• Fe-Ti rich aggregates occur in rodingites from the Western Carpathians • The aggregates consist of ilmenite, rutile, titanite and calcite • Rutile formed by retrograde breakdown of titanite • Crystallization age of rutile is 102.6 ±... more
• Fe-Ti rich aggregates occur in rodingites from the Western Carpathians • The aggregates consist of ilmenite, rutile, titanite and calcite • Rutile formed by retrograde breakdown of titanite • Crystallization age of rutile is 102.6 ± 19.9 Ma, consistent with Alpine metamorphism • Rodingitization took place during exhumation and cooling of an accretionary wedge
