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GRUJIc, D. Channel flow and continental collision tectonics: an overview 25 vo ution of ideas on channel flow and ductile extrusion n the Himalaya-Tibetan Plateau system KLEMPERER, S. L. Crustal flow in Tibet: geophysical vidence for te physical 39 state of Tibetan lithosphere, and inferred patterns of active fow HODGES, K. V. A synthesis of the Channel Flow-Extrusion hypothesis as developed 7 for the Himalayan-Tibetan orogenic system Modeling channel flow and ductile extrusion processes BEAUMONT C., NGUYEN, M. H., JAMIESON, R. A. & ELLIS, S Crustal flow modes in 91 large hot orogens MDVEDEV, S. & BEAUMONT C. Growth of continental plateaus by channel inection 147 models designed to address constraints and thermomechanical consistency JAMIESON, R. A., BEAUMONT, C, NGUYEN, M. H. & GRUJIC, D. Provenance of the 165 Greater Himalayan Sequence and associated rocks: predictions of channel flow models GRASnMANN, B., EDWARDS, M. A & WIESMAYR, G. Kinematic dilatancy effects 183 on orogenic extrusion lONES, R. R. HOLDSWORT, R. E., HAND, M. & G.OSCOMBE, Ductile extrusion in 201 coninental collision zones: ambiguities in the definition of channel flow and its identification in ancient orogens WILL AMS, P. F. JIANG, D. & LIN, S. Interpretation of deformation fabrics of 221 infrastructure zone rocks in the context of channel flow and other tectonic models Gelogica constraints on channel fow and uctile extrusion as an important orogenic process Himalaya-Tibetan Plateau HARRTSON, T. M. Did the Himalayan Crystallines extrude partially molten from 237 beneath the Tibetan Plateau? ROBINSON, D M.i & PEARSON, 0. N. Exhumation of Greater Himalayan rock along 255 the Main Centra Thrust in Nepal: implications for channel low GoIN L, GLEESON, T. P., SEARLE M. P., ULLRICH, T. D. & PARRISiH R. R. 269 ocking f southward extrusion in favour of rapid crustal-scale buckling of the Greater Himalayan sequence, Nar valley, central Nepal SCALLE'r, B. & SEARLE, M P. Mechanisms and timescales of felsic magma 293 segregation, ascent and emplacement in the Himalaya ANNEN, C, & SCAILLE T B. Thermal evolution of leucogranites in extensional faults: 309 impications for Miocene denudation rates in the Himalaya WANG, LL Q. & GUOSHIENG, Q 40Ar /3Ar thermochronological constraints o the 327 cooling and exhumation history of he South Tibetan Detachment System, Nyalam area, southern Tibet SARLE, M. P,, LAW, R. D. & JESSUP, M. J. Crustal structure, restoration and evolution 355 f the Greater Himalaya in Nepal-South Tibet: implications for channel flow and ductile extrusion of the middle crust JFSSUP, M. J., Law. R. D., SEARLE, M. P & IHBBARD, M. S. Structural evolution and 379 orticity of flow during extrusion and exhumation of the Greater Himalayan Slab. Mount Everest Massif, Tibet/Nepal: implications for orogen-scale flow partitioning HoLSTAFR, L. S. & GRUJIC, D. Pulsed channel flow in Bhuan 415 CAROSI R, MONTOMOLI, C., RUBATTO D. & VLSONA D. No ral-sense shear zones 425 n he core of the igher Himalayan Crystallines (Bhutan Himalaya): evidence for extrusion? LEE, J., MCCLELLAND, W., WANG, Y., BLYTHE, A. & MCWILLIAMS, M. 445 Oligocene-Miocene middle crustal flow n southern Tibet: geochronolog of Mabja Dome AOYA, M., WALLS, S. R., KAWAKAMI, T., LEE, J., WANG, Y. & MAEDA, H. 471 The Malashan gneiss dome in south Tibet: comparative study with the Kngmar dome with special reference to kinematics of deformation and origin of associated granites ldletnides and Appalachians XYPOLIAS P. & KOKALAS, S. Heterogeneous ductile deformation along a 497 mid-crustal extuding shear zone: an example from the External Hellenides (Greece) ATCHR, R. D. JR. & MERSCHAT, A, J. The Appalachian Inner Piedmont: 517 an exhumed strke-parallel, tectonically forced orogenic channel dia Cordilera RaOWN R. L. & GISON H. D. An argument for channel flow in the 543 sothen Caadian Cordillera and comparison with Himalayan tectonics CARI . D & SIMONY P. S. Ductile thrustin versus channel flow in the 561 southeastern Canadian Cordillera: evolution of a coherent crystalline thrust sheet KUIR Y. D., WILLIAMS, P. F & KRUSE, S. Possibility of channel flow n 589 he southern Canadian Cordillera: a new approach to explain existing data