Localized distribution of granulite facies rocks in the Bamble lithotectonic domain
U–Pb zircon ages yield magmatic crystallization around 1545 ± 7 and 1542 ± 5 Ma.
U–Pb zircon age of 1139 ± 11 Ma represents robust estimate for the granulite-facies metamorphism.
P–T modeling yields P > 1.15 GPa and T > 850 °C of Grt + Opx ± Cpx + Pl + Bt + Qz-assemblage.
Metamorphism controlled by fluid availability, deformation, composition, P and T gradients