P–T evolution of Precambrian eclogite in the Sveconorwegian orogen, SW Sweden
Conditions of the prograde, peak-pressure and part of the decompressional P–T path of two Precambrian eclogites in the eastern Sveconorwegian orogen have been determined using the pseudosection approach. Cores of garnet from a Fe–Ti-rich eclogite record a first prograde and syn-deformational stage along a Barrovian gradient from ~670 °C and 7 kbar to 710 °C and 8.5 kbar. Garnet rims grew during fu
