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Volumn 28, Issue 9, 2001, Pages 1855-1858

Upper mantle discontinuity structure in the region of the Tonga Subduction Zone

Author keywords

[No Author keywords available]

Indexed keywords

OCEANOGRAPHY; SEISMOLOGY; TECTONICS;

EID: 0035333028     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000GL012192     Document Type: Article
Times cited : (30)

References (19)
  • 3
    • 0001533423 scopus 로고
    • Olivine-Spinel transitions: Experimental and thermodynamic constraints and implications for the nature of the 400-km seismic discontinuity
    • (1987) J. Geophys. Res , vol.92 , pp. 4853-4866
    • Bina, C.R.1    Wood, B.J.2
  • 5
    • 84964203940 scopus 로고
    • Bootstrap methods for standard errors, confidence intervals, and other measures of statistical accuracy
    • (1986) Star. Sci , vol.1 , pp. 54-77
    • Efron, B.1    Tibshirani, R.2
  • 12
    • 0028830309 scopus 로고
    • Direct evidence for the unduration 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
    • 0034213424 scopus 로고    scopus 로고
    • Multiple seismic discontinuities near the base of the transition zone in the Earth's mantle
    • (2000) Nature , vol.405 , pp. 559-562
    • Simmons, N.A.1    Gurrola, H.2
  • 18
    • 0027519006 scopus 로고
    • Catastrophic overturn of the Earth's mantle driven by multiple phase changes and internal heat generation
    • (1993) Geophys. Res. Lett , vol.20 , pp. 101-104
    • Weinstein, S.A.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.