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Volumn 306, Issue 5693, 2004, Pages 91-94

Geochemical evidence for excess iron in the mantle beneath Hawaii

Author keywords

[No Author keywords available]

Indexed keywords

EARTH (PLANET); FLUXES; IRON COMPOUNDS; REACTION KINETICS; VOLCANOES;

EID: 7444237523     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1101050     Document Type: Article
Times cited : (213)

References (30)
  • 16
    • 7544232940 scopus 로고    scopus 로고
    • Materials and methods
    • Materials and methods are available as supporting material on Science Online.
    • Science Online
  • 23
    • 7544242812 scopus 로고    scopus 로고
    • note
    • -4. These experiments imply that metallic liquids in equilibrium with lower mantle mineralogy should be very low in oxygen content and that FeO should be released from the core to the mantle at the CMB, if oxygen is present in the outer core at 9 weight percent (wt %) (FeO = 40 wt %) (22).
  • 30
    • 7544224549 scopus 로고    scopus 로고
    • note
    • We thank S. Sorenson (Smithsonian Institution) and A. T. Anderson for providing samples; A. J. Campbell for support on the Element; and A. D. Brandon, B. Buffett, M. Hirschmann, and C. Langmuir for comments and discussions. Constructive reviews by C.-T. Lee and P. Reiners are gratefully acknowledged. NSF EAR-0309786 (M.H.) supported this work.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.