Sm-Nd, Pb-Pb and U-Pb isotopic results are presented for samples from the Pilgujrvi Suite of the Pechenga Series. Whole rock samples and clinopyroxenes of ferropicritic volcanics yield a Sm-Nd isochron age of 1990 + 66 Ma with e Nd + 1.6 + 0.4. This age is also supported by the Pb-Pb data on ferropicrites, although the Pb isotopic system was partly disturbed by secondary processes. One 90% concordant U-Pb zircon analysis from a felsic metasediment indicates a minimum age of 1970 Ma for the deposition.
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Hanski et al. (1990) studied this question.
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