See more from this Division: Topical Sessions
See more from this Session: Strengthening Links between Metamorphic Conditions and Time: New Advances in High-Temperature Geochronology and Tracing P-T-t Paths of Metamorphic Terranes
Abstract:
Sm-Nd whole rock isotope data of garnet lherzolite yields εNd(0) = -8.8, indicating that the Sm-Nd isotope system is strongly decoupled from the Re-Os and Lu-Hf systems. Although melt extraction would result in correlated depletions in Sm/Nd, Lu/Hf, and Re/Os ratios, the Sm-Nd systematics have been subsequently modified in a way that left the Lu-Hf and Re-Os systems unaffected. Sm-Nd isotope systematics of olivine-garnet pyroxenite and garnet periditite as well as the associated garnet lherzolite indicate that these rocks were metasomatized by LREE-rich fluids during the Sveconorwegian orogeny at 1149 ± 11 Ma [2]. On the basis of a Sm-Nd isochron age of low-pressure kelyphitic rims on garnet, emplacement of these mantle rocks into the crust likely started with Late Proterozoic (~600 Ma) rifting and was complete by the Scandian phase of the Caledonian orogeny (~400 Ma).
[1] Beyer et al. (2004) Geology, 32, 609-612. [2] Lapen et al. (2005) CMP 150, 131-145.
See more from this Division: Topical Sessions
See more from this Session: Strengthening Links between Metamorphic Conditions and Time: New Advances in High-Temperature Geochronology and Tracing P-T-t Paths of Metamorphic Terranes