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205 related items for PubMed ID: 31024064

  • 1. Buoyant hydrous mantle plume from the mantle transition zone.
    Kuritani T, Xia QK, Kimura JI, Liu J, Shimizu K, Ushikubo T, Zhao D, Nakagawa M, Yoshimura S.
    Sci Rep; 2019 Apr 25; 9(1):6549. PubMed ID: 31024064
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  • 2. Continental flood basalts derived from the hydrous mantle transition zone.
    Wang XC, Wilde SA, Li QL, Yang YN.
    Nat Commun; 2015 Jul 14; 6():7700. PubMed ID: 26169260
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  • 9. High 3He/4He in central Panama reveals a distal connection to the Galápagos plume.
    Bekaert DV, Gazel E, Turner S, Behn MD, de Moor JM, Zahirovic S, Manea VC, Hoernle K, Fischer TP, Hammerstrom A, Seltzer AM, Kulongoski JT, Patel BS, Schrenk MO, Halldórsson SA, Nakagawa M, Ramírez CJ, Krantz JA, Yücel M, Ballentine CJ, Giovannelli D, Lloyd KG, Barry PH.
    Proc Natl Acad Sci U S A; 2021 Nov 23; 118(47):. PubMed ID: 34799449
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  • 12. LIP formation and protracted lower mantle upwelling induced by rifting and delamination.
    Petersen KD, Schiffer C, Nagel T.
    Sci Rep; 2018 Nov 08; 8(1):16578. PubMed ID: 30410091
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  • 18. Insights into the dynamics of mantle plumes from uranium-series geochemistry.
    Bourdon B, Ribe NM, Stracke A, Saal AE, Turner SP.
    Nature; 2006 Dec 07; 444(7120):713-7. PubMed ID: 17151659
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  • 20. Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation.
    Doucet LS, Li ZX, Gamal El Dien H.
    Sci Rep; 2021 Aug 20; 11(1):16958. PubMed ID: 34417509
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