Fig. 11From: Interpretation of gravity–magnetic anomalies to delineate subsurface configuration beneath east geothermal province along the Mahanadi rift basin: a case study of non-volcanic hot springsPlot of one-dimensional equilibrium geotherms as calculated for crust up to 3 km depth for four different mantle heat flow values, and 5 different crustal heat production rates but considering two different crustal thicknesses: a for 34-km-thick crust, and b for 50-km-thick crustBack to article page