Granulite-gneiss belt: A special type of tectonic structure, the uniqueness of which is not limited to high-grade metamorphism

Авторы
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
Язык
English
Страницы
329-332
Статус
Published
Том
510
Год
2015
Организации
  • 1 Peoples Friendship University of Russia
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Другие записи

SPECIFICS OF THE ECLOGITE-FACIES METAMORPHISM IN THE PRECAMBRIAN

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. Том 510. 2015. С. 323-328