Untitled Document
Behaviour of allanite during incipient partial melting
in the Southern Central Alps
Courtney Gregory1, Daniela Rubatto1, Jöerg Hermann1 and Alfons Berger2
1 Research School of Earth Sciences, Australian
National University, Canberra, ACT 0200, Australia
2 Institute of Geological Sciences, University of Bern, CH-3012 Bern, Switzerland
The chemical and U-Th-Pb isotopic behaviour of accessory allanite during
incipient partial melting was investigated in a field-based study of
upper-amphibolite facies migmatites in the southern Central Alps (Switzerland).
Orthogneiss and leucosome sampled from the core of the migmatite zone
(peak T of ~680-720°C) to its limit (T ~650°C), contained both zircon
and allanite, which permitted a comparison of U-Th-Pb systematics in
these phases.
Allanite found in orthogneiss showed complex internal zoning (see backscatter
electron or BSE image in Fig. 1), suggestive of multi-stage growth. Bright
BSE cores with high La/Lu and Th/U and low Eu/Eu* chemical signatures
yielded Permian ages and thus were inherited from the pre-Alpine magmatic
protolith. In contrast, chemically distinct overgrowths and single grains
gave age populations between 30 ± 1 Ma and 23 ± 1 Ma in line with an
Alpine metamorphic origin. Textural and inclusion relationships with
major melt-formed minerals and their LREE-depletion supports the interpretation
that allanite was an anatectic phase. Further evidence is provided by
comparing magmatic and metamorphic mineral Eu compositions (Fig. 1).
Plagioclase did not impose a negative Eu anomaly on co-existing metamorphic
phases because 80-90 % of the bulk-rock Eu was actually hosted in metamorphic
allanite and titanite. To account for this, it is suggested that metamorphic
allanite and titanite formed during feldspar breakdown, which would have
occurred above the wet solidus for this system (i.e. at T > 650°C).
The inheritance of Permian cores provides first hand evidence for minimal
Pb diffusion in allanite during Alpine partial melting (i.e. ~7 million
years above 650°C). Importantly, in samples where co-existing zircon
had rare or limited metamorphic overgrowths (i.e. at T < 700°C), allanite
was the only accessory mineral chronometer that recorded the Alpine event.
The U-Th-Pb system in allanite therefore presents a solid, complementary
approach for the geochronology of low-temperature (~650-700°C) partial
melt processes in the crust.
Accepting allanite as a melt-product, the youngest U-Th-Pb age obtained
from a discordant leucosome indicates that the Alpine melting regime
lasted over several million years (until 23 Ma) and later than previously
accepted. Combined with previous constraints, the prolonged high temperature
evolution down to 23 Ma requires a subsequent period of fast cooling
(~100 ± 20°C/Ma) for the studied samples.