Garnet trace element systematics in an amphibolite- to granulite-facies metapelitic sequence (Ivrea-Verbano Zone, Italy)
Abstract This study examines the systematic changes in two-dimensional trace element distributions in garnet from metapelites of the Kinzigite Formation (Ivrea-Verbano Zone, north-west Italy) across a continuous metamorphic field gradient from 0.4 to 0.6 GPa, ~ 650–700 °C to 1.0 GPa, ~ 900 °C, plus a garnet formed at ~...
Ankan Bhattacharyya, Daniela Rubatto, Jörg Hermann
· Contributions to Mineralogy... · 0 citations