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Journal Abstract Search

298 related items for PubMed ID: 31036864

  • 1. Role of Weak Materials in Earthquake Rupture Dynamics.
    Hirono T, Tsuda K, Kaneki S.
    Sci Rep; 2019 Apr 29; 9(1):6604. PubMed ID: 31036864
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  • 2. Low coseismic shear stress on the Tohoku-Oki megathrust determined from laboratory experiments.
    Ujiie K, Tanaka H, Saito T, Tsutsumi A, Mori JJ, Kameda J, Brodsky EE, Chester FM, Eguchi N, Toczko S, Expedition 343 and 343T Scientists.
    Science; 2013 Dec 06; 342(6163):1211-4. PubMed ID: 24311683
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  • 7. Stable creeping fault segments can become destructive as a result of dynamic weakening.
    Noda H, Lapusta N.
    Nature; 2013 Jan 24; 493(7433):518-21. PubMed ID: 23302798
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  • 10. Microphysical Modeling of Carbonate Fault Friction at Slip Rates Spanning the Full Seismic Cycle.
    Chen J, Niemeijer AR, Spiers CJ.
    J Geophys Res Solid Earth; 2021 Mar 24; 126(3):e2020JB021024. PubMed ID: 33868888
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  • 14. Earthquake slip weakening and asperities explained by thermal pressurization.
    Wibberley CA, Shimamoto T.
    Nature; 2005 Aug 04; 436(7051):689-92. PubMed ID: 16079843
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  • 15. Seismic potential of weak, near-surface faults revealed at plate tectonic slip rates.
    Ikari MJ, Kopf AJ.
    Sci Adv; 2017 Nov 04; 3(11):e1701269. PubMed ID: 29202027
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  • 16. Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone.
    Aretusini S, Meneghini F, Spagnuolo E, Harbord CW, Di Toro G.
    Nat Commun; 2021 Apr 30; 12(1):2481. PubMed ID: 33931641
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  • 19. Presence of interplate channel layer controls of slip during and after the 2011 Tohoku-Oki earthquake through the frictional characteristics.
    Nakata R, Hori T, Miura S, Hino R.
    Sci Rep; 2021 Mar 19; 11(1):6480. PubMed ID: 33742049
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  • 20. Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake.
    Sun T, Wang K, Iinuma T, Hino R, He J, Fujimoto H, Kido M, Osada Y, Miura S, Ohta Y, Hu Y.
    Nature; 2014 Oct 02; 514(7520):84-7. PubMed ID: 25231864
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