METAMORPHISM OF THE KORVATUNDRA STRUCTURE OF THE LAPLAND-KOLA OROGEN (Arctic Zone of the Fennoscandian Shield)
E.A. Nitkina1, O.A. Belyaev1, D.V. Dolivo-Dobrovol'skii2, N.E. Kozlov1, T.V. Kaulina1, N.E. Kozlova1
1Geological Institute of the Kola Science Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, 184209, Russia
2Institute of Precambrian Geology and Geochronology, nab. Makarova 2, St. Petersburg, 199034, Russia
Keywords: Metamorphism, deformations, P-T conditions, U-Pb, Sm-Nd, Rb-Sr, Korvatundra structure, Arctic zone of the Fennoscandian Shield
Abstract
We study the P - T conditions and age of metamorphic evolution of the rocks that make up the Korvatundra structure in the northeast of the Fennoscandian Shield. The rocks underwent progressive metamorphism of the amphibolite facies at 625-660 ºC and 8.7-8.8 kbar 1945 ± 34 Ma (Sm-Nd data). The pegmatite cutting the metamorphic paragenesis that formed at this stage has an age of 1917 ± 6 Ma (zircon U-Pb data). Metamorphic transformations after 1917 Ma are manifested locally as discrete zones of blastomylonites in the rocks of the northern part and some inner sites of the Korvatundra structure. Both local increases and decreases in temperature and pressure are possible in these zones. The formation of light titanite with an age of 1863 ± 44 Ma marks the next stage of shear strain. Low-temperature alterations (chloritization and silicification) took place in the zones of final deformations 1722 ± 5 Ma (Rb-Sr data). Beginning from 1.94 Ga, the general deformational and metamorphic history of the Korvatundra structure, Lapland Granulite Belt, and Tana Belt confirms the assumption of the formation of a single inverted metamorphic zoning within the Korvatundra structure and the overlying Lapland-Kolvitsa Collision Belt in the Paleoproterozoic. The obtained data supplement the idea of the Paleoproterozoic geodynamic evolution of the Lapland-Kola orogen.
|
