Abstract
Pb isotopic composition and concentrations were determined for whole-rock samples from the Pliocene-Pleistocene, acid, Tuscan Igneous Province, Italy, in order to clarify their relation to the Cenozoic alkaline volcanism of Central Italy. The Pb of the Tuscan rocks is fairly uniform in its isotopic composition, despite variable and high 87Sr/86Sr ratios (0.711–0.725; Barberi et al, 1971).
A comparison of the Pb isotopic composition in the Tuscan and the potassic alkaline rocks strongly suggests a continuous mixing relation between both rock series, with partial melts of mantle material and argillaceous sedimentary rocks as likely end-members. Such an interrelation could also provide a simple explanation for the range in the Sr isotopic ratio within the Tuscan rocks. The favoured model envisages a similar history for both rock-series; it is suggested that their main petrographic differences result from a lower portion of mantle-derived material in the parental material for the Tuscan rocks, and from the mineral phases present in the residue during partial melting of the source region.
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Vollmer, R. Isotopic evidence for genetic relations between acid and alkaline rocks in Italy. Contr. Mineral. and Petrol. 60, 109–118 (1977). https://doi.org/10.1007/BF00372277
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DOI: https://doi.org/10.1007/BF00372277