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Modeling two-dimensional structure at the core-mantle boundary

Helmberger, D. V. and Garnero, E. J. and Ding, X. (1996) Modeling two-dimensional structure at the core-mantle boundary. Journal of Geophysical Research B, 101 (B6). 13,963-13,972. ISSN 0148-0227. http://resolver.caltech.edu/CaltechAUTHORS:20121128-103352821

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Abstract

Recent studies of SKS waveform modeling emphasize the strong variation of seismic properties at the core-mantle boundary (CMB) and the need for two-dimensional and three-dimensional waveform modeling capabilities. In particular, the bifurcation of SKS into SP _dKS and SKP _dS near 110° shows strong regional variations. The first of these phases has a P wave diffraction along the bottom of the mantle near the source, while the latter phase occurs at the receiver end. Generalized ray theory proves effective in generating theoretical seismograms in this type of problem because each of these diffractions is associated with a particular transmission coefficient: T_(sp) which transmits shear waves into primary waves when crossing the CMB and T_(sp) which transmits the primary waves back into shear waves at the receiver end. Each region can then be isolated and have its separate fine structure, sharp or gradational. Two classes of boundaries are explored: the CMB as a simple, sharp interface and the CMB with a very low velocity transition layer (10% slower than reference models). The two diffractions produced by these structures have diagnostic arrival times and wave shapes and when combined with the geometric SKS produce distinct waveform characteristics not easily generated by other means. Since the ray paths associated with these three phases are virtually identical in the mantle and only differ along a short sample of CMB and in the one-dimensional fluid core, we can isolate the small localized CMB region sampled. Thus the waveform character of the extended SKS in the range of 105° to 120° becomes an excellent CMB probe which we demonstrate on a small sample of observations from the Fiji-Tonga region as recorded in North America.


Item Type:Article
Related URLs:
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http://dx.doi.org/10.1029/96JB00534DOIUNSPECIFIED
http://www.agu.org/pubs/crossref/1996/96JB00534.shtmlPublisherUNSPECIFIED
Additional Information:© 1996 American Geophysical Union. Received 31 May 1995; revised December 8, 1995; accepted 13 February 1996. This research was supported by the National Science Foundation grant EAR-93-16441. We thank Don Anderson, Larry Burdick, Steve Roecker, and an anonymous referee for constructive reviews and Steve Grand, who first recognized these strange seismograms. This is contribution 5530 of the Division of Geological and Planetary Sciences, California Institute of Technology.
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NSFEAR-93-16441
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Caltech Division of Geological and Planetary Sciences5530
Record Number:CaltechAUTHORS:20121128-103352821
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20121128-103352821
Official Citation: Helmberger, D. V., E. J. Garnero, and X. Ding (1996), Modeling two-dimensional structure at the core-mantle boundary, J. Geophys. Res., 101(B6), 13,963–13,972, doi:10.1029/96JB00534.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:35706
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:28 Nov 2012 18:48
Last Modified:27 Dec 2012 03:04

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