Localized occurrences of granulite: P-T modeling, U-Pb geochronology and distribution of early-Sveconorwegian high-grade metamorphism in Bamble, South Norway
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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

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