Abstract
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.
Original language | Undefined/Unknown |
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Pages (from-to) | 1622–1683 |
Number of pages | 62 |
Journal | International Geology Review |
Volume | 53 |
Issue number | 14 |
DOIs | |
Publication status | Published - 2011 |
MoE publication type | A1 Journal article-refereed |
Keywords
- Fennoscandian Shield
- geochemistry
- mantle metasomatism
- Nd-Sr-Hf and U-Pb isotopes
- shoshonitic
- Svecofennian