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Journal Abstract Search

131 related items for PubMed ID: 38215182

  • 21. Aseismic transient slip on the Gofar transform fault, East Pacific Rise.
    Liu Y, McGuire JJ, Behn MD.
    Proc Natl Acad Sci U S A; 2020 May 12; 117(19):10188-10194. PubMed ID: 32345716
    [Abstract] [Full Text] [Related]

  • 22. Earthquake slip weakening and asperities explained by thermal pressurization.
    Wibberley CA, Shimamoto T.
    Nature; 2005 Aug 04; 436(7051):689-92. PubMed ID: 16079843
    [Abstract] [Full Text] [Related]

  • 23. Interaction of natural and hydraulic fractures: the impact on reservoir pressure buildup and risk of shear fault reactivation in the Upper Devonian Duvernay Formation, Fox Creek, Alberta.
    Li Q, Konstantinovskaya E, Zhmodik A, Ibelegbu C.
    Geomech Geophys Geo Energy Ge Resour; 2023 Aug 04; 9(1):21. PubMed ID: 36875936
    [Abstract] [Full Text] [Related]

  • 24. A laboratory perspective on accelerating preparatory processes before earthquakes and implications for foreshock detectability.
    Goebel THW, Schuster V, Kwiatek G, Pandey K, Dresen G.
    Nat Commun; 2024 Jul 03; 15(1):5588. PubMed ID: 38961092
    [Abstract] [Full Text] [Related]

  • 25. Seismicity at the Castor gas reservoir driven by pore pressure diffusion and asperities loading.
    Cesca S, Stich D, Grigoli F, Vuan A, López-Comino JÁ, Niemz P, Blanch E, Dahm T, Ellsworth WL.
    Nat Commun; 2021 Aug 10; 12(1):4783. PubMed ID: 34376685
    [Abstract] [Full Text] [Related]

  • 26. Fault healing promotes high-frequency earthquakes in laboratory experiments and on natural faults.
    McLaskey GC, Thomas AM, Glaser SD, Nadeau RM.
    Nature; 2012 Nov 01; 491(7422):101-4. PubMed ID: 23128232
    [Abstract] [Full Text] [Related]

  • 27. Analytical Solution to Assess the Induced Seismicity Potential of Faults in Pressurized and Depleted Reservoirs.
    Wu H, Vilarrasa V, De Simone S, Saaltink M, Parisio F.
    J Geophys Res Solid Earth; 2021 Jan 01; 126(1):e2020JB020436. PubMed ID: 35860610
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  • 32. Is complex fault zone behaviour a reflection of rheological heterogeneity?
    Fagereng Å, Beall A.
    Philos Trans A Math Phys Eng Sci; 2021 Mar 22; 379(2193):20190421. PubMed ID: 33517872
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  • 34. Creep fronts and complexity in laboratory earthquake sequences illuminate delayed earthquake triggering.
    Cebry SBL, Ke CY, Shreedharan S, Marone C, Kammer DS, McLaskey GC.
    Nat Commun; 2022 Nov 11; 13(1):6839. PubMed ID: 36369222
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  • 36. Fault zone fabric and fault weakness.
    Collettini C, Niemeijer A, Viti C, Marone C.
    Nature; 2009 Dec 17; 462(7275):907-10. PubMed ID: 20016599
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  • 37. The role of fluid pressure in induced vs. triggered seismicity: insights from rock deformation experiments on carbonates.
    Scuderi MM, Collettini C.
    Sci Rep; 2016 Apr 26; 6():24852. PubMed ID: 27112408
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  • 39. Excitation of San Andreas tremors by thermal instabilities below the seismogenic zone.
    Wang L, Barbot S.
    Sci Adv; 2020 Sep 26; 6(36):. PubMed ID: 32917611
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  • 40. Episodic creep events on the San Andreas Fault caused by pore-pressure variations.
    Khoshmanesh M, Shirzaei M.
    Nat Geosci; 2018 Aug 26; 11(8):610-614. PubMed ID: 29937919
    [Abstract] [Full Text] [Related]

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