Zagros Mountains. Journal of the Geological Society, London 158, 969–81.CrossRefGoogle Scholar
Homke, S., Verges, J., Garces, 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 and Planetary Science Letters 225, 397410.CrossRefGoogle Scholar
Jackson, J. A. 1980. Reactivation of basement faults and crustal shortening in orogenic belts. Nature 283, 343–6.CrossRefGoogle Scholar
Jackson, J. & McKenzie, D. 1984. Active tectonics of the Alpine-Himalayan belt between western Turkey and Pakistan. Geophysical Journal of the Royal Astronomical Society 64, 561–86.CrossRefGoogle Scholar
Khadivi, S., Mouthereau, F., Larasoana, J.-C., Verges, J., Lacombe, O., Khademi, E., Beamud, E., Melinte-Dobrinescu, M. & Suc, J. P. 2010. Magnetochronology of synorogenic Miocene foreland sediments in the Fars arc of the Zagros Folded Belt (SE Iran). Basin Research 22, 918–32.CrossRefGoogle Scholar
Kittler, J. 1976. A locally sensitive method for cluster analysis. Pattern Recognition 8, 2333.CrossRefGoogle Scholar
Lacombe, O. 2001. Paleostress magnitudes associated with development of mountain belts: insights from tectonic analyses of calcite twins in the Taiwan Foothills. Tectonics 20, 834–49.CrossRefGoogle Scholar
Lacombe, O., Amrouch, K., Mouthereau, F. & Dissez, L. 2007. Calcite twinning constraints on late Neogene stress patterns and deformation mechanisms in the active Zagros collision belt. Geology 35, 263–6.CrossRefGoogle Scholar
Lacombe, O., Angelier, J., Rocher, M., Bergues, J., Chu, H.-T., Deffontaines, B. & Hu, J.-C. 1996. Contraintes et plissement au front d'une chaîne de collision: l'exemple des calcaires récifaux pliocènes de Yutengping (Taiwan). Bulletin de la Société Géologique de France 167, 361–74.Google Scholar
Lacombe, O. & Mouthereau, F. 2002. Basement-involved shortening and deep detachment tectonics in forelands of orogens: insights from recent collision belts (Taiwan, western Alps, Pyrenees). Tectonics 21, 1030, doi:10.1029/2001TC901018, 22 pp.CrossRefGoogle Scholar
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, doi:10.1029/2005TC001831.CrossRefGoogle Scholar
Lisle, R. J. 2000. Predicting patterns of strain from three-dimensional fold geometries: neutral surface folds and forced folds. In Forced Folds and Fractures (eds Cosgrove, J. W. & Ameen, M. S.), pp. 213–21.Geological Society of London, Special Publication no. 169.Google Scholar
Marcotte, D. & Henry, E. 2002. Automatic joint set clustering using a mixture of bivariate normal distributions. International Journal of Rock Mechanics and Mineral Sciences 39, 323–34.CrossRefGoogle Scholar
McQuarrie, N. 2004. Crustal scale geometry of the Zagros fold-thrust belt, Iran. Journal of Structural Geology 26, 519–35.CrossRefGoogle Scholar
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, 4 pp.CrossRefGoogle Scholar
McQuillan, H. 1973. Small-scale fracture density in Asmari Formation of Southwest Iran and its relation to bed thickness and structural setting. American Association of Petroleum Geologists Bulletin 57, 2367–85.Google Scholar
McQuillan, H. 1974. Fracture patterns on Kuh-e Asmari Anticline, Southwest Iran. American Association of Petroleum Geologists Bulletin 58, 236–46.Google Scholar
Mobasher, K. & Babaie, H. 2008. Kinematic significance of fold- and fault-related fracture systems in the Zagros mountains, southern Iran. Tectonophysics 451, 156–69.CrossRefGoogle Scholar
Molinaro, M., Leturmy, P., Guezou, J.-C., Frizon De Lamotte, D. & Eshraghi, S. A. 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, 19 pp.CrossRefGoogle Scholar
Mouthereau, F., Lacombe, O. & Meyer, B. 2006. The Zagros folded belt (Fars, Iran): constraints from topography and critical wedge modelling. Geophysical Journal International 165, 336–56.CrossRefGoogle Scholar
Mouthereau, F., Lacombe, O., Tensi, J., Bellahsen, N., Kargar, S. & Amrouch, K. 2007 a. Mechanical constraints on the development of the Zagros Folded Belt. In Thrust Belts and Foreland Basins; From fold kinematics to hydrocarbon systems, Frontiers in Earth Sciences (eds Lacombe, O., Lavé, J., Vergès, J. & Roure, F.), pp. 247–66. Springer-Verlag.CrossRefGoogle Scholar
Mouthereau, F., Tensi, J., Bellahsen, N., Lacombe, O., De Boisgrollier, T. & Kargar, S. 2007 b. Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: the Zagros Folded Belt (Fars, Iran). Tectonics 26, TC5006, doi:10.1029/2007TC002098, 28 pp.CrossRefGoogle Scholar
Oveisi, B., Lave, J., Van Der Beek, P., Carcaillet, J., Benedetti, L. & Aubourg, C. 2009. Thick- and thin-skinned deformation rates in the Central Zagros Simple Folded Zone (Iran) indicated by displacement of geomorphic surfaces. Geophysical Journal International 176, 627–54.CrossRefGoogle Scholar
Price, N. J. 1966. Fault and Joint Development in Brittle and Semi-Brittle Rocks. London: Pergamon Press, 176 pp.Google Scholar
Regard, V., Bellier, O., Thomas, J.-C., Abbassi, 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 deforming system. Tectonics 23, TC4007, doi:10.1029/2003TC001599, 24 pp.CrossRefGoogle Scholar
Roustaei, M., Nissen, E., Abbassi, M., Gholamzadeh, A., Ghorashi, M., Tatar, M., Yamini-Fard, F., Bergman, E., Jackson, J. & Parsons, B. 2010. The 2006 March 25 Fin earthquakes (Iran) – insights into the vertical extents of faulting in the Zagros Simply Folded Belt. Geophysical Journal International 181, 1275–91.Google Scholar
Sanderson, D. J. 1982. Models of strain variation in nappes and thrust sheets: a review. Tectonophysics 88, 201–33.CrossRefGoogle Scholar
Sattarzadeh, Y., Cosgrove, J. W. & Vita-Finzi, C. 2000. The interplay of faulting and folding during the evolution of the Zagros deformation belt. In Forced Folds and Fractures (eds Cosgrove, J. W. & Ameen, M. S.), pp. 187–96. Geological Society of London, Special Publication no. 169.Google Scholar
Sepehr, M. & Cosgrove, J. W. 2005. The 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, 13 pp.CrossRefGoogle Scholar
Sherkati, S., Letouzey, J. & Frizon De Lamotte, D. 2006. The Central Zagros fold-thrust belt (Iran): new insights from seismic data, field observations and sandbox modelling. Tectonics 25, TC4007, doi:10.1029/2004TC001766, 27 pp.CrossRefGoogle Scholar
Srivastava, D. C. & Engelder, T. 1990. Crack-propagation sequence and pore-fluid conditions during fault-bend folding in the Appalachian Valley and Ridge, central Pennsylvania. Geological Society of America Bulletin 102, 116–28.2.3.CO;2>CrossRefGoogle Scholar
Stearns, D. W. & Friedman, M. 1972. Reservoirs in fractured rocks. American Association of Petroleum Geologists Memoir 16, 82100.Google Scholar
Stephenson, B. J., Koopman, A., Hillgartner, H., McQuillan, H., Bourne, S., Noad, J. J. & Rawnsley, K. 2007. Structural and stratigraphic controls on fold-related fracturing in the Zagros Mountains, Iran: implications for reservoir development. In Fractured Reservoirs (eds Lonergan, L., Jolly, R. J. H., Rawnsley, K. & Sanderson, D. J.), pp.121. Geological Society of London, Special Publication no. 270.Google Scholar
Stocklin, J. 1968. Structural history and tectonics of Iran; a review. American Association of Petroleum Geologists Bulletin 52, 1229–58.Google Scholar
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. Journal of Petroleum Geology 24, 171–90.CrossRefGoogle Scholar
Talebian, M. & Jackson, J. A. 2004. A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran. Geophysical Journal International 156, 506–26.CrossRefGoogle Scholar
Tatar, M., Hatzfeld, D. & Ghafori-Ashtiany, M. 2004. Tectonics of the central Zagros (Iran) deduced from microearthquakes seismicity. Geophysical Journal International 156, 255–66.CrossRefGoogle Scholar
Tavani, S., Storti, F., Fernandez, O., Munoz, J. A. & Salvini, F. 2006. 3-D deformation pattern analysis and evolution of the Anisclo anticline, southern Pyrenees. Journal of Structural Geology 28, 695712.CrossRefGoogle Scholar
Thorbjornsen, K. L. & Dunne, W. M. 1997. Origin of a thrust-related fold; geometric vs kinematic tests. Journal of Structural Geology 19, 303–19.CrossRefGoogle Scholar
Vernant, P., Nilforoushan, F., Hatzfeld, D., Abbassi, M. R., 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. Geophysical Journal International 157, 381–98.CrossRefGoogle Scholar
Wennberg, O. P., Svånå, T., Azizzadeh, M., Aqrawi, A. M. M., Brockbank, P., Lyslo, K. B. & Ogilvie, S. 2007. Fracture intensity vs. mechanical stratigraphy in platform top carbonates: the Aquitanian of the Asmari Formation, Khaviz Anticline, Zagros, SW Iran. Petroleum Geoscience 12, 235–45.CrossRefGoogle Scholar
Wollmer, F. W. 1995. C Program for automatic contouring of spherical orientation data using a modified Kamb method. Computers and Geosciences 21, 2149.Google Scholar