Sammanfattning
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.
| Originalspråk | Odefinierat/okänt |
|---|---|
| Sidor (från-till) | 1622–1683 |
| Antal sidor | 62 |
| Tidskrift | International Geology Review |
| Volym | 53 |
| Nummer | 14 |
| DOI | |
| Status | Publicerad - 2011 |
| MoE-publikationstyp | A1 Tidskriftsartikel-refererad |
Nyckelord
- Fennoscandian Shield
- geochemistry
- mantle metasomatism
- Nd-Sr-Hf and U-Pb isotopes
- shoshonitic
- Svecofennian
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