“…Among the most prominent examples is the survival of Ar-isotopic microscale disequilibria in polygenetic white mica through metamorphic temperatures exceeding 600°C (Giorgis et al, 2000;Di Vincenzo et al, 2001). The persistence of Rb-Sr biotite signatures in ultramafic rocks through eclogite facies metamorphism (Kühn et al, 2000) and the unaltered preservation of Rb-Sr phengite signatures set at >600°C in eclogites (Glodny et al, 2003(Glodny et al, , 2005 can be explained by modally controlled closed system behaviour (see discussion in Glodny et al, 2003). Shielding is another mechanism that can prevent isotopic systems from being reset even at extreme temperatures (Montel et al, 2000).…”