Session Information2007 Fall Meeting |
Tectonophysics |
Wednesday Afternoon 2 | |||
| Time | Session | Location | Title |
| 1600 | T34C | MW 3018 | Crustal Channel Flow: Processes and Evidence From Ancient and Active Orogens II Presiding: D Grujic, Dalhousie University; G Hilley, Stanford University [Abstracts] |
| 1600 | T34C-01 | MW 3018 | Erosion-Induced Reactivation of the Main Central Thrust zone: Model and Implications for Channel Flow in the Himalayan-Tibetan System C Beaumont, *R A Jamieson, M H Nguyen INVITED [details] |
| 1615 | T34C-02 | MW 3018 | Is rapid exhumation of the High Himalaya driven by ramp overthrusting, the formation of mid-crustal duplex, or out-of-sequence thrusting associated with channel flow? F Herman, *J Avouac, L Bollinger, G Maheo, K Farley, M Harrison INVITED [details] |
| 1630 | T34C-03 | MW 3018 | Unchannelized collapse of thickened continental crust and metamorphic core complex formation *R Bendick, J Baldwin INVITED [details] |
| 1645 | T34C-04 | MW 3018 | Channel Flow in the Deep Crust and its Topographic Expression *L Royden INVITED [details] |
| 1700 | T34C-05 | MW 3018 | Quantifying landscape differences across the Tibet plateau: Implications for topographic relief evolution *J Liu, P Tapponnier, Y Gaudemer, L Ding [details] |
| 1710 | T34C-06 | MW 3018 | U(-Th)-Pb age Constraints on the Timing and Duration of Channel Flow in the Mt. Everest Region, Eastern Himalaya *J M Cottle, M P Searle, M S Horstwood, D J Waters, S R Noble, R R Parrish [details] |
| 1720 | T34C-07 | MW 3018 | Empirical Constraints on Extrusion Mechanisms Derived From Pressure-Temperature-Time Histories From the Himalayan Metamorphic Core (Sutlej Valley, NW India) *J Chambers, M Caddick, T Argles, M Horstwood, N Harris, R Parrish, T Ahmad [details] |
| 1730 | T34C-08 | MW 3018 | Did the Karakoram fault interrupt mid-crustal channel flow in the western Himalaya? *M L Leech [details] |
| 1740 | T34C-09 | MW 3018 | Construction of the Eastern Himalaya by Thick-skinned Thrust Stacking of the Indian Basement: No Lower Crustal Flow from Tibet is Needed *A Yin, C S Dubey, T K Kelty, A A Webb, G E Gehrels, T M Harrison, J Celerie, J Dai [details] |
| 1750 | T34C-10 | MW 3018 | Slip-rate gradients along the eastern Kunlun fault: Implications for crustal strength in eastern Tibet *N Harkins, E Kirby, X Shi, E Wang [details] |