Fig. 4From: Pore-fluid-dependent controls of matrix and bulk thermal conductivity of mineralogically heterogeneous sandstonesa Comparison of calculated matrix thermal conductivities (λm) from bulk rock measurements under air-saturated versus water-saturated conditions. b Comparison of calculated matrix thermal conductivities (λm) from mineralogical composition data (RVA) versus λm calculations from bulk rock measurements (λb) under air-saturated and water-saturated conditionsBack to article page