Peculiarity of ultrametamorphism in the juncture zone of the Aldan shield and Dzhugdzhur-Stanovoi folded area

The processes of ultrametamorphism in the juncture zone between the Aldan shield and Stanovoi folded area are manifested in granitization (volume-for-volume replacement of gneisses by trondhjemite gneisses Lc1) and subsequent migmatization with formation of several leucosome generations Lc2, Lc3, Lc...

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Veröffentlicht in:Geochemistry international 2012-07, Vol.50 (7), p.619-637
Hauptverfasser: Sedova, I. S., Glebovitsky, V. A., Samorukova, L. M.
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Sprache:eng
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