Three-dimensional p-velocity structure of the summit caldera of Newberry Volcano, Oregon [electronic resource].
- Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 1985.
- Physical Description:
- Pages: 5 : digital, PDF file
- Additional Creators:
- United States. Department of Energy. Office of Scientific and Technical Information
- Restrictions on Access:
- Free-to-read Unrestricted online access
- A three-dimensional high-resolution seismic study of the summit caldera of Newberry Volcano, Oregon, was conducted by the US Geological Survey using an adaptation of the method applied by Mercessian et al. (1984). Preliminary interpretation of the traveltime residuals reveals a ring of high P-velocity material coinciding with the inner ring fault system of the caldera in the upper 2 km. A zone of lower P velocities extends deeper than 2 km in the center of the caldera. 9 refs., 5 figs.
- Published through SciTech Connect., 01/01/1985., "doe/ra/50294-t4", "DE86005740", Dawson, P.B.; Stauber, D.A.; Iyer, N.M.; Mooney, W.D., and Geological Survey, Menlo Park, CA (USA)
- Funding Information:
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