1.8 Ga magmatism in southern Finland: strongly enriched mantle and juvenile crustal sources in a post-collisional setting

The similar to 1.8 Ga post-kinematic intrusions were emplaced within the SSAC subsequent to the continental collision with the Volgo-Sarmatia craton from the SE, during a shift from contraction to extension, that is, in a post-collisional setting.

Bibliographic Details
Published in:	International Geology Review
Main Authors:	Rutanen, Henrikki, Andersson, Ulf B., Väisänen, Markku, Johansson, Åke, Fröjdö, Sören, Lahaye, Yann, Eklund, Olav
Format:	Article in Journal/Newspaper
Language:	unknown
Published:	2011
Subjects:	Fennoscandian Shield geochemistry mantle metasomatism Nd-Sr-Hf and U-Pb isotopes shoshonitic Svecofennian Fennoscandian
Online Access:	https://research.abo.fi/en/publications/9e0b7028-f1a0-482c-a3e2-021986327aaa https://doi.org/10.1080/00206814.2010.496241

Description
Summary:	The similar to 1.8 Ga post-kinematic intrusions were emplaced within the SSAC subsequent to the continental collision with the Volgo-Sarmatia craton from the SE, during a shift from contraction to extension, that is, in a post-collisional setting.