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.
|Number of pages||62|
|Journal||International Geology Review|
|Publication status||Published - 2011|
|MoE publication type||A1 Journal article-refereed|
- Fennoscandian Shield
- mantle metasomatism
- Nd-Sr-Hf and U-Pb isotopes