Interrelation between fault zone structures and earthquake processes

1995 ◽  
Vol 145 (3-4) ◽  
pp. 647-676 ◽  
Author(s):  
Keiiti Aki
Keyword(s):  
Fault Zone ◽  
Fault Zone Structures

scholarly journals High-resolution Imaging of Fault Zone Structures with Seismic Fault Zone Waves

2007 ◽  
Vol SpecialIssue ◽  
pp. 78-79 ◽  
Author(s):  
Y. Ben-Zion ◽  
Z. Peng ◽  
M. Lewis ◽  
J. McGuire
Keyword(s):  
High Resolution ◽  
Fault Zone ◽  
High Resolution Imaging ◽  
Seismic Fault ◽  
Resolution Imaging ◽  
Fault Zone Structures ◽  
Fault Zone Waves

No abstract available. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.s01.23.2007" target="_blank">10.2204/iodp.sd.s01.23.2007</a>

scholarly journals Fault zone structures and strain localization in clinoptilolite-tuff (Nižný Hrabovec, Slovak Republic)

2020 ◽  
Vol 138 ◽  
pp. 104090
Author(s):  
Cornelius Tschegg ◽  
Zhaoliang Hou ◽  
A. Hugh N. Rice ◽  
Joachim Fendrych ◽  
Elisabeth Matiasek ◽  
...  
Keyword(s):  
Fault Zone ◽  
Strain Localization ◽  
Slovak Republic ◽  
Fault Zone Structures ◽  
Clinoptilolite Tuff

scholarly journals Characteristics of the Lithology, Fault-Related Rocks and Fault Zone Structures in TCDP Hole-A

2007 ◽  
Vol 18 (2) ◽  
pp. 243 ◽  
Author(s):  
Sheng-Rong Song ◽  
Li-Wei Kuo ◽  
En-Chao Yeh ◽  
Chien-Ying Wang ◽  
Jih-Hao Hung ◽  
...  
Keyword(s):  
Fault Zone ◽  
Fault Zone Structures

Modeling fault‐zone guided waves of microearthquakes in a geothermal reservoir

Geophysics ◽  
1997 ◽  
Vol 62 (4) ◽  
pp. 1278-1284 ◽  
Author(s):  
Min Lou ◽  
José A. Rial ◽  
P. E. Malin
Keyword(s):  
Fault Zone ◽  
Guided Waves ◽  
Velocity Structure ◽  
Geothermal Field ◽  
Guided Wave ◽  
S Wave ◽  
Low Velocity ◽  
Geothermal Fields ◽  
Coso Geothermal Field ◽  
Fault Zone Structures

Fault‐zone guided waves have been identified in microearthquake seismograms recorded at the Coso Geothermal Field, California. The observed guided waves have particle motions and propagation group velocities similar to Rayleigh wave modes. A numerical method has been employed to simulate the guided‐wave propagation through the fault zone. By comparing observed and synthetic waveforms the fault‐zone width and its P‐ and S‐wave velocity structure have been estimated. It is suggested here that the identification and modeling of such guided waves is an effective tool to locate fracture‐induced, low‐velocity fault‐zone structures in geothermal fields.

Shear strength behavior of Mont Terri Opalinus Claystone in fault zone

2015 ◽  
Vol 10 (1) ◽  
pp. 31-38
Author(s):  
Ildikó Buocz ◽  
Nikoletta Rozgonyi-Boissinot ◽  
Ákos Török
Keyword(s):  
Shear Strength ◽  
Fault Zone ◽  
Strength Behavior ◽  
Mont Terri
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