Fig. 10From: Validation of Play Fairway Analysis of the geothermal potential of Camas Prairie, south-central Idaho, by an exploration wellMulticomponent geothermometric temperature estimate (~ 115 °C). Mineral assemblage consists of calcite, chalcedony, K-clinoptilolite, K-feldspar, fluorite, laumontite, and illite (used to swap for Mg and not shown in the diagram)Back to article page