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On Genesis of Garnet Plagiogranitoids of the Lapland Granulite Belt
Abstract. On the basis of geological, geochemical and petrographic data the comparison of plagiogranitoids of the northern and north-west part of the Lapland Granulite Belt with acid granulites has been carried out. The conclusion of sintectonic intrusion of rocks initial for garnet plagiogranitoids into rocks undergone metamorphism of granulite facies has been made. Petrogeochemical data assume an opportunity of plagiogranitoid substance formation as a result of diatexis from the substratum corresponding to acid granulites by its structure. Presence of granulite facies rocks in the plagiogranitoids assumes two stages of granulite metamorphism which had been broken off in time by a stage of plagiogranitoid intrusion. The data of vibroseismic sounding show loss of stratification in the northern part of the belt connected with palingenesis processes.
Printed reference: Kozlov N.E., Kozlova N.E. On Genesis of Garnet Plagiogranitoids of the Lapland Granulite Belt // Vestnik of MSTU. 1998. V. 1, No 3. P. -.
Electronic reference: Kozlov N.E., Kozlova N.E. On Genesis of Garnet Plagiogranitoids of the Lapland Granulite Belt // Vestnik of MSTU. 1998. V. 1, No 3. P. -. URL: http://vestnik.mstu.edu.ru/v01_3_n03/articles/05_kozl.zip.
(In Russian, p.10, fig. 4, tables 5, ref 15, MS Word 95, WinZip)
