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U.S. Department of Energy
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Detection of regional seismic phases on the RSTN at frequencies up to 16 Hz

Conference ·
OSTI ID:5176138

In an ongoing study to determine the capability of in-country seismic stations to monitor nuclear test ban treaties, the detection levels of regional earthquakes in eastern North America recorded on the Regional Seismic Test Network (RSTN) were examined over the entire bandwidth of RSTN. One hundred and nine earthquakes were chosen and ranges in magnitude from 2.0 to 5.1. Over all magnitude ranges, the detection rates were higher for all four phases (P/sub n/, P/sub g/, S/sub n/, L/sub g/) in the low frequency (< 8 Hz) than in the high frequency (> 8 Hz) band. For ranges greater than 1000 km, there are no significant arrivals at the high frequencies. P/sub n/ and S/sub n/ are the most useful phases for detection at high frequencies. P/sub g/ is useful at high frequencies for close distances. The most detections are at the lower frequencies (2-4 Hz) except for L/sub g/, which is best in the 1-2 Hz band. (ACR)

Research Organization:
Lawrence Livermore National Lab., CA (USA). Seismic Monitoring Research Program
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
5176138
Report Number(s):
UCRL-94897; CONF-860183-1; ON: DE86014442
Country of Publication:
United States
Language:
English