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Journal Abstract Search

110 related items for PubMed ID: 17730816

  • 1. Dislocations in spinel and garnet high-pressure polymorphs of olivine and pyroxene: implications for mantle rheology.
    Madon M, Poirier JP.
    Science; 1980 Jan 04; 207(4426):66-8. PubMed ID: 17730816
    [Abstract] [Full Text] [Related]

  • 2. Pyroxene-garnet transformation in coorara meteorite.
    Smith JV, Mason B.
    Science; 1970 May 15; 168(3933):832-3. PubMed ID: 17768916
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  • 3. Sound velocities of majorite garnet and the composition of the mantle transition region.
    Irifune T, Higo Y, Inoue T, Kono Y, Ohfuji H, Funakoshi K.
    Nature; 2008 Feb 14; 451(7180):814-7. PubMed ID: 18273016
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  • 4. Olivine-garnet transformation in a meteorite.
    Mason B, Nelen J, White JS.
    Science; 1968 Apr 05; 160(3823):66-7. PubMed ID: 17808783
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  • 5. Ultradeep (>300 kilometers) ultramafic xenoliths: petrological evidence from the transition zone.
    Sautter V, Haggerty SE, Field S.
    Science; 1991 May 10; 252(5007):827-30. PubMed ID: 17744263
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  • 8. Catalysis of the olivine to spinel transformation by high clinoenstatite.
    Sharp TG, Rubie DC.
    Science; 1995 Aug 25; 269(5227):1095-8. PubMed ID: 17755533
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  • 9. Direct observation of dissociated dislocations in garnet.
    Allen FM, Smith BK, Buseck PR.
    Science; 1987 Dec 18; 238(4834):1695-7. PubMed ID: 17737669
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  • 11. Carbon solubility in olivine and the mode of carbon storage in the Earth's mantle.
    Keppler H, Wiedenbeck M, Shcheka SS.
    Nature; 2003 Jul 24; 424(6947):414-6. PubMed ID: 12879066
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  • 12. Melting relations of the aliende meteorite.
    Seitz MG, Kushiro I.
    Science; 1974 Mar 08; 183(4128):954-7. PubMed ID: 17756754
    [Abstract] [Full Text] [Related]

  • 13. A new high-pressure form of Mg2SiO4 highlighting diffusionless phase transitions of olivine.
    Tomioka N, Okuchi T.
    Sci Rep; 2017 Dec 11; 7(1):17351. PubMed ID: 29229951
    [Abstract] [Full Text] [Related]

  • 14. Ringwoodite lamellae in olivine: Clues to olivine-ringwoodite phase transition mechanisms in shocked meteorites and subducting slabs.
    Chen M, El Goresy A, Gillet P.
    Proc Natl Acad Sci U S A; 2004 Oct 19; 101(42):15033-7. PubMed ID: 15479764
    [Abstract] [Full Text] [Related]

  • 15. An Overview of the Experimental Studies on the Electrical Conductivity of Major Minerals in the Upper Mantle and Transition Zone.
    Dai L, Hu H, Jiang J, Sun W, Li H, Wang M, Vallianatos F, Saltas V.
    Materials (Basel); 2020 Jan 15; 13(2):. PubMed ID: 31952310
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  • 16. 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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  • 17. Pure climb creep mechanism drives flow in Earth's lower mantle.
    Boioli F, Carrez P, Cordier P, Devincre B, Gouriet K, Hirel P, Kraych A, Ritterbex S.
    Sci Adv; 2017 Mar 01; 3(3):e1601958. PubMed ID: 28345037
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  • 18. Single-crystal elastic properties of the modified spinel (Beta) phase of magnesium orthosilicate.
    Sawamoto H, Weidner DJ, Sasaki S, Kumazawa M.
    Science; 1984 May 18; 224(4650):749-51. PubMed ID: 17780624
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  • 19. Striped iron zoning of olivine induced by dislocation creep in deformed peridotites.
    Ando J, Shibata Y, Okajima Y, Kanagawa K, Furusho M, Tomioka N.
    Nature; 1984 May 18; 414(6866):893-5. PubMed ID: 11780058
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  • 20. Metal saturation in the upper mantle.
    Rohrbach A, Ballhaus C, Golla-Schindler U, Ulmer P, Kamenetsky VS, Kuzmin DV.
    Nature; 2007 Sep 27; 449(7161):456-8. PubMed ID: 17898766
    [Abstract] [Full Text] [Related]

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