25th Himalaya-Karakoram-Tibet Workshop: San Francisco 2010 : Program and Extended AbstractsNational Science Foundation, San Francisco State University, 2010 - 23 pages |
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Page A-20
... orogenic crust by ductile weakening following thermal relaxation and radioactive heating , augmented by a small component of ' melt ' weakening . Channel flow is driven outward from beneath the orogen by the pressure difference between ...
... orogenic crust by ductile weakening following thermal relaxation and radioactive heating , augmented by a small component of ' melt ' weakening . Channel flow is driven outward from beneath the orogen by the pressure difference between ...
Page A-21
... orogen tectonic models , and most likely in nature as well . The interior plateau region of the orogen will be governed by the flow of hot , weak mid- or lower crust and may develop channel flows or other deformation styles ( Jamieson ...
... orogen tectonic models , and most likely in nature as well . The interior plateau region of the orogen will be governed by the flow of hot , weak mid- or lower crust and may develop channel flows or other deformation styles ( Jamieson ...
Page A-66
... orogen , their thermobarometrical and geochronological evolution place important constraints on the geodynamic evolution of the Himalaya in particular , and continental collisions in general . We report SHRIMP - RG trace element ( REE ) ...
... orogen , their thermobarometrical and geochronological evolution place important constraints on the geodynamic evolution of the Himalaya in particular , and continental collisions in general . We report SHRIMP - RG trace element ( REE ) ...
Common terms and phrases
25th Himalaya-Karakoram-Tibet Workshop ages belt beneath Bhutan Cenozoic Central Tibet channel flow China Cite constraints continental crustal deformation Department of Earth detrital dome Earth Sciences earthquakes eastern erosion evolution exhumation Figure folds foreland Formation Geochronology Geol Geophys Geophysics Geosciences glacial glacier gneiss granite Greater Himalayan Sequence Himalaya Himalaya-Karakoram-Tibet Workshop San Implications INDEPTH India Indian plate indicate Indus isotopic June Kunlun Leech Leo Pargil Lesser Himalayan leucogranites Lhasa lithosphere lower crust Main Central Thrust mantle margin metamorphic migmatites Miocene Moho Nepal normal faults northern Open-File Report ophiolitic orogen Pakistan paleomagnetic Proceedings Qaidam Qaidam Basin Qiangtang Quaternary range region River rocks samples sedimentary sediments seismic Shan shortening southern Tibet strain strike-slip structure subduction surface suture zone tectonic temperature terrane Tethyan Tibet Tibetan Plateau U-Pb U.S. Geological Survey University uplift upper valley velocity western Workshop San Francisco Zanskar zircon