| REMAGNETISATION IN THE ROCKS OF THE EAST EUROPEAN CRATON |
N.V. Lubnina Lomonosov Moscow State University, Moscow, 119991, Leninskiye Gory, Geological Department; lubnina@rambler.ru Distribution of remagnetisation was studied in the NeoArchean-Paleozoic rocks of the East European craton. The paper describes typical stages of remagnetization correlating with the plume events (2.5-2.4 Ga, 2.3-2.1 Ga, 1.27-1.20 Ga, 380-360 Ma, 250-240 Ma), with the collapse and fluid effects during the collision and orogenic events (1,95-1,85 Ga; 1,80-1,70 Ga; 440-380 Ma and 320-280 Ma). |
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