A source of bias in multiple ScS differential travel times determined by waveform correlation-Reference-Cited by-同舟云学术

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A source of bias in multiple ScS differential travel times determined by waveform correlation

Published:1977-12 Issue:12 Volume:4 Page:593-595
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Butler Rhett

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/v004/i012/GL004i012p00593/GL004i012p00593.pdf

Reference12 articles.

1. The Q of the Earth;Anderson;J. Geophys. Res.,1977

2. Time Function Appropriate for Deep Earthquakes;Burdick;Bull. Seism. Soc. Am.,1974

3. Carpenter , E. W. Absorption of Elastic Waves - an Operator for a Constant Q Mechanism H. M. Stationary Office 1966

4. Dispersive Body Waves;Futterman;J. Geophys. Res.,1962

5. Estimation of the Attenuation Operator for Multiple ScS Waves;Jordon;Geophys. Res. Lett.,1977

Cited by 9 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Global upper mantle structure from long-period differential travel times;Journal of Geophysical Research: Solid Earth;1991-04-10

2. Lateral heterogeneity and azimuthal anisotropy in the North Atlantic determined fromSS-Sdifferential travel times;Journal of Geophysical Research;1987

3. Multiple SCS travel times and attenuation beneath Mexico and Central America;Geophysical Research Letters;1983-04

4. The geoid, small-scale convection, and differential travel time anomalies of shear waves in the central Indian Ocean;Journal of Geophysical Research;1983

5. Travel-time residuals of PP waves reflected under oceanic and continental platform regions;Physics of the Earth and Planetary Interiors;1980-10

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