Abstract
Three independent Pb isotope homogenizing processes operating on large volumes of rock material during limited intervals in the Phanerozoic have been used to define a unique evolutionary curve for rock and ore lead isotopic compositions of the southern Massif Central, France. The model is
where xt, yt and zt are the calculated isotopic ratios (206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb respectively) at time t years ago and L1, L2 and L3 are the decay constants of 238U, 235U and 232Th respectively. The model gives the following ages for averages of the three sets of data used in its generation: age of mineralization for carbonate-hosted lead-zinc ore of Les Malines, ca. 150 Ma; emplacement of the Saint-Guiral-Liron granite, ca. 290 Ma; and an estimated average age of a group of Cambrian syngenetic deposits, ca. 520 Ma. These ages are in close agreement with ages determined by independent methods.
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Sinclair, A.J., Macquar, J.C. & Rouvier, H. Re-evaluation of lead isotopic data, southern Massif Central, France. Mineral. Deposita 28, 122–128 (1993). https://doi.org/10.1007/BF00196336
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DOI: https://doi.org/10.1007/BF00196336