T167 Metamorphic Petrology: New Approaches and Outcomes

Monday, 2 November 2015
1:30 PM - 5:30 PM
Room 317

DECODING MULTIPLE HIGH-TEMPERATURE METAMORPHIC EVENTS USING PHASE EQUILIBRIA MODELLING, LU–HF GARNET GEOCHRONOLOGY AND IN SITU U–PB MONAZITE GEOCHRONOLOGY

Paper number: T167-16
Program: Technical Sessions
Time: 5:15 PM – 5:30 PM

Authors

Abstract

Migmatitic paragneiss and orthogneiss from the Fosdick migmatite–granite complex in West Antarctica record two metamorphic events: one in the Devonian–Carboniferous and the other in the Cretaceous. SHRIMP U–Pb monazite ages define two dominant populations at 365–300 Ma (from cores of polychronic grains) and 120–96 Ma (from rims of polychronic grains and from monochronic grains). For five paragneisses and two orthogneisses, Lu–Hf garnet ages range from 116 to 111 Ma, c. 12–17 Myr older than Sm–Nd garnet ages of 102–99 Ma from three of the same samples.

LA–ICP–MS analysis shows that garnet grains have Lu-enriched rims relative to Lu-depleted cores. By contrast, garnet grains generally have flat Sm concentrations consistent with high-temperature diffusive resetting. Lutetium enrichment of garnet rims is interpreted to record the breakdown of a Lu-rich accessory mineral such as apatite or monazite during the final stage of garnet growth immediately prior to the metamorphic peak. Alternatively, the Lu-enriched rims may reflect the preferential retention of Lu in garnet during breakdown to cordierite in the presence of melt concomitant with the initial stages of exhumation. Therefore, garnet is interpreted to be part of the Cretaceous mineral paragenesis and the Lu–Hf garnet ages are interpreted to record the timing of close-to-peak metamorphism for this event.

For the Devonian–Carboniferous event, phase equilibria modelling of the metasedimentary protoliths to the paragneiss and a diatexite migmatite restrict the peak P–T conditions to 720–800°C at 0.45–1.0 GPa. For the Cretaceous event, using both forward and inverse phase equilibria modelling of residual paragneiss and orthogneiss compositions, the P–T conditions after decompression are estimated to have been 850–880°C at 0.65–0.80 GPa. These P–T conditions occurred between c. 106 and c. 96 Ma, determined from Y-enriched rims on monazite that record the timing of garnet and biotite breakdown to cordierite in the presence of melt. The effects of this younger metamorphic event are dominant throughout the Fosdick complex.