
Zoisite‐ and clinozoisite‐segregations in metabasites
High‐pressure zoisite‐ and clinozoisite‐bearing segregations are common in garnet‐ and albite‐bearing amphibolites of the Palaeozoic part of the Lower Schieferhülle, south‐central Tauern Window, Austria. The zoisite segregations (primary assemblage: Zo+Qtz+Cal) formed during an early to pre‐Hercynian high‐pressure event (P≫0.6 GPa, T =500–550 °C) by …