International audienceThe purpose of this article is to address the problem of the focal mechanism determination using few seismological records acquired by a sparse network of 3-component sensors. Such cases are frequently encountered in reservoir contexts for the monitoring of the fluid-induced microseismicity. Focal mechanisms of fluid-induced earthquakes are characterized by a non-double-couple part. However, we show and discuss that the double-couple moment tensor approximation is valid as a source model. Then, we propose a nonlinear inversion method of the direct P-, SV- and SH-wave amplitudes, based on a simulated annealing algorithm to determine double-couple focal mechanisms. Simultaneously, we determine the associated uncertainty....
We present a new method using high frequency full waveform information to determine the focal mecha...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...
International audienceThe purpose of this article is to address the problem of the focal mechanism d...
International audienceWe have developed a method that enables computing double-couple focal mechanis...
International audienceWe have developed a method that enables computing double-couple focal mechanis...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
International audienceWe propose an inversion method of the direct wave amplitudes P, SV, and SH to ...
Abstract We propose an inversion method of the direct wave amplitudes P, SV, and SH to determine the...
Nous proposons une méthode d inversion non linéaire des amplitudes des ondes directes P, SV et SH ba...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
We present a new method using high frequency full waveform information to determine the focal mecha...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...
International audienceThe purpose of this article is to address the problem of the focal mechanism d...
International audienceWe have developed a method that enables computing double-couple focal mechanis...
International audienceWe have developed a method that enables computing double-couple focal mechanis...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
We develop a non linear inversion method based on the simulated annealing and using the amplitudes o...
International audienceWe propose an inversion method of the direct wave amplitudes P, SV, and SH to ...
Abstract We propose an inversion method of the direct wave amplitudes P, SV, and SH to determine the...
Nous proposons une méthode d inversion non linéaire des amplitudes des ondes directes P, SV et SH ba...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
In this research, we use high frequency waveform information to determine the focal mechanisms of sm...
We present a new method using high frequency full waveform information to determine the focal mecha...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...
Improving the knowledge of seismogenic faults requires the integration of geological, seismological,...