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Journal Abstract Search

181 related items for PubMed ID: 28630912

  • 1. A nearly water-saturated mantle transition zone inferred from mineral viscosity.
    Fei H, Yamazaki D, Sakurai M, Miyajima N, Ohfuji H, Katsura T, Yamamoto T.
    Sci Adv; 2017 Jun; 3(6):e1603024. PubMed ID: 28630912
    [Abstract] [Full Text] [Related]

  • 2. 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
    [Abstract] [Full Text] [Related]

  • 3. Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite.
    Huang X, Xu Y, Karato S.
    Nature; 2005 Apr 07; 434(7034):746-9. PubMed ID: 15815625
    [Abstract] [Full Text] [Related]

  • 4. Metallic iron limits silicate hydration in Earth's transition zone.
    Zhu F, Li J, Liu J, Dong J, Liu Z.
    Proc Natl Acad Sci U S A; 2019 Nov 05; 116(45):22526-22530. PubMed ID: 31636209
    [Abstract] [Full Text] [Related]

  • 5. 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
    [Abstract] [Full Text] [Related]

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  • 7. Electrical conductivity of olivine, wadsleyite, and ringwoodite under upper-mantle conditions.
    Xu Y, Poe BT, Shankland TJ, Rubie DC.
    Science; 1998 May 29; 280(5368):1415-8. PubMed ID: 9603726
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  • 10. Viscosity of bridgmanite determined by in situ stress and strain measurements in uniaxial deformation experiments.
    Tsujino N, Yamazaki D, Nishihara Y, Yoshino T, Higo Y, Tange Y.
    Sci Adv; 2022 Apr 29; 8(13):eabm1821. PubMed ID: 35353572
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  • 12. Earth's interior. Dehydration melting at the top of the lower mantle.
    Schmandt B, Jacobsen SD, Becker TW, Liu Z, Dueker KG.
    Science; 2014 Jun 13; 344(6189):1265-8. PubMed ID: 24926016
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  • 14. Hydration-reduced lattice thermal conductivity of olivine in Earth's upper mantle.
    Chang YY, Hsieh WP, Tan E, Chen J.
    Proc Natl Acad Sci U S A; 2017 Apr 18; 114(16):4078-4081. PubMed ID: 28377520
    [Abstract] [Full Text] [Related]

  • 15. Variation in bridgmanite grain size accounts for the mid-mantle viscosity jump.
    Fei H, Ballmer MD, Faul U, Walte N, Cao W, Katsura T.
    Nature; 2023 Aug 18; 620(7975):794-799. PubMed ID: 37407826
    [Abstract] [Full Text] [Related]

  • 16. 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 18; 3(3):e1601958. PubMed ID: 28345037
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  • 17. Quantitative analysis of hydrogen sites and occupancy in deep mantle hydrous wadsleyite using single crystal neutron diffraction.
    Purevjav N, Okuchi T, Tomioka N, Wang X, Hoffmann C.
    Sci Rep; 2016 Oct 11; 6():34988. PubMed ID: 27725749
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  • 18. Dislocation-accommodated grain boundary sliding as the major deformation mechanism of olivine in the Earth's upper mantle.
    Ohuchi T, Kawazoe T, Higo Y, Funakoshi K, Suzuki A, Kikegawa T, Irifune T.
    Sci Adv; 2015 Oct 11; 1(9):e1500360. PubMed ID: 26601281
    [Abstract] [Full Text] [Related]

  • 19. Seismic evidence of negligible water carried below 400-km depth in subducting lithosphere.
    Green HW, Chen WP, Brudzinski MR.
    Nature; 2010 Oct 14; 467(7317):828-31. PubMed ID: 20927105
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  • 20. Evidence for a Fe3+-rich pyrolitic lower mantle from (Al,Fe)-bearing bridgmanite elasticity data.
    Kurnosov A, Marquardt H, Frost DJ, Ballaran TB, Ziberna L.
    Nature; 2017 Mar 23; 543(7646):543-546. PubMed ID: 28289289
    [Abstract] [Full Text] [Related]

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