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Numerical modeling of fluid effects on seismic properties of fractured magmatic geothermal reservoirs

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Figure

Figure 1. Comparison of natural rock with its conceptual representations. (a) Natural fractured rock with microscopic and macroscopicfractures of complex shape
Figure 3. Typical stratigraphy of the Icelandic crust. Pyroclasticrocks, lava flows, shallow dykes and sills, and intracrustal magmachambers are characterized in our study as potential host rocks forgeothermal reservoirs.
Figure 4. Lithological classification (a), physical properties (b–e) of dry rocks versus dry frame bulk modulus, and hydraulic permeabilityversus bulk density (f), as reported in the literature for low confining pressures
Fig. 4a for the drained bulk modulus, with the boxes indicat-ing the 25th and 75th percentiles, and dots are values outsidethese percentiles.
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