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Elastodynamic analysis for slow tectonic loading with spontaneous rupture episodes on faults with rate‐ and state‐dependent friction
- N. Lapusta, J. Rice, Y. Ben‐Zion, Gutuan Zheng
- Geology
- 10 October 2000
We present an efficient and rigorous numerical procedure for calculating the elastodynamic response of a fault subjected to slow tectonic loading processes of long duration within which there are…
Earthquake clusters in southern California I: Identification and stability
- I. Zaliapin, Y. Ben‐Zion
- Geology
- 1 June 2013
We use recent results on statistical analysis of seismicity to present a robust method for comprehensive detection and analysis of earthquake clusters. The method is based on nearest‐neighbor…
Collective behavior of earthquakes and faults: Continuum‐discrete transitions, progressive evolutionary changes, and different dynamic regimes
- Y. Ben‐Zion
- Geology
- 1 December 2008
Crustal deformation patterns are affected by multiscale granulation and healing processes associated with phase transitions between continuum and discrete states of rocks. The ongoing…
Wrinkle-like slip pulse on a fault between different
- D. Andrews, Y. Ben‐Zion
- Physics
- 10 January 1997
Pulses of slip velocity can propagate on a planar interface governed by a constant coefficient of friction, where the interface separates different elastic materials. Such pulses have been found in…
Potency-magnitude scaling relations for southern California earthquakes with 1.0
- Y. Ben‐Zion, Lupei Zhu
- Geology
- 1 March 2002
Linear and quadratic scaling relations between potency P 0 and local magnitude M L for southern California earthquakes are derived using observed data of small events (1.0 < M L < 3.5) recorded in…
Characterization of Fault Zones
- Y. Ben‐Zion, C. Sammis
- Geology
- 1 March 2003
There are currently three major competing views on the essential geometrical, mechanical, and mathematical nature of faults. The standard view is that faults are (possibly segmented and…
Temporal Changes of Shallow Seismic Velocity Around the Karadere-Düzce Branch of the North Anatolian Fault and Strong Ground Motion
- Zhigang Peng, Y. Ben‐Zion
- Geology
- 1 March 2006
We analyze temporal variations of seismic velocity along the Karadere-Düzce branch of the north Anatolian fault using seismograms generated by repeating earthquake clusters in the aftershock zones of…
Properties of seismic fault zone waves and their utility for imaging low-velocity structures
- Y. Ben‐Zion
- Geology
- 10 June 1998
A two-dimensional solution for the scalar wave equation in a model of two vertical layers between two quarter spaces is used to study properties of seismic waves in a laterally heterogeneous…
Systematic analysis of crustal anisotropy along the Karadere—Düzce branch of the North Anatolian fault
- Zhigang Peng, Y. Ben‐Zion
- Geology
- 1 October 2004
S U M M A R Y We perform a systematic analysis of crustal anisotropy along and around the Karadere–Duzce branch of the North Anatolian fault (NAF), which ruptured during the 1999 Mw 7.4 Izmit and Mw…
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