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 |
|---|---|
| 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