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126 related items for PubMed ID: 34434077
21. Weak phases production and heat generation control fault friction during seismic slip. Rattez H, Veveakis M. Nat Commun; 2020 Jan 17; 11(1):350. PubMed ID: 31953398 [Abstract] [Full Text] [Related]
22. Evidence for fault weakness and fluid flow within an active low-angle normal fault. Floyd JS, Mutter JC, Goodliffe AM, Taylor B. Nature; 2001 Jun 14; 411(6839):779-83. PubMed ID: 11459052 [Abstract] [Full Text] [Related]
23. The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults. Collettini C, Tesei T, Trippetta F, Scuderi MM, Richardson E, Marone C, Pozzi G, Viti C. J Vis Exp; 2021 Nov 06; (177):. PubMed ID: 34806713 [Abstract] [Full Text] [Related]
26. Dynamic weakening during earthquakes controlled by fluid thermodynamics. Acosta M, Passelègue FX, Schubnel A, Violay M. Nat Commun; 2018 Aug 06; 9(1):3074. PubMed ID: 30082789 [Abstract] [Full Text] [Related]
27. Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway. Dunkel KG, Morales LFG, Jamtveit B. Philos Trans A Math Phys Eng Sci; 2021 Mar 22; 379(2193):20190423. PubMed ID: 33517873 [Abstract] [Full Text] [Related]
29. Fault weakening and earthquake instability by powder lubrication. Reches Z, Lockner DA. Nature; 2010 Sep 23; 467(7314):452-5. PubMed ID: 20865001 [Abstract] [Full Text] [Related]
30. 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 [Abstract] [Full Text] [Related]
32. The role of fluids in lower-crustal earthquakes near continental rifts. Reyners M, Eberhart-Phillips D, Stuart G. Nature; 2007 Apr 26; 446(7139):1075-8. PubMed ID: 17460671 [Abstract] [Full Text] [Related]
37. Seismic potential of weak, near-surface faults revealed at plate tectonic slip rates. Ikari MJ, Kopf AJ. Sci Adv; 2017 Nov 18; 3(11):e1701269. PubMed ID: 29202027 [Abstract] [Full Text] [Related]
38. From slow to fast faulting: recent challenges in earthquake fault mechanics. Nielsen S. Philos Trans A Math Phys Eng Sci; 2017 Sep 28; 375(2103):. PubMed ID: 28827428 [Abstract] [Full Text] [Related]
39. 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 28; 119(11):8107-8131. PubMed ID: 26167425 [Abstract] [Full Text] [Related]
40. Rock mechanics. Superplastic nanofibrous slip zones control seismogenic fault friction. Verberne BA, Plümper O, de Winter DA, Spiers CJ. Science; 2014 Dec 12; 346(6215):1342-4. PubMed ID: 25504714 [Abstract] [Full Text] [Related] Page: [Previous] [Next] [New Search]