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Abstract
A three-dimensional high-resolution seismic study of the summit caldera of Newberry Volcano, Oregon, was conducted by the U. S. Geological Survey using an adaptation of the method applied by Nercessian 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.
Study Area
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | Three-dimensional P-velocity structure of he summit caldera of Newberry Volcano, Oregon |
| ISBN | 093441260X |
| Volume | 9 |
| Issue | 2 |
| Year Published | 1985 |
| Language | English |
| Publisher | Geothermal Resources Council |
| Description | 5 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Conference publication |
| Larger Work Title | Transactions - Geothermal resources council |
| First page | 411 |
| Last page | 415 |
| Conference Title | 1985 International Symposium on Geothermal Energy, Geothermal Resources Council 1985 Annual Meeting |
| Conference Location | Kailua-Kona, HI |
| Country | United States |
| State | Oregon |
| Other Geospatial | Newberry Volcano |
| Google Analytic Metrics | Metrics page |