Abstract
We have revisited and re-interpreted deformation structures in the classical ore province of west Bergslagen, part of the ∼1.9-1.8Ga old Svecofennian orogen in south-central Sweden. Four successive phases and styles of deformation reflect (1) continental rifting associated with bimodal magmatism in continental back-arc basins (D
Original language | English |
---|---|
Pages (from-to) | 95-119 |
Journal | Precambrian Research |
Issue number | 216-219 |
DOIs | |
Publication status | Published - 2012 |