Willcome to Links to Mantle
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Anisotropic Convection of the Upper Mantle - Anisotropic Convection of the Upper Mantle --
Gaherty: Regional Upper Mantle Models - Regional Upper Mantle Seismic Models. My research, done in conjuction with Tom Jordan (MIT) and Mamoru Kato (Kyoto Univ), has focused on the development... --
The Upper Mantle - Slide 5 of 36. The Upper Mantle. That part of the earth below the crust and above the depth at which quartz based minerals convert to high density phases.. --
The Upper Mantle - The Upper Mantle. That part of the earth below the crust and above the depth at which quartz based minerals convert to high density phases is often... --
Gaherty: Regional Upper Mantle Models - Regional Upper Mantle Seismic Models. My research, done in conjuction with Tom Jordan (MIT) and Mamoru Kato (Kyoto Univ), has focused on the development... --
Seismic studies of the upper mantle and transition zone - Next: Introduction. Seismic studies of the upper mantle and transition zone. Peter M. Shearer. Institute of Geophysics and Planetary Physics, Scripps... --
Crust and Upper Mantle Structure of S. California - Crustal and Upper Mantle Structure of Southern California. B.S. Thesis. 1996 Geophysical Research Letters publication. Recent Modeling Results. Shear-Wave. --
Histogram of Upper Mantle P-Velocity - Histogram of Upper Mantle P-Velocity. Return to SeisView Main Page. --
REBOUND - UPPER MANTLE LATERAL VISCOSITY VARIATIONS AND POSTGLACIAL REBOUND: APPLICATION TO THE BARENTS SEA. Georg Kaufmann. 1. and Patrick Wu. 2. 1. Research... --
Upper Mantle Anisotropy - Next: Upper Mantle Velocity Up: Seismic studies of the Previous: Introduction. Upper Mantle Anisotropy. Recent years have seen a large number of... --
Depths in NA-upper mantle - at a depth of 070 km. at a depth of 100 km. at a depth of 130 km. at a depth of 170 km. at a depth of 200 km. at a depth of 230 km. at a depth of 270 km... --
Upper-mantle S-wave velocity structure - Upper-mantle S-wave velocity structure. Vs anomalies in Indo-Australian plate region. at 25km depth. at 50km depth. at 75km depth. at 100km depth. at... --
The Upper Mantle - Slide 5 of 36. The Upper Mantle. That part of the earth below the crust and above the depth at which quartz based minerals convert to high density phases.. --
Shangxing Gao's Publication: The role of upper mantle localized high temperatu - For Journal of Geophysical Research. The role of upper mantle localized high temperature and partial melting on teleseismic P- and S-wave attenuation.... --
Oceanus Science Slides: Lithosphere - Ocean Drilling Program

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