Geochemical systematics and U–Pb zircon age of the Vulvara anorthosite massif, Lapland granulite belt, Baltic shield: magmatic sources and metamorphic alteration of the rocks

ABSTRACT

The Vulvara anorthosites occur among the rocks of intermediate composition, in contrast to most Lapland granulite belt (LGB) anorthosites, associated with mafic granulites. The U-Pb, Sm-Nd and REE geochemical data were used to compare Vulvara with other LGB anorthosites. The intrusion of the Vulvara massif occurred in the interval of 2100–1965 Ma. The first metamorphic processing took place 1947 ± 11 Ma ago under granulite facies. Postgranulite transformations occurred 1900–1850 Ma ago under amphibolite facies; earlier (1896 ± 15 Ma) and later (1852 ± 17 Ma, 1846 ± 16 Ma) thermal events were established. The Vulvara anorthosites, in comparison with other LGB anorthosites, are distinguished by a more acidic composition of plagioclase, a higher F number of rocks and mafic minerals, a higher content of SiO₂, Na₂O, K₂O, Ba, Sr, Zr, Nb, Rb, and a lower content of CaO. The Sm-Nd and REE geochemistry suggest that there are three groups of LGB anorthosites, distinguished both by age and magma source.

KEYWORDS:

• Anorthosites
• Lapland granulite belt
• geochemistry of rocks
• U–Pb zircon age

Acknowledgements

The authors remember Academician F.P. Mitrofanov with warmth and gratitude. He considered anorthosites to be one of the most interesting geological objects and did much to study them on the Kola Peninsula. The authors are also grateful to Dr V.V. Balaganskii and Dr D.R. Zozulya for their kind help and to the reviewers for their critical remarks and recommendations. The study was carried out within the framework of the State Assignment for Geological Institute of the KSC RAS (research topic No. 0226-2019-0052).

Disclosure statement

No potential conflict of interest was reported by the author(s).