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Volumn 27, Issue 13, 2000, Pages 1981-1984

Seismic evidence for a thinner mantle transition zone beneath the South Pacific Superswell

Author keywords

[No Author keywords available]

Indexed keywords

MANTLE STRUCTURE; SEISMIC VELOCITY; TRANSITION ZONE; VELOCITY STRUCTURE;

EID: 0034352820     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999GL011280     Document Type: Article
Times cited : (22)

References (18)
  • 5
    • 0032503196 scopus 로고    scopus 로고
    • Elastic wave velocities of forsterite and its β-spinel form and chemical boundary hypothesis for the 410-km discontinuity
    • (1998) J. Geophys. Res. , vol.103 , pp. 9591-9608
    • Fujisawa, H.1
  • 7
    • 0024928664 scopus 로고
    • The system Mg2SiO4-Fe2SiO4 at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel
    • (1989) J. Geophys. Res. , vol.94 , pp. 15663-15670
    • Katsura, T.1    Ito, E.2
  • 10
    • 0028830309 scopus 로고
    • Direct evidence for the undulation of the 660-km discontinuity beneath Tonga: Comparison of Japan and California array data
    • (1995) Geophys. Res. Lett. , vol.22 , pp. 531-534
    • Niu, F.1    Kawakatsu, H.2
  • 16
    • 0026472472 scopus 로고
    • Upper-mantle seismic discontinuities and the thermal structure of subduction zones
    • (1992) Nature , vol.356 , pp. 678-682
    • Vidale, J.E.1    Benz, H.M.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.