Deep seismic survey extending from Western Washington to Mist Gas Field, Oregon. Final report [electronic resource].
- Washington, D.C. : United States. Dept. of Energy, 1992. and Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy.
- Physical Description:
- 31 pages : digital, PDF file
- Additional Creators:
- United States. Department of Energy and United States. Department of Energy. Office of Scientific and Technical Information
- Restrictions on Access:
- Free-to-read Unrestricted online access
- Between October 1988 and September 1990, approximately 217 kilometers of vibroseis seismic reflection data was collected in Washington State. In particular, the profiles were placed to image a body of low resistivity rocks postulated to be marine sediments which were delineated by Stanley using magnetotelluric methods. The low resistivity rocks are known as the Southwestern Washington Cascade Conductor (SWCC). The profile data was processed using standard reflection seismic methods and also state-of-the-art data enhancing and 3-D reconstruction methods. Along with the reflection data, several dynamite refraction profiles and 3 component data were collected. The reflection and refraction data has been interpreted by Lawrence Berkeley Laboratory, Morgantown Energy Technology Center and the University of West Virginia. Results of the Lawrence Berkeley and University of West Virginia work are presented in a separate reports. This report summarizes the data acquisition and processing portions of the project.
- Published through SciTech Connect., 10/01/1992., "doe/mc/24155--3488", "DE94000021", "AB0520000", Hollis, D.D., and Geophysical Systems Corp., Pasadena, CA (United States)
- Type of Report and Period Covered Note:
- Final; 01/01/1988 - 12/31/1992
- Funding Information:
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