The Upper Crustal P-wave Velocity Structure of Newberry Volcano, Central Oregon
xii, 98 p. : ill. (some col.) === The upper-crustal seismic-velocity structure of Newberry volcano, central Oregon, is imaged using P-wave travel time tomography. The inversion combines a densely-spaced seismic line collected in 2008 with two USGS seismic experiments from the 1980s. A high-velocity...
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| Language: | en_US |
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University of Oregon
2011
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| Online Access: | http://hdl.handle.net/1794/11475 |