Non-double-couple (“non-DC”) earthquake mechanisms differ from what is expected for pure shear faulting in a homogeneous, isotropic, elastic medium. Until the mid-1980s, the DC assumption underlay nearly all seismological analysis, and was highly successful in advancing our understanding of tectonic processes and of seismology in general. In recent years, though, many earthquakes have been found that do not fit the DC model. Earthquakes that depart strongly from DC theory range in size over many orders of magnitude and occur in many environments, but are particularly common in volcanic and geothermal areas. Moreover, minor departures from the DC model are detected increasingly frequently in studies using high-quality data. These observation...
A planar seismic source approximates a real fault. In nature, several faults are activated in the vo...
Several reasons for the failure can be proposed: 1. The multidimensional character of seismicity: t...
Many major faults separate two tectonic plates that slowly move past each other in opposite directio...
Historically, most quantitative seismological analysis has been based on the assumption that earthqu...
Abstract. Most studies assume that earthquakes have double-couple (DC) source mechanisms, correspond...
Abstract. Historically, most quantitative seismological analyses have been based on the assumption t...
earthquakes and nearly identically repeating events. Using non-double-couple earthquakes, I aim to b...
Non double couple (NDC) sources are considered in framework of the hypothesis that the process of se...
Earthquakes with anomalous non-double-couple (non-DC) mechanisms have been observed at many geotherm...
Abstract To better understand the connection between earthquake production and geothermal/magmatic s...
We discuss various methods used to investigate the geometric complexity of earthquakes and earthquak...
A large portion of deep earthquakes including intermediate-depth (100~300km in depth) and deep-focus...
Most of 26 small (0.4M3.1) microearthquakes at Long Valley caldera in mid-1997, analyzed using data ...
The occurrence of earthquakes is the mirror of the stress patterns inside the brittle lithosphere. T...
The statistical properties of seismicity are known to be affected by several factors such as the rhe...
A planar seismic source approximates a real fault. In nature, several faults are activated in the vo...
Several reasons for the failure can be proposed: 1. The multidimensional character of seismicity: t...
Many major faults separate two tectonic plates that slowly move past each other in opposite directio...
Historically, most quantitative seismological analysis has been based on the assumption that earthqu...
Abstract. Most studies assume that earthquakes have double-couple (DC) source mechanisms, correspond...
Abstract. Historically, most quantitative seismological analyses have been based on the assumption t...
earthquakes and nearly identically repeating events. Using non-double-couple earthquakes, I aim to b...
Non double couple (NDC) sources are considered in framework of the hypothesis that the process of se...
Earthquakes with anomalous non-double-couple (non-DC) mechanisms have been observed at many geotherm...
Abstract To better understand the connection between earthquake production and geothermal/magmatic s...
We discuss various methods used to investigate the geometric complexity of earthquakes and earthquak...
A large portion of deep earthquakes including intermediate-depth (100~300km in depth) and deep-focus...
Most of 26 small (0.4M3.1) microearthquakes at Long Valley caldera in mid-1997, analyzed using data ...
The occurrence of earthquakes is the mirror of the stress patterns inside the brittle lithosphere. T...
The statistical properties of seismicity are known to be affected by several factors such as the rhe...
A planar seismic source approximates a real fault. In nature, several faults are activated in the vo...
Several reasons for the failure can be proposed: 1. The multidimensional character of seismicity: t...
Many major faults separate two tectonic plates that slowly move past each other in opposite directio...