Evolution and major features of the Early Precambrian crust of the East European craton

Authors
Mints M.V. 1 , Dokukina K.A. 1 , Konilov A.N. 1 , Philippova I.B. 1 , Zlobin V.L. 1 , Babayants P.S. 1 , Belousova E.A. 1 , Blokh Y.I. 1 , Bogina M.M. 1 , Bush W.A. 1 , Dokukin P.A. 1 , Kaulina T.V. 1 , Natapov L.M. 1 , Piip V.B. 1 , Stupak V.M. 1 , Suleimanov A.K. 1 , Trusov A.A. 1 , Van K.V. 1 , Zamozhniaya N.G. 1
Collection of articles
East European Craton: Early Precambrian History and 3D Models of Deep Crustal Structure
Language
English
Pages
333-354
State
Published
Volume
510
Year
2015
Organizations
  • 1 Peoples Friendship University of Russia
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GRANULITE-GNEISS BELT: A SPECIAL TYPE OF TECTONIC STRUCTURE, THE UNIQUENESS OF WHICH IS NOT LIMITED TO HIGH-GRADE METAMORPHISM

Article
Mints M.V., Dokukina K.A., Konilov A.N., Philippova I.B., Zlobin V.L., Babayants P.S., Belousova E.A., Blokh Y.I., Bogina M.M., Bush W.A., Dokukin P.A., Kaulina T.V., Natapov L.M., Piip V.B., Stupak V.M., Suleimanov A.K., Trusov A.A., Van K.V., Zamozhniaya N.G.
East European Craton: Early Precambrian History and 3D Models of Deep Crustal Structure. Vol. 510. 2015. P.. 329-332