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Volumn 190, Issue 1-2, 2001, Pages 57-63

Mineralogy of subducted basaltic crust (MORB) from 25 to 37 GPa, and chemical heterogeneity of the lower mantle

Author keywords

Density; High pressure; Lower mantle; Mid ocean ridge basalts; Slabs

Indexed keywords

CHEMICAL COMPOSITION; HIGH PRESSURE; LOWER MANTLE; MID-OCEAN RIDGE BASALT; SLAB;

EID: 0034900786     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00375-2     Document Type: Article
Times cited : (241)

References (34)
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    • Ono, S.1
  • 20
  • 21
    • 0033583235 scopus 로고    scopus 로고
    • Dipping low-velocity layer in the mid-lower mantle: Evidence for geochemical heterogeneity
    • (1999) Science , vol.283 , pp. 1888-1891
    • Kaneshima, S.1    Helffrich, G.2
  • 23
    • 0028469074 scopus 로고
    • Absence of an aluminous phase in the upper part of the Earth's lower mantle
    • (1994) Nature , vol.370 , pp. 131-133
    • Irifune, T.1
  • 24
    • 0028165606 scopus 로고
    • Constraints on the melting temperature of the lower mantle from high-pressure experiments on MgO and magnesiowüstite
    • (1994) Nature , vol.371 , pp. 506-508
    • Zerr, A.1    Boehler, R.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.