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Fig. 11 | Geothermal Energy

Fig. 11

From: Coda wave interferometry during the heating of deep geothermal reservoir rocks

Fig. 11

Comparison of simulated and laboratory CWI measurements with the time dilatation model. We represent the CWI measurements obtained at the laboratory (orange line) during second heating cycles of Westerly Granite and simulated results (blue line) with volumetric strain. We compare the measurements to those expected from the time dilatation model (black line). A linear regression is fitted the measurements to estimate the slopes

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