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THREE-DIMENSIONAL P-VELOCITY STRUCTURE OF THE SUMMIT CALDERA OF NEWBERRY VOLCANO, OREGON.

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, , , and

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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.

Additional Publication Details

Publication type:
Conference Paper
Publication Subtype:
Conference Paper
Title:
THREE-DIMENSIONAL P-VELOCITY STRUCTURE OF THE SUMMIT CALDERA OF NEWBERRY VOLCANO, OREGON.
ISBN:
093441260X
Volume
9
Issue:
pt 2
Year Published:
1985
Language:
English
Publisher:
Geothermal Resources Council
Publisher location:
Davis, CA, USA
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, USA