2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 304-4
Presentation Time: 9:00 AM-6:30 PM

THE EFFECT OF TRAPPED CRYSTALLIZING MELTS ON RUTILE AND CONSEQUENCES FOR ZR-IN-RUTILE THERMOMETRY


GALSTER, Federico, Institute of Earth Sciences, University of Lausanne, Lausanne, 1015, Switzerland; Department of Geological Sciences, University of Texas, Austin, TX 78712-1722 and MÜNTENER, Othmar, Institute of Earth Sciences, University of Lausanne, Lausanne, 1015, Switzerland, federico.galster@unil.ch

Zr-in-Rutile thermometry in granulitic terranes results in a large set of calculated temperatures and is of difficult interpretation.

We report an example of corundum and quartz bearing UHT granulite highly depleted in H2O, SiO2, K2O and LILE supporting the decoupling of the rock in isolated microdomains during cooling from ~950 to ~650°C.

Corundum and quartz coexist in single thin sections but occur in texturally different domains: corundum is observed in grt + pl + spl + rt domains interpreted as the highly depleted counterpart, while quartz occurs in pl + rt ± kfs domains interpreted as crystallized trapped melts.

We recognize three groups of rutile: 1) pro-grade rutile preserving peak temperatures; 2) retro-grade rutile and 3) pro-grade rutile re-equilibrated during cooling.

1- In restitic domains we observe texturally homogeneous rutile (with minor inclusions) and rutiles with a net of oriented needles of Zr-rich phases; mineral inclusions (e.g. qtz + sil + zrn) and Zr-in-Rutile temperatures (comprised systematically between ~950°C and ~1050°C) support a pro-grade growth of rutile and UHT metamorphism respectively.

2- Crystallized melts are rich in homogeneous rutile with Zr-in-Rutile temperatures comprised between ~650 and ~950°C and chemically different (Zr vs Zr/Hf; Cr vs Nb; Nb, Ta, Nb/Ta, W and U) from rutiles observed in the restitic domains, these are interpreted as post-peak rutiles.

3- Exclusively at the intersection between crystallized melts and restitic domains it is possible to observe homogeneous rutiles with “low” Zr-in-Rutile temperatures (850-650°C) and surrounded by a thin rim of microzircons; these rutiles have inclusions and chemistry compatible with pro-grade rutiles in restitic domains and are interpreted as pro-grade rutiles re-equilibrated (in terms of Zr content) during cooling.

These observations highlight the importance of presence/absence of fluids during cooling for the preservation/re-equilibration of Zr content in rutile and provide a key for the interpretation of Zr-in-Rutile thermometry in granulites. In fact similar differences in rutile texture and chemistry are observed in less depleted granulites without, however, the clear spatial distribution observed in our sample.