Fig. 12From: 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 constrained by the 3D geological model but has variable density within individual rock units. Colors show density variation according to the color bar. Specific density ranges for each rock unit are shown in Table 1. Each panel shows the following rock units: a Mzu, b Mzu + Trt, c Mzu + Trt + Tda, and d Mzu + Trt + Tda + TboBack to article page