Conditions of Metamorphism of Rocks of the Kichan Structure in the Archean Tiksheozero Greenstone Belt (Belomorian Region, Fennoscandinavian Shield)

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Metamorphic rocks of the Kichan structure of the Tiksheozero greenstone belt were formed after differentiated volcanic series and represented by gneisses, schists, and amphibolites. Conditions of metamorphism correspond to the high-pressure part of the epidote-amphibolite and amphibolite facies. The Gibbs energy minimization method has shown that mineral assemblages of metabasites (plagioclase + biotite + hornblende + garnet) occupy low- and medium-temperature regions in the P–T diagram (550–720 °C, 3–10 kbar). Metamorphic conditions for assemblages of kyanite-garnet-biotite and garnet + two-mica gneisses correspond to temperature 600–730 °C and pressure 6–8 kbar, which is consistent with petrographic observations. When using multiple mineral equilibria, the best intersections of reaction lines correspond to 640–650 °C, 7.8–8.0 kbar with decreasing to 620–630 °C, 6.2–6.5 kbar if Ti-containing phases and H2O are taken into account. For metabasic mineral assemblages, the calculated water activity is close to 0.6, while for gneisses it reaches 0.9–1.0. According to predecessors, mineral assemblages and texture of the studied rocks were formed during the Proterozoic (1.80–1.76 Ga) stage of metamorphism of Archean volcanics synchronous with the late stages of the formation of the Svecofennian and Lapland-Kola orogens. Supracrustal series of volcanics were presumably formed in marginal-oceanic settings in the transition zone between the Karelian Craton and the Belomorian mobile belt.

作者简介

A. Usoltseva

Saint Petersburg State University, Institute of Earth Sciences

Email: st097637@student.spbu.ru
Saint Petersburg, Russia

T. Myskova

Institute of Precambrian Geology and Geochronology RAS

Saint Petersburg, Russia

S. Baltybaev

Saint Petersburg State University, Institute of Earth Sciences; Institute of Precambrian Geology and Geochronology RAS

Saint Petersburg, Russia

O. Galankina

Institute of Precambrian Geology and Geochronology RAS

Saint Petersburg, Russia

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