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Fig. 13 | Geothermal Energy

Fig. 13

From: 3D geophysical inversion modeling of gravity data to test the 3D geologic model of the Bradys geothermal area, Nevada, USA

Fig. 13

Maps of the a observed gravity data, b gravity data calculated for the 3D geologically constrained heterogeneous rock unit, density inversion model, and c the RMS misfit between the two (i.e., misfit = observed − calculated). The majority of the misfit across the model area is near zero (green) and indicates good fit (RMS misfit = 0.55 mGal). Units on the color bars are mGal. Locations of gravity measurements are indicated by black dots

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