Fig. 10From: 3D geophysical inversion modeling of gravity data to test the 3D geologic model of the Bradys geothermal area, Nevada, USAPerspective view towards the north of a 3D density model for the Bradys geothermal area that is colored according to model density values derived from homogeneous unit geophysical inversion modeling. Specific density values for each rock unit are shown in Table 1 Back to article page