Analysis of shear wave splitting anisotropy in the Tres Virgenes Volcanic Complex, Baja California Sur, Mexico

•The birefringence parameters are due to anisotropic systems, which vary azimuthally.•Anisotropy is strongly controlled by the fault systems.•Most of the NW-SE fast polarizations follow the opening direction of the Gulf of California. We analyze the seismicity that occurred in the Tres Vírgenes Volc...

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Veröffentlicht in:	Geothermics 2021-07, Vol.94, p.102115, Article 102115
Hauptverfasser:	Chacón-Hernández, F., Zúñiga, F.R., Campos-Enríquez, J.O., Lermo-Samaniego, J., Jiménez-Méndez, N.
Format:	Artikel
Sprache:	eng
Schlagworte:	Anisotropy Birefringence Delay time Ductile-brittle transition Earthquakes Fault lines Fluid flow fractures Geological faults Geothermal power Parameters Polarization Reservoirs S waves Seismic activity Seismicity Shear shear wave splitting Splitting Stations statistical tests Tres Virgenes geothermal field Volcanic activity
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