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
... foreland , and the channel is interpreted to have been uplifted and exhumed to the surface by climate - enhanced erosion focused on the flank of the plateau . Exhumation occurs between coeval basal thrust - sense , and overlying normal ...
... foreland , and the channel is interpreted to have been uplifted and exhumed to the surface by climate - enhanced erosion focused on the flank of the plateau . Exhumation occurs between coeval basal thrust - sense , and overlying normal ...
Page A-159
... Foreland Relationships Yogesh Ray1 , Pradeep Srivastava1 , Y.P. Sundriyal2 1 Wadia Institute of Himalayan Geology , 33 GMS Road , Dehradun 248001 , India , yogeshwihg@gmail.com 2 Department of Geology , HNB Garhwal University , Srinagar ...
... Foreland Relationships Yogesh Ray1 , Pradeep Srivastava1 , Y.P. Sundriyal2 1 Wadia Institute of Himalayan Geology , 33 GMS Road , Dehradun 248001 , India , yogeshwihg@gmail.com 2 Department of Geology , HNB Garhwal University , Srinagar ...
Page A-228
... foreland basin type according to Jordan's classification of foreland basins . Based on rock - types and fossils , five sedimentary facies - belts or petro - stratigraphic units are recognized from north to south in the basin : a flysch ...
... foreland basin type according to Jordan's classification of foreland basins . Based on rock - types and fossils , five sedimentary facies - belts or petro - stratigraphic units are recognized from north to south in the basin : a flysch ...
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