Figure 5. Geologic map showing the Vodlozero domain [Lobach-Zhuchenko et al., 2002]. 1 - localities with the oldest dated rocks in the domain: KV - mafic volcanites at the Vinela and Cherva rivers, TL - tonalites at the Lairuchei River; GAV - Vodla gneisses and amphibolites; TV - tonalites at the Vyg River; TPL - Palaya Lamba tonalites; 2 - tonalitic gneiss, granitic gneiss, and migmatite, undifferentiated. Greenstone belts: the oldest (3.0-2.92 Ga), 3 - with multimodal volcanism, 4 - with bimodal volcanism; 5 - younger (2.9-2.85 Ga), with bimodal volcanism, 6 - with bimodal volcanism, undated. Numerals indicate greenstone belts: 1 = Hautavaara, 2 = Koikary, 3 = Semchensky, 4 = Palaya Lamba, 5 = Oster, 6 = Shilos, 7 = Kamennye Ozera, 8 = Kenozero. Intrusions: 7 - gabbronorite, gabbro, diorites; 8 - tonolites, trondhjemit; 9 - high-Mg granite; 10 - subalkaline rocks: a, granitods, b, mafic dikes; 11 - granite; 12-granulite facies area with charnockite and enderbite plutons; 13 - boundaries of granulite facies area; 14 - mafites of Matkalachtinskaja zone; 15 - Central-Karelian domen; 16 - Proterozoic rocks; 17 - rapakivi plutons; 18 - Paleozoic rocks.