earthquake. Many authors have proposed that the Landers earthquake directly stressed the Hector Mine fault. Our model of the Landers aftershock sequence, however, suggests there is an 85 % chance that the Hector Mine hypocenter was actually triggered by a chain of smaller earthquakes that was initiated by the Landers main shock. We perform our model simulations using the Monte Carlo method based on the Gutenberg-Richter relationship, Omori’s law, Båth’s law, and assumptions that all earthquakes, including aftershocks, are capable of producing aftershocks and that aftershocks produce their own aftershocks at the same rate that other earthquakes do. In general, our simulations show that if it has been more than several days since an M 7 mai...
We have constructed a model for the occurrence of aftershocks and aftershock sequences. The aftersho...
Studies of many large strike-slip earthquakes have shown that the seismicity rate increases in quadr...
Aftershocks are the most striking evidence of earthquake interactions and the physical mechanisms at...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
Abstract The observed seismicity rate increase after large earthquakes in sites that are located sev...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
[1] Triggered earthquakes can be large, damaging, and lethal as evidenced by the1999 shocks in Turke...
Coseismic stress changes have been the primary physical principle used to explain aftershocks and tr...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
Coseismic stress changes have been the primary physical principle used to explain aftershocks and tr...
tion; 7209 Seismology: Earthquake dynamics and mechanics; KEYWORDS: aftershocks, foreshocks, Hector...
Large earthquakes are followed by a decaying number of smaller earthquakes, called aftershocks, whic...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
[1] The November 2000 New Ireland earthquake sequence started with a Mw = 8.0 left-lateral main shoc...
We have constructed a model for the occurrence of aftershocks and aftershock sequences. The aftersho...
Studies of many large strike-slip earthquakes have shown that the seismicity rate increases in quadr...
Aftershocks are the most striking evidence of earthquake interactions and the physical mechanisms at...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
Abstract The observed seismicity rate increase after large earthquakes in sites that are located sev...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
[1] Triggered earthquakes can be large, damaging, and lethal as evidenced by the1999 shocks in Turke...
Coseismic stress changes have been the primary physical principle used to explain aftershocks and tr...
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftersho...
Coseismic stress changes have been the primary physical principle used to explain aftershocks and tr...
tion; 7209 Seismology: Earthquake dynamics and mechanics; KEYWORDS: aftershocks, foreshocks, Hector...
Large earthquakes are followed by a decaying number of smaller earthquakes, called aftershocks, whic...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
[1] The November 2000 New Ireland earthquake sequence started with a Mw = 8.0 left-lateral main shoc...
We have constructed a model for the occurrence of aftershocks and aftershock sequences. The aftersho...
Studies of many large strike-slip earthquakes have shown that the seismicity rate increases in quadr...
Aftershocks are the most striking evidence of earthquake interactions and the physical mechanisms at...