Zircon demonstrates 1.92 Ga high-T metamorphism in the Trivandrum Block.
Monazites preserve a vestige of this event.
The high-T event is older than some of the basement orthogneisses in the Block.
The overprinting Neoproterozoic-Cambrian granulite was long-lived (45 Myr).
At least some of the paragneisses in the Trivandrum Block are polymetamorphic.