Zobrazeno 1 - 3
of 3
pro vyhledávání: '"гнейс"'
Autor:
A. M. Sazonov, K. A. Zablotsky, U. . Linnemann, E. A. Zvyagina, N. A. Nekrasova, E. A. Naumov, S. A. Sil′yanov
Publikováno v:
Литосфера, Vol 0, Iss 2, Pp 49-59 (2017)
The paper provides justification of Paleo Archaean age (3221 ± 15 Ma) of the granulite plutonic metamorphism that formed the Kan metamorphic complex of the Archaean crust in the Angara-Kan block of the Siberian craton. The age was defined on the bas
Externí odkaz:
https://doaj.org/article/7967dfa2332245b3ac9fab8d02f91a7b
Autor:
E. A. Naumov, K. A. Zablotsky, N.A. Nekrasova, S.A. Sil’yanov, E. A. Zvyagina, U. Linnemann, A. M. Sazonov
Publikováno v:
Литосфера, Vol 0, Iss 2, Pp 49-59 (2017)
The paper provides justification of Paleo Archaean age (3221 ± 15 Ma) of the granulite plutonic metamorphism that formed the Kan metamorphic complex of the Archaean crust in the Angara-Kan block of the Siberian craton. The age was defined on the bas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d1375e3df5fbc76d67751e7aea2b6488
https://doi.org/10.24930/1681-9004-2017-2-049-059
https://doi.org/10.24930/1681-9004-2017-2-049-059
Publikováno v:
Geological Journal; № 4 (2014); ст. 91-102
Геологический журнал; № 4 (2014); ст. 91-102
Геологічний журнал; № 4 (2014); ст. 91-102
Геологический журнал; № 4 (2014); ст. 91-102
Геологічний журнал; № 4 (2014); ст. 91-102
The late paleoarhean (3297±22 Ma) age of tonalite gneisses was at first identified on West-Azov block. They are characterized by a positive value of εNd(3300) = 0,3÷1,8, that they are juvenile source. With the new geochronological data, in the wes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::368e0765b488417726ecf02dca327554
http://geojournal.igs-nas.org.ua/article/view/139191
http://geojournal.igs-nas.org.ua/article/view/139191