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Volumn 306, Issue 5694, 2004, Pages 259-261

Variable azimuthal anisotropy in earth's lowermost mantle

Author keywords

[No Author keywords available]

Indexed keywords

ANISOTROPY; EARTH (PLANET); MATHEMATICAL MODELS; WAVEFORM ANALYSIS;

EID: 5044226099     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1103411     Document Type: Article
Times cited : (102)

References (34)
  • 22
    • 5044237182 scopus 로고    scopus 로고
    • note
    • We used a full wave-theory method to construct synthetic seismograms (75) for general forms of D″ anisotropy in the D″ layer. This is a convenient method for modeling waves diffracted along a spherical boundary.
  • 26
    • 0002235083 scopus 로고    scopus 로고
    • M. Gurnis, M. Wysession, E. Knittle, B. Buffet, Eds. (American Geophysical Union, Washington, DC)
    • L. Stixrude in The Core-Mantle Boundary Region, M. Gurnis, M. Wysession, E. Knittle, B. Buffet, Eds. (American Geophysical Union, Washington, DC, 1998), pp. 83-96.
    • (1998) The Core-Mantle Boundary Region , pp. 83-96
    • Stixrude, L.1
  • 30
    • 0037741964 scopus 로고    scopus 로고
    • J. Badro et al., Science 300, 789 (2003).
    • (2003) Science , vol.300 , pp. 789
    • Badro, J.1
  • 33
    • 5044221433 scopus 로고    scopus 로고
    • note
    • Additional figures are available as supporting material on Science Online.
  • 34
    • 5044235349 scopus 로고    scopus 로고
    • note
    • We thank M. Bostock for assistance in accessing some of the Canadian National Seismic Network waveform data, S. Ford and D. Wiens for data from the South Pacific, and the Incorporated Research Institutions for Seismology Data Management Center for all other waveform data. This work was supported by the U.S. National Science Foundation. V.M. was on leave to Institut de Physique du Globe de Paris while part of this work was done.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.