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Volumn 316, Issue 5830, 2007, Pages 1468-1471

Seismic evidence for deep-water transportation in the mantle

Author keywords

[No Author keywords available]

Indexed keywords

DEEP SEA; MANTLE; SEISMIC DATA; SUBDUCTION; TRANSPORT PROCESS;

EID: 34250182800     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1140855     Document Type: Article
Times cited : (250)

References (31)
  • 3
    • 84867911346 scopus 로고    scopus 로고
    • American Geophysical Union, Washington, DC
    • S. Karato, in Geophys. Monogr. 138 (American Geophysical Union, Washington, DC, 2003), pp. 135-152.
    • (2003) Geophys. Monogr. 138 , pp. 135-152
    • Karato, S.1
  • 13
    • 84975730066 scopus 로고    scopus 로고
    • American Geophysical Union, Washington, DC
    • G. R. Helffrich, in Geophys. Monogr. 96 (American Geophysical Union, Washington, DC, 1996), pp. 215-222.
    • (1996) Geophys. Monogr. 96 , pp. 215-222
    • Helffrich, G.R.1
  • 16
    • 0034700463 scopus 로고    scopus 로고
    • X. Yuan et al., Nature 408, 958 (2000).
    • (2000) Nature , vol.408 , pp. 958
    • Yuan, X.1
  • 22
    • 34250204844 scopus 로고    scopus 로고
    • The bottom of the serpentinite layer appears to be also slightly diffusive because it is not resolved in the higher-frequency image SOM, If serpentinization of the mantle peridotite occurs in an equilibrium manner, this boundary may be expected to be sharp. Our result, however, does not support this scenario. The detailed mechanism of water transportation in the mantle wedge is poorly known, and some additional factor appears to be necessary to fully explain our observation
    • The bottom of the serpentinite layer appears to be also slightly diffusive because it is not resolved in the higher-frequency image (SOM). If serpentinization of the mantle peridotite occurs in an equilibrium manner, this boundary may be expected to be sharp. Our result, however, does not support this scenario. The detailed mechanism of water transportation in the mantle wedge is poorly known, and some additional factor appears to be necessary to fully explain our observation.
  • 23
    • 0007803766 scopus 로고
    • S
    • H. Okada, J. Phys. Earth 27 (suppl.), S53 (1979).
    • (1979) J. Phys. Earth , vol.27 , Issue.SUPPL. , pp. 53
    • Okada, H.1
  • 27
    • 34250162084 scopus 로고    scopus 로고
    • H. Kawakatsu, S. Watada, EOS Trans. AGU 86 (Fall Meet. Suppl.), abstract DI41A (2005).
    • H. Kawakatsu, S. Watada, EOS Trans. AGU 86 (Fall Meet. Suppl.), abstract DI41A (2005).
  • 30
    • 85015631525 scopus 로고    scopus 로고
    • American Geophysical Union, Washington, DC
    • A. Hasegawa, J. Nakajima, in Geophys. Monogr. 150 (American Geophysical Union, Washington, DC, 2004), pp. 81-94.
    • (2004) Geophys. Monogr , vol.150 , pp. 81-94
    • Hasegawa, A.1    Nakajima, J.2
  • 31
    • 34250219925 scopus 로고    scopus 로고
    • We thank H. Iwamori and C. Bina for discussions and J. Nakajima for the tomographic model. An anonymous reviewer provided useful comments. This research was supported by the Japan Society for the Promotion of Science and by the Ministry of Education, Culture, Sports, Science and Technology of Japan
    • We thank H. Iwamori and C. Bina for discussions and J. Nakajima for the tomographic model. An anonymous reviewer provided useful comments. This research was supported by the Japan Society for the Promotion of Science and by the Ministry of Education, Culture, Sports, Science and Technology of Japan.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.