Seismic imaging for velocity and attenuation structure in geothermal fields [electronic resource].
- Published
- Washington, D.C. : United States. Dept. of Energy, 1989.
Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy. - Physical Description
- Pages: (5 pages) : digital, PDF file
- Additional Creators
- Lawrence Livermore National Laboratory, United States. Department of Energy, and United States. Department of Energy. Office of Scientific and Technical Information
Access Online
- Restrictions on Access
- Free-to-read Unrestricted online access
- Summary
- We have applied the attenuation inversion technique developed by Evans and Zucca (1988) to a seismic tomographic data set taken at Newberry Volcano by Achauer et al. (1988). Our preliminary results suggest that the interpretation of the velocity data by Achauer et al. that a magma chamber is present 3 km beneath the caldera is not confirmed by the attenuation data.
- Report Numbers
- E 1.99:ucrl-100841
E 1.99: conf-891031--11
conf-891031--11
ucrl-100841 - Subject(s)
- Other Subject(s)
- Note
- Published through SciTech Connect.
06/01/1989.
"ucrl-100841"
" conf-891031--11"
"DE90010742"
Annual meeting of the Geothermal Resources Council: the geysers - three decades of achievement: a window on the future, Santa Rosa, CA (USA), 1-4 Oct 1989.
Evans, J.R.; Zucca, J.J. - Funding Information
- W-7405-ENG-48
View MARC record | catkey: 14383741