Publications

Scientific publications

Голубев А.И., Иващенко В.И., Трофимов Н.Н., Кондрашова Н.И., Лавров О.Б.
Рудные формации и металлогенические комплексы Карелии
// Геология и полезные ископаемые Карелии. Вып. 11. Петрозаводск: КарНЦ РАН, 2008. C. 155-176
The associations of some ore and geological formations, revealed by ore-formation analysis of deposits and occurrences in the Karelian region, provide an additional argument in favour of its subdivision into three metallogenic subprovinces (Karelian, Svecofennian and Belomorian) and are used as a basis for differentiating metallogenic complexes responsible for the metallogenic pattern and economic potential of each subprovince. The main metallogenic complexes of the Karelian subprovince are: a Middle Lopian copper-gold volcanogenic and copper-nickel komatiite-andesite-basaltic complex of greenstone belts; a Late Lopian gold-rare-metal plutonogenic-granitic and gold-iron ore jaspilitic complex; a Sumian noble-metal-chromite layered pluton complex; a Svecofennian composite (V, U, Ti, PGM, Au, Cu, Mo) picrite-dolerite-black shale paleorift and diamondiferous kimberlitic plume complex; a Middle Riphean diamondiferous kimberlite-lamproite plume and Vendian noble-metal conglomerate aulacogen complex. The main metallogenic complexes of the Svecofennian subprovince are: a Middle Riphean uranium, aulacogen unconformity zone complex and an Early Riphean rare-metal-tin, tectonomagmatic activation zone complex and a Svecofennian complex (V, Mo, PGM) black shale island-arc complex. The main metallogenic complexes of the Belomorian subprovince are a Svecofennian rare-metal, tectonomagmatic activation zone complex and a Late Lopian gold-chromium-nickel ultramafic plume complex.
Last modified: December 15, 2009