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Journal Abstract Search

263 related items for PubMed ID: 27436676

  • 1.
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  • 3. Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers.
    Uchida N, Nakajima J, Wang K, Takagi R, Yoshida K, Nakayama T, Hino R, Okada T, Asano Y.
    Nat Commun; 2020 Nov 10; 11(1):5676. PubMed ID: 33173070
    [Abstract] [Full Text] [Related]

  • 4. An inverted continental Moho and serpentinization of the forearc mantle.
    Bostock MG, Hyndman RD, Rondenay S, Peacock SM.
    Nature; 2002 May 30; 417(6888):536-8. PubMed ID: 12037564
    [Abstract] [Full Text] [Related]

  • 5. Tracing halogen and B cycling in subduction zones based on obducted, subducted and forearc serpentinites of the Dominican Republic.
    Pagé L, Hattori K.
    Sci Rep; 2017 Dec 19; 7(1):17776. PubMed ID: 29259321
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  • 6. Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface.
    Lee C, Kim Y.
    Sci Rep; 2023 Dec 05; 13(1):21425. PubMed ID: 38052949
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  • 7. Role of warm subduction in the seismological properties of the forearc mantle: An example from southwest Japan.
    Lee C, Kim Y.
    Sci Adv; 2021 Jul 05; 7(28):. PubMed ID: 34244142
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  • 8. Carbonates and intermediate-depth seismicity: Stable and unstable shear in altered subducting plates and overlying mantle.
    Prakash A, Holyoke CW, Kelemen PB, Kirby SH, Kronenberg AK, Lamb WM.
    Proc Natl Acad Sci U S A; 2023 May 23; 120(21):e2219076120. PubMed ID: 37186835
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  • 10. Seismic evidence for a cold serpentinized mantle wedge beneath Mount St Helens.
    Hansen SM, Schmandt B, Levander A, Kiser E, Vidale JE, Abers GA, Creager KC.
    Nat Commun; 2016 Nov 01; 7():13242. PubMed ID: 27802263
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  • 11. Trench-parallel flow and seismic anisotropy in the Mariana and Andean subduction systems.
    Kneller EA, van Keken PE.
    Nature; 2007 Dec 20; 450(7173):1222-5. PubMed ID: 18097407
    [Abstract] [Full Text] [Related]

  • 12. Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edge.
    Jadamec MA, Billen MI.
    Nature; 2010 May 20; 465(7296):338-41. PubMed ID: 20485433
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  • 13. Highly oxidising fluids generated during serpentinite breakdown in subduction zones.
    Debret B, Sverjensky DA.
    Sci Rep; 2017 Sep 04; 7(1):10351. PubMed ID: 28871200
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  • 14. Water input into the Mariana subduction zone estimated from ocean-bottom seismic data.
    Cai C, Wiens DA, Shen W, Eimer M.
    Nature; 2018 Nov 04; 563(7731):389-392. PubMed ID: 30429549
    [Abstract] [Full Text] [Related]

  • 15. Anisotropic thermal conductivity of antigorite along slab subduction impacts seismicity of intermediate-depth earthquakes.
    Chien YH, Marzotto E, Tsao YC, Hsieh WP.
    Nat Commun; 2024 Jun 18; 15(1):5198. PubMed ID: 38890301
    [Abstract] [Full Text] [Related]

  • 16. Seismic imaging of mantle wedge corner flow and arc magmatism.
    Hasegawa A.
    Proc Jpn Acad Ser B Phys Biol Sci; 2018 Jun 18; 94(5):217-234. PubMed ID: 29760317
    [Abstract] [Full Text] [Related]

  • 17. 3D anisotropic structure of the Japan subduction zone.
    Wang Z, Zhao D.
    Sci Adv; 2021 Jan 18; 7(4):. PubMed ID: 33523923
    [Abstract] [Full Text] [Related]

  • 18. Trench-parallel anisotropy produced by foundering of arc lower crust.
    Behn MD, Hirth G, Kelemen PB.
    Science; 2007 Jul 06; 317(5834):108-11. PubMed ID: 17615354
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  • 20. Subducted carbon weakens the forearc mantle wedge in a warm subduction zone.
    Oyanagi R, Okamoto A.
    Nat Commun; 2024 Aug 26; 15(1):7159. PubMed ID: 39187495
    [Abstract] [Full Text] [Related]

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