Multistage development of a hydrothermal W deposit during the Variscan late-orogenic evolution: the Puy-les-Vignes breccia pipe (Massif Central, France)

Special Issue Minéralisations périgranitiques

Open Access

Fig. 15

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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