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Volumn 86, Issue 1-3, 1994, Pages 147-164

Variability of P660s phases as a consequence of topography of the 660 km discontinuity

Author keywords

[No Author keywords available]

Indexed keywords

AMPLITUDE; CONVERTED PHASE; MOHO; P660S PHASE; TIME DELAY; TOPOGRAPHY;

EID: 0028555084     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/0031-9201(94)05066-X     Document Type: Article
Times cited : (49)

References (30)
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    • Effects of phase transitions and possible compositional changes on the seismological structure near 650 km depth
    • (1991) Geophys. Res. Lett. , vol.18 , pp. 1743-1746
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    • (1988) Tectonics , vol.7 , pp. 141-155
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  • 16
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  • 17
    • 0343982348 scopus 로고
    • Seismic reflections from the upper mantle discontinuities beneath the Mid-Atlantic Ridge observed by a seismic array in Hokkaido Region, Japan
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  • 22
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    • S-P conversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity
    • (1990) J. Geophys. Res. , vol.101 , pp. 1-35
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  • 23
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    • Global mapping of topography on the 660-km discontinuity
    • (1992) Nature , vol.355 , pp. 791-796
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  • 28
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    • Detection of underside P reflections at mantle discontinuities by stacking broadband data
    • (1988) Geophys. Res. Lett. , vol.15 , pp. 669-672
    • Wajeman1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.