The physics of earthquakes

By Hiroo Kanamori, E. Brodsky. 2001

931 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/a3a455fbead3ab5dec44293a58596d933b90498b

How researchers see this paper

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

In Geophysics

1. A. Bizzarri
2. Massimo Cocco
3. S. Nielsen
4. E. Brodsky
5. S. Marty
6. Kurama Okubo
7. A. Schubnel
8. Á. Corral

Citations in the corpus

• New constraints on mechanisms of remotely triggered seismicity at Long Valley Caldera (2005, background): “where V− and V+ are the crack propagation velocities before and after the imposed stress, respectively, and p is an empirical growth exponent that is measured by laboratory experiments to be at least 10 and is more commonly measured to be 20–40 for rocks [Atkinson, 1984; Kanamori and Brodsky, 2004].”
• Fitting and goodness-of-fit test of non-truncated and truncated power-law distributions (2012, background): “A well known example of (truncated or not) power-law distribution is the Gutenberg-Richter law for earthquake “size” (Kagan, 2002; Kanamori and Brodsky, 2004; Utsu, 1999).”
• A thermal pressurization model for the spontaneous dynamic rupture propagation on a three‐dimensional fault: 1. Methodological approach (2006, background): “Several mechanisms have been proposed in the literature to explain this sudden drop of the friction coefficient and the associated dynamic fault weakening; they include melting [Jeffreys, 1942; McKenzie and Brune, 1972; Richards, 1976; Cardwell et al., 1978; Sibson, 1977; Allen, 1979], acoustic flui”
• Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, background): “However, these methods can only be used to infer relative stress changes during a seismic event and thus yield incomplete information about the earthquake source (e.g. the dynamic strength and energy budget remain poorly constrained, e.g. Kanamori and Brodsky, 2004).”
• Dynamics, Radiation, and Overall Energy Budget of Earthquake Rupture With Coseismic Off‐Fault Damage (2019, background): “…is an important parameter to quantify the proportion of radiated energy to the sum of radiated energy and fracture energy, which essentially evaluates the balance between the radiated energy as seismic waves and the dissipated energy due to on- and off-fault fracturing (Kanamori and Brodsky, 2004).”