Fig. 15


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Tera-Wasserburg diagrams for two samples of hydrothermal rutile hosted in quartz-wolframite-arsenopyrite veins from the Puy-les-Vignes deposit. Weighted mean ages are calculated from linear regression of the discordia line crossing the concordia curve at its lower-age intercept. Error ellipses are quoted at 2σ level of uncertainty. U/Pb isotopic data are reported in Table 2.

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