Skip to main content
Geothermal Energy

Science – Society – Technology

Figure 7 | Geothermal Energy

Figure 7

From: Characterization of ambient seismic noise near a deep geothermal reservoir and implications for interferometric methods: a case study in northern Alsace, France

Figure 7

Tomographic inversion of the theoretical time shifts induced by the synthetic anisotropic ADNE. Yellow dots correspond to the stations used in the inversion. The ideal model is homogenous with a phase speed of 2.45 km/s (white color). Green/blue (resp. yellow) colors correspond to over-estimated (resp. under-estimated) phase speeds; both causal and acausal time shifts are included in the inverse problem. The black line delimits the resolved zone.

Back to article page