438 related articles for article (PubMed ID: 21998385)
1. Flash heating leads to low frictional strength of crustal rocks at earthquake slip rates.
Goldsby DL; Tullis TE
Science; 2011 Oct; 334(6053):216-8. PubMed ID: 21998385
[TBL] [Abstract][Full Text] [Related]
2. Friction falls towards zero in quartz rock as slip velocity approaches seismic rates.
Di Toro G; Goldsby DL; Tullis TE
Nature; 2004 Jan; 427(6973):436-9. PubMed ID: 14749829
[TBL] [Abstract][Full Text] [Related]
3. Intermittent lab earthquakes in dynamically weakening fault gouge.
Rubino V; Lapusta N; Rosakis AJ
Nature; 2022 Jun; 606(7916):922-929. PubMed ID: 35650443
[TBL] [Abstract][Full Text] [Related]
4. Fast-moving dislocations trigger flash weakening in carbonate-bearing faults during earthquakes.
Spagnuolo E; Plümper O; Violay M; Cavallo A; Di Toro G
Sci Rep; 2015 Nov; 5():16112. PubMed ID: 26552964
[TBL] [Abstract][Full Text] [Related]
5. Molecular origin of sliding friction and flash heating in rock and heterogeneous materials.
Piroozan N; Sahimi M
Sci Rep; 2020 Dec; 10(1):22264. PubMed ID: 33335303
[TBL] [Abstract][Full Text] [Related]
6. Earthquake slip weakening and asperities explained by thermal pressurization.
Wibberley CA; Shimamoto T
Nature; 2005 Aug; 436(7051):689-92. PubMed ID: 16079843
[TBL] [Abstract][Full Text] [Related]
7. Understanding dynamic friction through spontaneously evolving laboratory earthquakes.
Rubino V; Rosakis AJ; Lapusta N
Nat Commun; 2017 Jun; 8():15991. PubMed ID: 28660876
[TBL] [Abstract][Full Text] [Related]
8. Excitation of San Andreas tremors by thermal instabilities below the seismogenic zone.
Wang L; Barbot S
Sci Adv; 2020 Sep; 6(36):. PubMed ID: 32917611
[TBL] [Abstract][Full Text] [Related]
9. Variations in strength and slip rate along the san andreas fault system.
Jones CH; Wesnousky SG
Science; 1992 Apr; 256(5053):83-6. PubMed ID: 17802597
[TBL] [Abstract][Full Text] [Related]
10. Ultralow friction of carbonate faults caused by thermal decomposition.
Han R; Shimamoto T; Hirose T; Ree JH; Ando J
Science; 2007 May; 316(5826):878-81. PubMed ID: 17495168
[TBL] [Abstract][Full Text] [Related]
11. Talc-bearing serpentinite and the creeping section of the San Andreas fault.
Moore DE; Rymer MJ
Nature; 2007 Aug; 448(7155):795-7. PubMed ID: 17700697
[TBL] [Abstract][Full Text] [Related]
12. Dynamic weakening during earthquakes controlled by fluid thermodynamics.
Acosta M; Passelègue FX; Schubnel A; Violay M
Nat Commun; 2018 Aug; 9(1):3074. PubMed ID: 30082789
[TBL] [Abstract][Full Text] [Related]
13. Micromechanics of sea ice frictional slip from test basin scale experiments.
Sammonds PR; Hatton DC; Feltham DL
Philos Trans A Math Phys Eng Sci; 2017 Feb; 375(2086):. PubMed ID: 28025302
[TBL] [Abstract][Full Text] [Related]
14. Ultra-thin clay layers facilitate seismic slip in carbonate faults.
Smeraglia L; Billi A; Carminati E; Cavallo A; Di Toro G; Spagnuolo E; Zorzi F
Sci Rep; 2017 Apr; 7(1):664. PubMed ID: 28386064
[TBL] [Abstract][Full Text] [Related]
15. 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; 126(3):e2020JB021024. PubMed ID: 33868888
[TBL] [Abstract][Full Text] [Related]
16. The earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway).
Menegon L; Campbell L; Mancktelow N; Camacho A; Wex S; Papa S; Toffol G; Pennacchioni G
Philos Trans A Math Phys Eng Sci; 2021 Mar; 379(2193):20190416. PubMed ID: 33517876
[TBL] [Abstract][Full Text] [Related]
17. Heating, weakening and shear localization in earthquake rupture.
Rice JR
Philos Trans A Math Phys Eng Sci; 2017 Sep; 375(2103):. PubMed ID: 28827427
[TBL] [Abstract][Full Text] [Related]
18. Damage to the shallow Landers fault from the nearby Hector Mine earthquake.
Vidale JE; Li YG
Nature; 2003 Jan; 421(6922):524-6. PubMed ID: 12556890
[TBL] [Abstract][Full Text] [Related]
19. Rapid acceleration leads to rapid weakening in earthquake-like laboratory experiments.
Chang JC; Lockner DA; Reches Z
Science; 2012 Oct; 338(6103):101-5. PubMed ID: 23042892
[TBL] [Abstract][Full Text] [Related]
20. Stable creeping fault segments can become destructive as a result of dynamic weakening.
Noda H; Lapusta N
Nature; 2013 Jan; 493(7433):518-21. PubMed ID: 23302798
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]
