Hallandian 1.45 Ga high-temperature metamorphism in Baltica: P-T evolution and SIMS U-Pb zircon ages of aluminous gneisses, SW Sweden
The southernmost Baltic Shield exposes polymetamorphic continental crust that was largely formed and accreted during a series of 1.92-1.66 Ga Paleoproterozoic orogenic events and later reworked during the 1.14-0.90 Ga Sveconorwegian orogeny. An intermediate period of metamorphism, deformation and magmatism at 1.47-1.38 Ga has been attributed to the Hallandian orogeny, but due to overprinting by Sv
