Kinardo Flores Castro, Ramon Vaquer Navarro, C. de las Cuevas Müller, J.M. Grosso García
This study has attempted to establish the temperature of contact metamorphism at the skarn deposit of Villa Juárez. In order to find out consistent temperature values, several specimens of the skarn (wollastonite, calcite and marble) were analyzed by thermogravimetry, gas chromatography and microthermometry of fluid inclusions. The aforementioned techniques have allowed us to estimate the XCO, during the formation of those skarn minerals. The obtained results focus the existence of very low CO, molar fraction (0.02 or even lower) during the formation of the skarn.
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