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Journal Abstract Search

158 related items for PubMed ID: 35039494

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  • 23. Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates.
    Proctor BP, Mitchell TM, Hirth G, Goldsby D, Zorzi F, Platt JD, Di Toro G.
    J Geophys Res Solid Earth; 2014 Nov; 119(11):8107-8131. PubMed ID: 26167425
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  • 26. Shallow fault-zone dilatancy recovery after the 2003 Bam earthquake in Iran.
    Fielding EJ, Lundgren PR, Bürgmann R, Funning GJ.
    Nature; 2009 Mar 05; 458(7234):64-8. PubMed ID: 19262670
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  • 27. The impact of melt versus mechanical wear on the formation of pseudotachylyte veins in accretionary complexes.
    Moris-Muttoni B, Raimbourg H, Augier R, Champallier R, Le Trong E.
    Sci Rep; 2022 Jan 27; 12(1):1529. PubMed ID: 35087135
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  • 32. Frequency-Magnitude Statistics of Laboratory Foreshocks Vary With Shear Velocity, Fault Slip Rate, and Shear Stress.
    Bolton DC, Shreedharan S, Rivière J, Marone C.
    J Geophys Res Solid Earth; 2021 Nov 27; 126(11):e2021JB022175. PubMed ID: 35865108
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  • 34. Seismic potential of weak, near-surface faults revealed at plate tectonic slip rates.
    Ikari MJ, Kopf AJ.
    Sci Adv; 2017 Nov 27; 3(11):e1701269. PubMed ID: 29202027
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  • 35. Friction falls towards zero in quartz rock as slip velocity approaches seismic rates.
    Di Toro G, Goldsby DL, Tullis TE.
    Nature; 2004 Jan 29; 427(6973):436-9. PubMed ID: 14749829
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  • 38. An unload-induced direct-shear model for granular gouge friction in rock discontinuities.
    Wu W, Zou Y, Li X, Zhao J.
    Rev Sci Instrum; 2014 Sep 29; 85(9):093902. PubMed ID: 25273734
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  • 39. 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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