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- Underplating in the Himalaya-Tibet Collision Zone Revealed by . . . - Science
Nábělek et al (p 1371 ) present images of the crust and upper mantle of the Southern Tibetan plateau underthrust northward by the Indian plate, in which they trace the base of the Indian plate to 31°N
- Mapping crustal structure beneath southern Tibet: Seismic evidence for . . .
Nabelek et al (2009) observed a northerly dipping negative interface in the middle crust along the Hi-CLIMB profile and interpreted it as the MHT with a sharp velocity decrease caused by water released from underthrusting sediments In their model the Moho doublet only exists in the Lhasa terrane and the double phase merges south of the IYS
- Underplating in the Himalaya-Tibet Collision Zone Revealed by the Hi . . .
presented here clearly show that multiple e-h pairs can be generated and collected in a nanotube p-n junction Al-though implementation of devices exploiting e-h pair generation into photovoltaic cells will require substantial future effort, the process observed here has substantial implications for such tech-nology and represents a very import
- American Journal of Science, Vol. , September, ,P. 517–548, DOI 10. 2475 . . .
American Journal of Science SEPTEMBER 2009 NUMERICAL SIMULATION OF KINETICALLY-CONTROLLED CALC-SILICATE REACTIONS AND FLUID FLOW WITH TRANSIENT PERMEABILITY AROUND CRYSTALLIZING PLUTONS PETER I NABELEK Department of Geological Sciences, University of Missouri, Columbia, Missouri 65211, USA; nabelekp@missouri edu ABSTRACT
- Underplating in the Himalaya-Tibet Collision Zone Revealed by . . . - Science
In standard semiconduc-tors, competing loss mechanisms restrict impact excitation to extremely large biases (18) These results also differ strongly from pre-vious theory and experiments on SWNTs
- Tomographic imaging of the underthrusting Indian slab and mantle . . .
Analyses of the seismic data recorded during the Hi-CLIMB project have resulted in several important findings on the structure beneath southern to central Tibet, such as crustal heterogeneity (Nabelek et al , 2009), pattern of the Indian slab underthrusting (Liang et al , 2011), and diversity of S-wave splitting between southern and northern
- Underplating in the Himalaya-Tibet Collision Zone Revealed by the Hi . . .
presented here clearly show that multiple e-h pairs can be generated and collected in a nanotube p-n junction Al-though implementation of devices exploiting e-h pair generation into photovoltaic
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