Off-Fault Secondary Failure Induced by a Dynamic Slip Pulse

By J. Rice, C. Sammis, R. Parsons. 2005

291 citations recorded by the source corpus.

Subfields: Artificial Intelligence, Geophysics

View Paper: https://www.semanticscholar.org/paper/616938cd7a470bf48bac21efb894c8971e7c52b8

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Artificial Intelligence

1. Hiroo Kanamori
2. S. Nielsen
3. D. J. Andrews
4. L. Rivera
5. J. Rice

In Geophysics

1. S. Nielsen
2. J. Rice
3. E. L. Templeton
4. G. Toro
5. Hiroo Kanamori
6. L. Rivera
7. Stephen F. Smith
8. A. Bistacchi

Citations in the corpus

• Rupture dynamics with energy loss outside the slip zone (2003, result): “Rice et al. [2004] extend the results of Poliakov et al. [2002] to a steadily propagating slippulsewithfiniteslippinglength.Theyshowcontoursofa region near the crack tip in which a Coulomb failure criterion ismetandasmaller regioninwhichabsolutetensilevaluesof stress are reached.”
• Energy Partitioning During an Earthquake (2006, background): “Some energy is also expended for near and off-fault cracking associated with fault rupture [Rice et al. 2005; Andrews 2005].”
• Off-fault plasticity and earthquake rupture dynamics: 1. Dry materials or neglect of fluid pressure changes (2008, background): “shallower depths if Dc has weak or no depth dependence [Rice et al., 2005].”
• Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, background): “propagating along a fault, theoretical (Poliakov et al., 2002; Kame et al., 2003; Rice et al., 2005) and experimental (Rosakis et al.”
• Dynamics, Radiation, and Overall Energy Budget of Earthquake Rupture With Coseismic Off‐Fault Damage (2019, methodology): “Since the size of potential failure area is of the same order of magnitude as R0(z) (e.g. Poliakov et al., 2002), the damage zone is expected to decrease with depth, as mentioned by Rice et al. (2005), which is verified by this study.”
• Heating and weakening of faults during earthquake slip (2006, background): “, locally in excess of a Mohr-Coulomb yield criterion, as the rupture front passed by it [Andrews, 1976, 2005; Poliakov et al., 2002; Rice, 1980; Rice et al., 2005].”
• Nonplanar Faults: Mechanics of Slip and Off-fault Damage (2009, background): “Such stresses are highly localized around the rupture front and appear to be sufficiently intense to create a damage zone in the vicinity of the tip of propagating earthquake rupture (ANDREWS, 2004; 2005; RICE et al., 2005).”