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; October 2003; v. 93; no. 5; p. 1984-1993; DOI: 10.1785/0120020056
© 2003 Seismological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (6)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Morozov, I. B.
Right arrow Articles by Dueker, K. G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Depth-Domain Processing of Teleseismic Receiver Functions and Generalized Three-Dimensional Imaging

Igor B. Morozov and Kenneth G. Dueker

Department of Geological Sciences
University of Saskatchewan
Saskatoon, SK S7N 5E2, Canada
(I.B.M.)

Department of Geology and Geophysics
University of Wyoming
Laramie, WY 82071
(K.G.D.)

Stacking, either by itself or as a part of depth migration, is usually used for noise suppression in teleseismic receiver function (RF) images. However, stacking is neither the only signal enhancement method available, nor is it the most efficient in the environment of receiver-side source-generated noise typical for RF imaging. We generalize prestack depth migration methodology by introducing numerous signal-enhancement schemes in place of final summation. The method operates in full 3D, incorporates most of the existing imaging techniques, and suggests a generalized framework of RF depth imaging. We present four applications of this technique using the data from the teleseismic Continental Dynamics–Rocky Mountains teleseismic experiment: (1) building common-image gathers to assess depth focusing of RF images, (2) imaging using median and (3) coherency filters for noise suppression, and (4) generalized 3D common conversion point stacking. The results suggest that with the limited volumes and quality of the existing RF datasets, adaptive filters could be superior to record summation used in conventional depth migration.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
Crustal Scattering and Some Artifacts in Receiver Function Images
Bulletin of the Seismological Society of America, August 1, 2004; 94(4): 1492 - 1499.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2003 by the Seismological Society of America.