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Journal Abstract Search

619 related items for PubMed ID: 11385569

  • 1. High-pressure polymorphs of olivine and the 660-km seismic discontinuity.
    Chudinovskikh L, Boehler R.
    Nature; 2001 May 31; 411(6837):574-7. PubMed ID: 11385569
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  • 4. The elasticity of the MgSiO3 post-perovskite phase in the Earth's lowermost mantle.
    Iitaka T, Hirose K, Kawamura K, Murakami M.
    Nature; 2004 Jul 22; 430(6998):442-5. PubMed ID: 15269765
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  • 5. Multiple seismic discontinuities near the base of the transition zone in the Earth's mantle.
    Simmons NA, Gurrola H.
    Nature; 2000 Jun 01; 405(6786):559-62. PubMed ID: 10850712
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  • 9. Dislocation creep in MgSiO3 perovskite at conditions of the Earth's uppermost lower mantle.
    Cordier P, Ungár T, Zsoldos L, Tichy G.
    Nature; 2004 Apr 22; 428(6985):837-40. PubMed ID: 15103372
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  • 12. Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite.
    Yoshino T, Manthilake G, Matsuzaki T, Katsura T.
    Nature; 2008 Jan 17; 451(7176):326-9. PubMed ID: 18202656
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  • 14. High-Temperature Phase Transition and Dissociation of (Mg, Fe)SiO3 Perovskite at Lower Mantle Pressures.
    Meade C, Mao HK, Hu J.
    Science; 1995 Jun 23; 268(5218):1743-5. PubMed ID: 17834995
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  • 15. Stability of Perovskite (MgSiO3) in the Earth's Mantle.
    Saxena SK, Dubrovinsky LS, Lazor P, Cerenius Y, Haggkvist P, Hanfland M, Hu J.
    Science; 1996 Nov 22; 274(5291):1357-9. PubMed ID: 8910272
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  • 16. Stability of magnesiowustite in Earth's lower mantle.
    Lin JF, Heinz DL, Mao HK, Hemley RJ, Devine JM, Li J, Shen G.
    Proc Natl Acad Sci U S A; 2003 Apr 15; 100(8):4405-8. PubMed ID: 12660368
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