| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9528845 | Ore Geology Reviews | 2005 | 50 Pages |
Abstract
Finally, the large volumes of anorthositic magmas that characterize the Sveconorwegian Orogeny formed a major concentration of Ti in the SW part of the Sveconorwegian orogenic belt under granulite facies conditions, about 40 million years after the last regional deformation of the Sveconorwegian Orogeny, between ca. 930 and 920 Ma.
Related Topics
Physical Sciences and Engineering
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Authors
Pär Weihed, Nicholas Arndt, Kjell Billström, Jean-Clair Duchesne, Pasi Eilu, Olof Martinsson, Heikki Papunen, Raimo Lahtinen,