Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; August 1995; v. 85; no. 4; p. 1244-1248
© 1995 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Chael, E. P.
Right arrow Articles by Pomeroy, P. W.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Propagation of high-frequency (4- to 50-Hz) P waves in the northeastern United States

Eric P. Chael, Patrick J. Leahy, Jerry A. Carter, Noël Barstow and Paul W. Pomeroy

Sandia National Laboratories, MS 0655, Albuquerque, New Mexico 87185
SAIC, 1300 North 17th St., Arlington, Virginia 22209
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
, POB 224, Stone Ridge, New York 10964

Abstract

We have measured the decay rate of high-frequency (4- to 50-Hz) P waves in the northeastern United States. We analyzed signals from 28 explosions of a 1988 USGS/AFGL/GSC refraction survey recorded at distances between 30 and 400 km. Over this range, the decay rate steadily increases from {Delta}–2 at 10 Hz to {Delta}–4 at 45 Hz. If one assumes geometric spreading of {Delta}–1.3, then the remaining decay is consistent with a nearly frequency-independent Q of about 1000. The results provide a useful parameterization for predicting P-wave spectra at near-regional ranges.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1995 by the Seismological Society of America.