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Reconstruction of ancestral drainage patterns in an internally draining region, Fars Province, Iran

Published online by Cambridge University Press:  17 February 2015

JACQUELINE LEE*
Affiliation:
Vero Beach, Florida, United States
*

Abstract

Google Earth imagery is used here in conjunction with a Geographic Information System to identify transverse drainages and recreate palaeodrainage in an internally draining region in Iran. At least 35 water gaps and 34 wind gaps are shown to exist in the region, as well as evidence for an integrated palaeodrainage that originated north of the internally draining region and emptied into the Mand watershed to the west. The topographic characteristics of the transverse drainages suggest a strong control by local topography, and support formation of the internally draining region by basin filling and overflow. Both climatic and tectonic factors may have controlled the loss of external connectivity.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 2015 

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References

AbuBakr, M., Ghoneim, E., El-Baz, F., Zeneldin, M. & Zeid, S. 2013. Use of radar data to unveil the paleolakes and the ancestral course of Wadi El-Arish, Sinai Peninsula, Egypt. Geomorphology 194, 3445.Google Scholar
Allen, M., Saville, C., Blanc, E., Talebian, M. & Nissen, E. 2013. Orogenic plateau growth: Expansion of the Turkish-Iranian Plateau across the Zagros fold-and-thrust belt. Tectonics 32, 171–90.CrossRefGoogle Scholar
Berberian, M. & King, G. 1981. Towards a paleogeography and tectonic evolution of Iran. Canadian Journal of Earth Sciences 18 (2), 210–65.Google Scholar
Beydoun, Z., Clarke, M. H. & Stoneley, R. 1992. Petroleum in the Zagros Basin: A late Tertiary foreland basin overprinted on the outer edge of a vast hydrocarbon-rich Paleozoic-Mesozoic passive margin shelf. In Foreland Basins and Fold Belts (eds Macqueen, R. & Leckie, D. A.), pp. 309–39. American Association of Petroleum Geologists, Memoir 55.Google Scholar
Bishop, P. 1995. Drainage rearrangement by river capture, beheading and diversion. Progress in Physical Geography 19 (4), 449–73.Google Scholar
Blanc, E. P., Allen, M. B., Inger, S. & Hassani, H. 2003. Structural styles in the Zagros simple folded zone, Iran. Journal of the Geological Society 160 (3), 401–12.Google Scholar
Bourne, J. A. & Twidale, C. R. 2011. Neglected and cryptostructural effects in drainage development. Cadernos do Laboratorio Xeolóxico de Laxe 36, 4157.Google Scholar
Bretis, B., Bartl, N. & Grasemann, B. 2011. Lateral fold growth and linkage in the Zagros fold and thrust belt (Kurdistan, NE Iraq). Basin Research 23 (6), 615–30.Google Scholar
Burbank, D. W. & Anderson, R. S. 2001. Holocene deformation and landscape responses. In Tectonic Geomorphology (eds Burbank, D. W. & Anderson, R. S.), pp. 159–74. Malden, MA: John Wiley & Sons.Google Scholar
Burbank, D., Meigs, A. & Brozovi’c, N. 1996. Interactions of growing folds and coeval depositional systems. Basin Research 8 (3), 199223.CrossRefGoogle Scholar
Burberry, C. M., Cosgrove, J. W. & Liu, J. G. 2007. Stream network characteristics used to infer the distribution of fold types in the Zagros Simply Folded Belt, Iran. Journal of Maps 3 (supplement 1), 3245.Google Scholar
Burberry, C. M., Cosgrove, J. W. & Liu, J. G. 2008. Spatial arrangement of fold types in the Zagros Simply Folded Belt, Iran, indicated by landform morphology and drainage pattern characteristics. Journal of Maps 4 (1), 417–30.Google Scholar
Burrato, P., Ciucci, F. & Valensise, G. 2003. An inventory of river anomalies in the Po Plain, Northern Italy: evidence for active blind thrust faulting. Annals of Geophysics 46 (5), 865–82.Google Scholar
Burrato, P., Vannoli, P., Fracassi, U., Basili, R. & Valensise, G. 2012. Is blind faulting truly invisible? Tectonic-controlled drainage evolution in the epicentral area of the May 2012, Emilia-Romagna earthquake sequence (northern Italy). Annals of Geophysics 55 (4), 525–31.Google Scholar
Carroll, A., Graham, S. & Smith, M. 2010. Walled sedimentary basins of China. Basin Research 22 (1), 1732.Google Scholar
Casciello, E., Vergés, J., Saura, E., Casini, G., Fernández, N., Blanc, E., Homke, S. & Hunt, D. 2009. Fold patterns and multilayer rheology of the Lurestan Province, Zagros Simply Folded Belt (Iran). Journal of the Geological Society 166 (5), 947–59.Google Scholar
Clark, G. M. 1989. Central and southern Appalachian water and wind gap origins: review and new data. Geomorphology 2 (1–3), 209–32.CrossRefGoogle Scholar
DeVogel, S. B., Magee, J. W., Manley, W. F. & Miller, G. H. 2004. A GIS-based reconstruction of late Quaternary paleohydrology: Lake Eyre, arid central Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 204 (1), 113.Google Scholar
Dordevic, M. M. 2012. Designing interactive screen overlays to enhance effectiveness of Google Earth geosciences resources. In Google Earth and Virtual Visualizations in Geoscience and Research (eds Whitmeyer, S. J., Bailey, J. B., De Paor, D. G. & Ornduff, T.), pp. 105–11. Geological Society of America, Special Paper 492.Google Scholar
Douglass, J., Meek, N., Dorn, R. I. & Schmeeckle, M. W. 2009. A criteria-based methodology for determining the mechanism of transverse drainage development, with application to the southwestern United States. Geological Society of America Bulletin 121 (3–4), 586–98.CrossRefGoogle Scholar
Douglass, J. & Schmeeckle, M. 2007. Analogue modeling of transverse drainage mechanisms. Geomorphology 84 (1–2), 2243.Google Scholar
Emami, H. 2008. Foreland propagation of folding and structure of the Mountain Front Flexure in the Pusht-e Kuh arc (NW Zagros, Iran). Ph.D. thesis, University of Barcelona. Published thesis.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. International Journal of Earth Sciences 102 (8), 2117–35.Google Scholar
Fattahi, M., Walker, R., Talebian, M., Sloan, R. & Rasheedi, A. 2014. Late Quaternary active faulting and landscape evolution in relation to the Gowk Fault in the South Golbaf Basin, SE Iran. Geomorphology 204, 334–43.CrossRefGoogle Scholar
Fisher, G. B., Amos, C. B., Bookhagen, B., Burbank, D. W. & Godard, V. 2012. Introduction: the application of Google Geo Tools to geosciences education. In Google Earth and Virtual Visualizations in Geoscience Education and Research (eds Whitmeyer, S. J., Bailey, J. B., De Paor, D. G. & Ornduff, T.), pp. viixix. Geological Society of America, Special Paper 492.Google Scholar
Fleeger, G. M. 1997. A tale of two valleys. Pennsylvania Geology 28 (1–2), 913.Google Scholar
Fossen, H. 2010. Structural Geology. Cambridge: Cambridge University Press, 463 pp.Google Scholar
Harper, J. A. 1997. Of ice and waters flowing: the formation of Pittsburgh's three rivers. Pennsylvania Geology 28 (3–4), 29.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 and Planetary Science Letters 225 (3), 397410.Google Scholar
Horton, R. E. 1945. Erosional development of streams and their drainage basins; hydrophysical approach to quantitative morphology. Geological Society of America Bulletin 56 (3), 275370.Google Scholar
Howard, A. D., Dietrich, W. E. & Seidl, M. A. 1994. Modeling fluvial erosion on regional to continental scales. Journal of Geophysical Research: Solid Earth 99 (B7), 13971–86.Google Scholar
Jahani, S., Callot, J.-P., Letouzey, J. & Frizon de Lamotte, D. 2009. The eastern termination of the Zagros Fold-and-Thrust Belt, Iran: structures, evolution, and relationships between salt plugs, folding, and faulting. Tectonics 28 (6), TC6004, published online 1 December 2009. doi: 10.1029/2008TC002418.Google Scholar
Kehl, M. 2009. Quaternary climate change in Iran–the state of knowledge. Erdkunde 63 (1), 117.Google Scholar
Khadivi, S., Mouthereau, F., Larrasoaña, J.-C., Vergés, 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 (SW Iran). Basin Research 22 (6), 918–32.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. Geological Magazine 148 (5–6), 940–63.Google Scholar
Lacombe, O., Grasemann, B. & Simpson, G. 2011. Introduction: geodynamic evolution of the Zagros. Geological Magazine 148 (5–6), 689–91.Google Scholar
Lamb, M. P. 2008. Formation of amphitheater-headed canyons. Ph.D. thesis, University of California, Berkeley. Published thesis.Google Scholar
Lamb, M. P. & Dietrich, W. E. 2009. The persistence of waterfalls in fractured rock. Geological Society of America Bulletin 121 (7–8), 1123–34.Google Scholar
Lamb, M. P., Howard, A. D., Johnson, J., Whipple, K. X., Dietrich, W. E. & Perron, J. T. 2006. Can springs cut canyons into rock? Journal of Geophysical Research: Planets 111 (E7), E07002, published online 25 July 2006. doi: 10.1029/2005JE002663.Google Scholar
Leblanc, M., Favreau, G., Maley, J., Nazoumou, Y., Leduc, C., Stagnitti, F., Van Oevelen, P. J., Delclaux, F. & Lemoalle, J. 2006. Reconstruction of Megalake Chad using shuttle radar topographic mission data. Palaeogeography, Palaeoclimatology, Palaeoecology 239 (1), 1627.Google Scholar
Lee, J. 2013. A survey of transverse drainages in the Susquehanna River basin, Pennsylvania. Geomorphology 186, 5067.Google Scholar
Leturmy, P., Molinaro, M. & de Lamotte, D. F. 2010. Structure, timing and morphological signature of hidden reverse basement faults in the Fars Arc of the Zagros (Iran). In Tectonic and Stratigraphic Evolution of Zagros and Makran during the Mesozoic–Cenozoic (eds Leturmy, P. & Robin, C.), pp. 121–38. Geological Society of London, Special Publication no. 330.Google Scholar
Mayer, L., Menichetti, M., Nesci, O. & Savelli, D. 2003. Morphotectonic approach to the drainage analysis in the North Marche region, central Italy. Quaternary International 101, 157–67.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 Bulletin 57 (12), 2367–85.Google Scholar
Molinaro, M., Leturmy, P., Guezou, J.-C., Frizon de Lamotte, D. & Eshraghi, S. 2005. The structure and kinematics of the southeastern Zagros fold-thrust belt, Iran: from thin-skinned to thick-skinned tectonics. Tectonics 24 (3), TC3007, published online 15 June 1005. doi: 10.1029/2004TC001633.Google Scholar
Morisawa, M. 1989. Rivers and valleys of Pennsylvania, revisited. Geomorphology 2 (1–3), 122.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, 2760.Google Scholar
Mouthereau, F., Tensi, J., Bellahsen, N., Lacombe, O., De Boisgrollier, T. & Kargar, S. 2007. Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: the Zagros Folded Belt (Fars, Iran). Tectonics 26 (5), TC5006, published online 27 September 2007. doi: 10.1029/2007TC002098.Google Scholar
Nelson, R. A. 1979. Natural fracture systems: Description and classification: Geologic notes. AAPG Bulletin 63 (12), 2214–21.Google Scholar
Oberlander, T. 1965. The Zagros Streams. Syracuse, NY: Syracuse University Press, 168 pp.Google Scholar
Oveisi, B., Lavé, 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 (2), 627–54.Google Scholar
Paola, C., Straub, K., Mohrig, D. & Reinhardt, L. 2009. The ‘unreasonable effectiveness’ of stratigraphic and geomorphic experiments. Earth Science Reviews 97 (1–4), 143.Google Scholar
Ramsey, L. A., Walker, R. T. & Jackson, J. 2008. Fold evolution and drainage development in the Zagros mountains of Fars province, SE Iran. Basin Research 20 (1), 2348.Google Scholar
Regard, V., Bellier, O., Braucher, R., Gasse, F., Bourlès, D., Mercier, J., Thomas, J. C., Abbassi, M., Shabanian, E. & Soleymani, S. 2006. 10Be dating of alluvial deposits from southeastern Iran (the Hormoz Strait area). Palaeogeography, Palaeoclimatology, Palaeoecology 242 (1), 3653.Google Scholar
Reif, D., Decker, K., Grasemann, B. & Peresson, H. 2012. Fracture patterns in the Zagros fold-and-thrust belt, Kurdistan Region of Iraq. Tectonophysics 576, 4662.Google Scholar
Roehler, H. W. 1992. Introduction to great Green River basin geology, physiography, and history of investigations. US Geological Survey Professional Paper 1506-A, 14 pp.Google Scholar
Sack, D. 2009. Evidence for climate change from desert basin palaeolakes. In Geomorphology of Desert Environments, 2nd edition (eds Parsons, A. J. & Abrahams, A. D.), pp. 743–56. The Netherlands: Springer.Google Scholar
Saville, C. 2013. Fluvial and tectonic geomorphology of orogenic plateaux. Ph.D. thesis, Durham University, UK. Published thesis.Google Scholar
Shaban, A., Sherkati, S. & Miri, S. A. 2011. Comparison between curvature and 3D strain analysis methods for fracture predicting in the Gachsaran oil field (Iran). Geological Magazine 148 (5–6), 868–78.Google Scholar
Sherkati, S. & Letouzey, J. 2004. Variation of structural style and basin evolution in the central Zagros (Izeh zone and Dezful Embayment), Iran. Marine and Petroleum Geology 21 (5), 535–54.Google Scholar
Sherkati, S., Letouzey, J. & Frizon de Lamotte, D. 2006. Central Zagros fold-thrust belt (Iran): New insights from seismic data, field observation, and sandbox modeling. Tectonics 25 (4), TC4007, published online 20 July 2006. doi: 10.1029/2004TC001766.Google Scholar
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. Journal of Structural Geology 27 (9), 1680–96.Google Scholar
Simpson, C., De Paor, D., Beebe, M. R. & Strand, J. R. 2012. Google Earth and virtual visualizations in geoscience education and research. In Google Earth and Virtual Visualizations in Geoscience and Research (eds Whitmeyer, S. J., Bailey, J. B., De Paor, D. G. & Ornduff, T.), pp. 183–97. Geological Society of America, Special Paper 492.Google Scholar
Sklar, L. S. & Dietrich, W. E. 2004. A mechanistic model for river incision into bedrock by saltating bed load. Water Resources Research 40 (6), W06301, published online 18 June 2004. doi: 10.1029/2003WR002496.Google Scholar
Sobel, E. R., Hilley, G. E. & Strecker, M. R. 2003. Formation of internally drained contractional basins by aridity-limited bedrock incision. Journal of Geophysical Research: Solid Earth 108 (B7), 2344, published online 22 July 2003. doi: 10.1029/2002JB001883.Google Scholar
Stearns, D. W. & Friedman, M. 1972. Reservoirs in fractured rock: Geologic exploration methods. In Stratigraphic Oil and Gas Fields - Classification, Exploration Methods and Case Histories (ed. Gould, H. R.), pp. 82106. American Association of Petroleum Geology, Special Volumes.Google Scholar
Stocklin, J. 1974. Possible ancient continental margins in Iran. In The Geology of Continental Margins (eds Burk, C. A. & Drake, C. L.), pp. 873–87. Berlin, Heidelberg: Springer.Google Scholar
Strecker, M., Alonso, R., Bookhagen, B., Carrapa, B., Hilley, G., Sobel, E. & Trauth, M. 2007. Tectonics and climate of the southern central Andes. Annual Review of Earth and Planetary Sciences 35, 747–87.Google Scholar
Tooth, S. 2013. Google Earth in geomorphology: re-enchanting, revolutionizing, or just another resource? In Treatise on Geomorphology (eds Shroder, J., Switzer, A. D. & Kennedy, D.), pp. 5364. San Diego: Academic Press, Methods in Geomorphology, no. 14.Google Scholar
Tucker, G. E. & Slingerland, R. 1996. Predicting sediment flux from fold and thrust belts. Basin Research 8 (3), 329–49.Google Scholar
Twidale, C. R. 2004. River patterns and their meaning. Earth-Science Reviews 67 (3–4), 159218.Google Scholar
Twidale, C. R. & Bourne, J. A. 2007. Fractures as planes of dislocation and two-way translocation: Their significance in landform development. Physical Geography 28 (3), 193217.Google Scholar
Vergés, J. 2007. Drainage responses to oblique and lateral thrust ramps: a review. In Sedimentary Processes, Environments and Basins: A Tribute to Peter Friend (eds Nichols, G., Paola, C. & Williams, E.), pp. 2947. Blackwell Publishing, International Association of Sedimentologists, Special Publication no. 38.Google Scholar
Walker, R. T. & Fattahi, M. 2011. A framework of Holocene and Late Pleistocene environmental change in eastern Iran inferred from the dating of periods of alluvial fan abandonment, river terracing, and lake deposition. Quaternary Science Reviews 30 (9), 1256–71.Google Scholar
Walker, R. T., Ramsey, L. A. & Jackson, J. 2011. Geomorphic evidence for ancestral drainage patterns in the Zagros Simple Folded Zone and growth of the Iranian plateau. Geological Magazine 148 (5–6), 901–10.Google Scholar
Wohl, E. 2012. The complexity of the real world in the context of the field tradition in geomorphology. Geomorphology 200, 50–8.Google Scholar
Zebari, M. 2013. Geometry and evolution of fold structures within the High Folded Zone: Zagros Fold-Thrust Belt, Kurdistan region, Iraq. Master's thesis, University of Nebraska, Lincoln, Nebraska. Published thesis.Google Scholar
Zelilidis, A. 2000. Drainage evolution in a rifted basin, Corinth graben, Greece. Geomorphology 35 (1–2), 6985.CrossRefGoogle Scholar
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