scholarly journals Dynamic versus static stress triggering and friction parameters: Inferences from the November 23, 1980, Irpinia earthquake

2000 ◽  
Vol 105 (B9) ◽  
pp. 21647-21659 ◽  
Author(s):  
C. Voisin ◽  
M. Campillo ◽  
I. R. Ionescu ◽  
F. Cotton ◽  
O. Scotti
2016 ◽  
Vol 121 (3) ◽  
pp. 1890-1909 ◽  
Author(s):  
Shyam Nandan ◽  
Guy Ouillon ◽  
Jochen Woessner ◽  
Didier Sornette ◽  
Stefan Wiemer

2015 ◽  
Vol 120 (1) ◽  
pp. 290-307 ◽  
Author(s):  
Maria Kozłowska ◽  
Beata Orlecka-Sikora ◽  
Grzegorz Kwiatek ◽  
Margaret S. Boettcher ◽  
Georg Dresen

2014 ◽  
Vol 597 ◽  
pp. 324-327
Author(s):  
Dong Ning Lei ◽  
Yong Jian Cai ◽  
Heng Li

Some faults rupture the surface followed by coseismic dislocation, which causes space stress changes and transmits or imposes static stress on or to neighboring faults.The static stress triggering leads to the adjacent fault ruptured in advance, which means a Coulomb stress increase and triggers a new earthquake event. In recent two decades, some studies on stress triggering became important field of seismotectonics. The occurrence of both Wenchuan M8.0 earthquake and Japan M9.0 eathquake have arisen interest of many researchers, and obtained much new result and understanding.


2002 ◽  
Vol 15 (3) ◽  
pp. 318-332 ◽  
Author(s):  
Yong-ge Wan ◽  
Zhong-liang Wu ◽  
Gong-wei Zhou ◽  
Jing Huang ◽  
Li-xin Qin

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