- http://id.worldcat.org/fast/1205660
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/surface_to_surface_missiles
- http://id.worldcat.org/fast/1204269
- http://id.worldcat.org/fast/900899
- http://id.worldcat.org/fast/1111285
- http://id.loc.gov/authorities/subjects/sh85119630
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/ground_motion
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/guided_missile_launching_and_basing_support
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/new_mexico
- http://id.loc.gov/authorities/subjects/sh85040496
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/seismic_data
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/hazards
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/launching_sites
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/confidence_level
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/nevada
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/seismic_waves
- http://experiment.worldcat.org/entity/work/data/3655096#Topic/seismology

- "Seismic hazard evaluations were conducted for specific sites in New Mexico and Nevada. For New Mexico, a model of seismicity was developed from historical accounts of medium to large shocks and the current microactivity record from local networks. Ninety percent confidence levels at Albuquerque and Roswell were computed to be 56 gals for a 10-year period and 77 gals for a 20-year period. Values of ground motion for Clovis were below these values. Peak velocity and displacement were also computed for each site. Deterministic spectra based on the estimated maximum credible earthquake for the zones which the sites occupy were also computed. For the sites in Nevada, the regionalizations used in Battis (1982) for the 'uniform seismicity' model were slightly modified. For 10- and 20-year time periods, peak acceleration values for Indian Springs were computed to be 94 gals and 123 gals and for Hawthorne 206 gals and 268 gals. Deterministic spectra were also computed. The input parameters were well determined for the analysis for the Nevada sites because of the abundance of data. The values computed for New Mexico, however, are likely upper limits. As more data are collected from the area of the Rio Grande rift zone, the pattern of seismicity will become better understood. At this time a more detailed, and thus more accurate, model may emerge."@en