Figure F24. Crossplot of Site 1195 porosity and thermal conductivity. Superimposed are the power law curves, constructed from the observed range in porosity, for ideal end-member sedimentary facies: sandstones (red/upper curve), limestones (blue/center curve) and shales (black/lower curve). The observed thermal conductivity values lay between the shale and sandstone curves, and given the large carbonate content of the sedimentary section, suggests that much of the sediment at Site 1195 represents a mixing of clay and sandstone with carbonates.

Figure F24. Crossplot of Site 1195 porosity and thermal conductivity. Superimposed are the power law curves, constructed from the observed range in porosity, for ideal end-member sedimentary facies: sandstones (red/upper curve), limestones (blue/center curve) and shales (black/lower curve). The observed thermal conductivity values lay between the shale and sandstone curves, and given the large carbonate content of the sedimentary section, suggests that much of the sediment at Site 1195 represents a mixing of clay and sandstone with carbonates.