Fold evolution and drainage development in the Zagros mountains of Fars province, SE Iran
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[1] J. Cosgrove,et al. Structural framework of the Zagros Fold-Thrust Belt, Iran , 2004 .
[2] R. Stoneley,et al. Subsidence history of the Middle East Zagros Basin, Permian to Recent , 1982, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[3] J. Mugnier,et al. Control of detachment dip on drainage development in regions of active fault-propagation folding , 2002 .
[4] Stephen M. Jones,et al. Onset of subduction as the cause of rapid pliocene-quaternary subsidence in the South Caspian Basin. , 2002 .
[5] D. F. D. Lamotte,et al. The origin of changes in structural style across the Bandar Abbas syntaxis, SE Zagros (Iran) , 2004 .
[6] Patience A. Cowie,et al. Displacement-length scaling relationship for faults: data synthesis and discussion , 1992 .
[7] M. Alavi,et al. Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution , 2004 .
[8] Christopher H. Scholz,et al. Scaling laws for large earthquakes: Consequences for physical models , 1982 .
[9] J. Vergés,et al. Magnetostratigraphy of Miocene–Pliocene Zagros foreland deposits in the front of the Push-e Kush Arc (Lurestan Province, Iran) , 2004 .
[10] J. Walsh,et al. Analysis of the relationship between displacements and dimensions of faults , 1988 .
[11] A. Nicol,et al. An alternative model for the growth of faults , 2002 .
[12] E. Shabanian,et al. Late Cenozoic partitioning of oblique plate convergence in the Zagros fold‐and‐thrust belt (Iran) , 2006 .
[13] T. Oberlander,et al. THE ORIGIN OF THE ZAGROS DEFILES , 1968 .
[14] M. Allen,et al. Structural styles in the Zagros Simple Folded Zone, Iran , 2003, Journal of the Geological Society.
[15] D. Stockli,et al. Exhumation of the west-central Alborz Mountains, Iran, Caspian subsidence, and collision-related tectonics , 2001 .
[16] J. Jackson,et al. Offset on the Main Recent Fault of NW Iran and implications for the late Cenozoic tectonics of the Arabia-Eurasia collision zone , 2001 .
[17] F. Masson,et al. Difference in the GPS deformation pattern of North and Central Zagros (Iran) , 2006 .
[18] D. Sanderson,et al. Displacements, segment linkage and relay ramps in normal fault zones , 1991 .
[19] Frederic Masson,et al. Present‐day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman , 2004 .
[20] Demitris Paradissis,et al. Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus , 2000 .
[21] G. Simpson. Role of river incision in enhancing deformation , 2004 .
[22] James Jackson,et al. The 2005 Qeshm Island earthquake (Iran)—a link between buried reverse faulting and surface folding in the Zagros Simply Folded Belt? , 2007 .
[23] S. Colman-Sadd. Fold Development in Zagros Simply Folded Belt, Southwest Iran , 1978 .
[24] M. Berberian,et al. Towards a paleogeography and tectonic evolution of Iran: Reply , 1981 .
[25] S. J. Haynes,et al. Evolution of the Zagros Suture Zone, Southern Iran , 1974 .
[26] J. Jackson,et al. A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran , 2004 .
[27] James Jackson,et al. Late Cenozoic reorganization of the Arabia‐Eurasia collision and the comparison of short‐term and long‐term deformation rates , 2004 .
[28] Sanjeev Gupta. Himalayan drainage patterns and the origin of fluvial megafans in the Ganges foreland basin , 1997 .
[29] N. McQuarrie,et al. Crustal scale geometry of the Zagros fold–thrust belt, Iran , 2004 .
[30] S. Ouchi. Response of alluvial rivers to slow active tectonic movement , 1985 .
[31] S. Sherkati,et al. Detachment folding in the Central and Eastern Zagros fold-belt (Iran): salt mobility, multiple detachments and late basement control , 2005 .
[32] M. Alavi. TECTONICS OF THE ZAGROS OROGENIC BELT OF IRAN - NEW DATA AND INTERPRETATIONS , 1994 .
[33] Andrea Walpersdorf,et al. The present‐day deformation of the central Zagros from GPS measurements , 2002 .
[34] O. Lacombe,et al. The Zagros folded belt (Fars, Iran): constraints from topography and critical wedge modelling , 2006 .
[35] M. Berberian. Master “blind” thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics , 1995 .
[36] C. Mansfield,et al. Fault growth by segment linkage: an explanation for scatter in maximum displacement and trace length data from the Canyonlands Grabens of SE Utah , 1995 .
[37] J. A. Jackson. Reactivation of basement faults and crustal shortening in orogenic belts , 1980, Nature.
[38] M. Strecker,et al. Implications of the fault scaling law for the growth of topography: mountain ranges in the broken foreland of north‐east Tibet , 2004 .
[39] D. Wells,et al. New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement , 1994, Bulletin of the Seismological Society of America.
[40] J. Stock,et al. Cenozoic evolution of Neotethys and implications for the causes of plate motions , 2003 .
[41] Timothy H. Dixon,et al. REVEL: A model for Recent plate velocities from space geodesy , 2002 .
[42] E. Fielding,et al. Growth of South Rough Ridge, Central Otago, New Zealand: using in situ cosmogenic isotopes and geomorphology to study an active, blind reverse fault , 2005 .
[43] D. Frizon de Lamotte,et al. The structure and kinematics of the southeastern Zagros fold‐thrust belt, Iran: From thin‐skinned to thick‐skinned tectonics , 2005 .
[44] J. Mugnier,et al. Growth and lateral propagation of fault‐related folds in the Siwaliks of western Nepal: Rates, mechanisms, and geomorphic signature , 2002 .
[45] R. Stoneley. The geology of the Kuh-e Dalneshin area of southern Iran, and its bearing on the evolution of southern Tethys , 1981, Journal of the Geological Society.
[46] N. Dawers,et al. Displacement-length scaling and fault linkage , 1995 .
[47] Patience A. Cowie,et al. A healing–reloading feedback control on the growth rate of seismogenic faults , 1998 .
[48] K. Davis,et al. Thrust-fault growth and segment linkage in the active Ostler fault zone, New Zealand , 2005 .
[49] P. E. Kent,et al. THE EMERGENT HORMUZ SALT PLUGS OF SOUTHERN IRAN , 1979 .
[50] E. Keller,et al. Geomorphic criteria to determine direction of lateral propagation of reverse faulting and folding , 1999 .
[51] Walter H. F. Smith,et al. New, improved version of generic mapping tools released , 1998 .
[52] J. Stöcklin,et al. Possible Ancient Continental Margins in Iran , 1974 .