Multi-isotope tracing of the 1.3–0.9 Ga evolution of Fennoscandia; crustal growth during the Sveconorwegian orogeny-Reference-Cited by-同舟云学术

Multi-isotope tracing of the 1.3–0.9 Ga evolution of Fennoscandia; crustal growth during the Sveconorwegian orogeny

Published:2021-03 Issue: Volume:91 Page:31-39
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Granseth Anette,Slagstad Trond,Roberts Nick M.W.,Hagen-Peter Graham,Kirkland Christopher L.,Møkkelgjerd Steinar H.H.,Røhr Torkil S.,Coint Nolwenn,Sørensen Bjørn Eske

Funder

Norges Geologiske Undersøkelse

Norges Teknisk-Naturvitenskapelige Universitet

Publisher

Elsevier BV

Subject

Geology

Reference82 articles.

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4. Nature and distribution of deep crustal reservoirs in the southwestern part of the Baltic Shield: evidence from Nd, Sr and Pb isotope data on late Sveconorwegian granites;Andersen;J. Geol. Soc.,2001

5. Crustal evolution in the SW part of the Baltic Shield: the Hf isotope evidence;Andersen;J. Petrol.,2002

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