scholarly journals First ionospheric images of the seismic fault slip on the example of the Tohoku-oki earthquake

2011 ◽  
Vol 38 (22) ◽  
pp. n/a-n/a ◽  
Author(s):  
Elvira Astafyeva ◽  
Philippe Lognonné ◽  
Lucie Rolland
Keyword(s):  
Fault Slip ◽  
Seismic Fault

Carbon-forming reactions under a reducing atmosphere during seismic fault slip

Geology ◽  
2014 ◽  
Vol 42 (9) ◽  
pp. 787-790 ◽  
Author(s):  
Kiyokazu Oohashi ◽  
Raehee Han ◽  
Takehiro Hirose ◽  
Toshihiko Shimamoto ◽  
Kentaro Omura ◽  
...  
Keyword(s):  
Fault Slip ◽  
Reducing Atmosphere ◽  
Seismic Fault

A New Insight into the Influence of Composition of Fault Rocks on Aseismic and Seismic Fault Slip

2019 ◽  
Vol 93 (3) ◽  
pp. 760-762
Author(s):  
Xiangli HE ◽  
Haibing LI ◽  
Huan WANG ◽  
Jialiang SI ◽  
Lei ZHANG ◽  
...  
Keyword(s):  
Fault Slip ◽  
Fault Rocks ◽  
Seismic Fault ◽  
Insight Into

Frictional melting of clayey gouge during seismic fault slip: Experimental observation and implications

2014 ◽  
Vol 41 (15) ◽  
pp. 5457-5466 ◽  
Author(s):  
Raehee Han ◽  
Takehiro Hirose ◽  
Gi Young Jeong ◽  
Jun-ichi Ando ◽  
Hideki Mukoyoshi
Keyword(s):  
Experimental Observation ◽  
Fault Slip ◽  
Seismic Fault ◽  
Frictional Melting

scholarly journals GLOBAL RELATIONS BETWEEN SEISMIC FAULT PARAMETERS AND MOMENT MAGNITUDE OF EARTHQUAKES

2004 ◽  
Vol 36 (3) ◽  
pp. 1482 ◽  
Author(s):  
B. C. Papazachos ◽  
E. M. Scordilis ◽  
D. G. Panagiotopoulos ◽  
C. B. Papazachos ◽  
G. F. Karakaisis
Keyword(s):  
Seismic Moment ◽  
Strike Slip ◽  
Fault Slip ◽  
Moment Magnitude ◽  
Empirical Formulas ◽  
Seismic Fault ◽  
Fault Parameters ◽  
The Moment ◽  
Fault Length ◽  
Global Relations

The most reliable of the globally available relative data have been used to derive empirical formulas which relate the subsurface fault length, L, the fault area, S, and fault width, w, with the moment magnitude, M. Separate such formulas have been derived for earthquakes generated by strike-slip faulting, by dip-slip faulting in continental regions and by dip-slip faulting in lithospheric subduction regions. The formula which relates the fault area with the magnitude is combined with the definition formulas of seismic moment and moment magnitude to derive also relations between the fault slip, u, and the moment magnitude for each of the three seismotectonic regimes. For a certain magnitude, the fault length is larger for strike-slip faults than for dip-slip faults, while the fault width is small for strike-slip faults, larger for dip-slip faults in continental regions and much larger for dip-slip faults in regions of lithospheric subduction. For a certain magnitude, fault slip is about the same for strike-slip faults and dip-slip faults in continental regions and smaller for dip-slip faults in regions of lithospheric subduction.

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