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U.S. Department of Energy
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Velocity logging and seismic velocity of rocks in the Rainier Mesa area, Nevada Test Site, Nevada

Technical Report ·
OSTI ID:7089609
Velocity data obtained in 38 vertical drill holes in the Rainier and Aqueduct Mesa area were evaluated. Twenty-three geophone surveys and 20 acoustic logs were used to define the in-situ velocity of rocks in the region. The vertical velocity profile can be subdivided into the caprock; the unsaturated zone, the base of which is approximately defined by the top of pervasive zeolitization; the saturated zone of zeolitized rocks; and the pre-Tertiary clastic and carbonate rocks. Comparisons of geophone and acoustic log surveys indicate considerable positive drift (higher acoustic log velocity) in several holes, and none of the postulated causes (dispersion, geologic structure, data error, invasion) can be isolated.
Research Organization:
Geological Survey, Las Vegas, NV (USA)
DOE Contract Number:
AI08-86NV10583
OSTI ID:
7089609
Report Number(s):
USGS-OFR-88-380; ON: TI89001653
Country of Publication:
United States
Language:
English