Frictional melt and seismic slip
By S. Nielsen, G. Toro, T. Hirose, T. Shimamoto. 2008
174 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/5447cd25921a8381730db2c32df9ebb589f9da48
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In Geophysics
Citations in the corpus
- Three‐dimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating: Effect of heterogeneous hydraulic diffusivity (2010, background): “An important next step would be to incorporate other known mechanisms that affect fault resistance to slip, such as melting [Sirono et al., 2006; Nielsen et al., 2008], reaction‐related pore pressurization [Sulem and Famin, 2009], temperature dependency of the conventional rate‐ and state‐dependent…”
- Statistical physics of fracture, friction, and earthquakes (2011, unknown): “There are some analyses of such systems assuming the Arrhenius-type viscosity (Fialko and Khazan, 2005; Nielsen et al., 2008).”
- Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, methodology): “…proposed that the advanced stages of frictional evolution (after the onset of pervasive melting across the sliding interface) are controlled by the shear resistance of a thin melt layer whose temperature, viscosity and thickness vary as slip evolves (Fialko and Khazan, 2005; Nielsen et al., 2008).”
- Earthquake ruptures with thermal weakening and the operation of major faults at low overall stress levels (2009, background): “…of naturally occurring pseudotachylytes, has been the subject of much work [Sibson, 1975; Spray, 1987, 1992, 1993, 1995; Tsutsumi and Shimamoto, 1997; Matsuzawa, 2004; Fialko and Khazan, 2004; Hirose and Shimamoto, 2005; Di Toro et al., 2006; Sirono et al., 2006; Nielsen et al., 2008].”
- The transition of dynamic rupture styles in elastic media under velocity-weakening friction (2012, background): “Nielsen et al. [2008] observed weakening by frictional melt in laboratory”