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Fig. 11 | Geothermal Energy

Fig. 11

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

Fig. 11

Maps of the a observed gravity data, b gravity data calculated for the 3D geologically constrained homogeneous rock unit, density inversion model, and c the misfit between the two (i.e., misfit = observed − calculated). The RMS misfit across the model area is characterized by large areas of zero (green) and non-zero (i.e., not green) misfit (RMS misfit = 1.04 mGal). The misfit is an improvement over that shown in Fig. 9. Units on the color bars are mGal. Locations of gravity measurements are indicated by black dots

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