Add to ORKGThe rule of dynamic strain to near source aftershock distribution of the 2014, Mw 6.0, Napa (California) earthquak
A technique for the calculation of strain changes in a two-dimensional elastic body with arbitrary i...
Abstract Båth’s law states that the differences in magnitudes between mainshocks and their largest ...
We compare the source time functions (i.e., moment release rates) of three large California mainshoc...
The rule of dynamic strain to near source aftershock distribution of the 2014, Mw 6.0, Napa (Califor...
The occurrence of the Mw 6.0 South Napa California earthquake, on 24 August 2014 at 03:20 a.m. local...
International audienceAftershocks rates seem to follow a power law decay, but the question of the af...
Three studies of site amplification factors, based on the recorded aftershocks, and one study based ...
After a strong earthquake, the possibility of the occurrence of either significant aftershocks or an...
Applying a simple general procedure for identifying aftershocks, we inves- tigate their statistical ...
International audienceTwo of the long-standing relationships of statistical seismology are power law...
Earthquakes can be triggered by other earthquakes. This can be due to local stress field changes by ...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
International audienceWe calculate stress changes resulting from the M = 6.0 West Napa earthquake on...
Large dynamic strains carried by seismic waves are known to trigger seismicity far from their source...
Large earthquakes are followed by a decaying number of smaller earthquakes, called aftershocks, whic...
A technique for the calculation of strain changes in a two-dimensional elastic body with arbitrary i...
Abstract Båth’s law states that the differences in magnitudes between mainshocks and their largest ...
We compare the source time functions (i.e., moment release rates) of three large California mainshoc...
The rule of dynamic strain to near source aftershock distribution of the 2014, Mw 6.0, Napa (Califor...
The occurrence of the Mw 6.0 South Napa California earthquake, on 24 August 2014 at 03:20 a.m. local...
International audienceAftershocks rates seem to follow a power law decay, but the question of the af...
Three studies of site amplification factors, based on the recorded aftershocks, and one study based ...
After a strong earthquake, the possibility of the occurrence of either significant aftershocks or an...
Applying a simple general procedure for identifying aftershocks, we inves- tigate their statistical ...
International audienceTwo of the long-standing relationships of statistical seismology are power law...
Earthquakes can be triggered by other earthquakes. This can be due to local stress field changes by ...
Abstract The potential locations of aftershocks, which can be large and damag-ing, are often forecas...
International audienceWe calculate stress changes resulting from the M = 6.0 West Napa earthquake on...
Large dynamic strains carried by seismic waves are known to trigger seismicity far from their source...
Large earthquakes are followed by a decaying number of smaller earthquakes, called aftershocks, whic...
A technique for the calculation of strain changes in a two-dimensional elastic body with arbitrary i...
Abstract Båth’s law states that the differences in magnitudes between mainshocks and their largest ...
We compare the source time functions (i.e., moment release rates) of three large California mainshoc...
