Estimating the mechanisms of small (M<4) earthquakes is quite challenging. A common scenario is that neither the available polarity data alone nor the well predictable near-station seismograms alone are sufficient to obtain reliable focal mechanism solutions for weak events. To handle this situation we introduce here a new method that jointly inverts waveforms and polarity data following a probabilistic approach. The procedure called joint waveform and polarity (JOWAPO) inversion maps the posterior probability density of the model parameters and estimates the maximum likelihood double-couple mechanism, the optimal source depth and the scalar seismic moment of the investigated event. The uncertainties of the solution are described by confide...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
We present a new method using high frequency full waveform information to determine the focal mecha...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
Characterizing seismic moment tensors of small‐ to moderate‐magnitude earthquakes (i.e., 2.5<M<4.0) ...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
We present a new method using high frequency full waveform information to determine the focal mecha...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
Characterizing seismic moment tensors of small‐ to moderate‐magnitude earthquakes (i.e., 2.5<M<4.0) ...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The analysis of earthquake focal mechanisms provides information about the stress regime, fault geom...
Rapid stress release at the source of an earthquake produces seismic waves. Observations of the part...
The polarity of the first motion of a seismic signal from an earthquake is an important constraint i...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
Earthquake source inversion is highly dependent on location determination and velocity models. Uncer...
We present a new method using high frequency full waveform information to determine the focal mecha...