Untitled Document
Dating the allanite-monazite metamorphic reaction
Daniela Rubatto1, Courtney Gregory1, Emilie Janot2 and
Ioan Gabudianu- Radulescu3
1 Research School of Earth Sciences, Australian National University,
Canberra, ACT 0200, Australia
2 Institute of Geological Sciences, University of Bern, Bern, Switzerland
3 Institute for Geography and Geology, Copenhagen, Denmark
Figure 1.
U-Pb geochronology is one of the most widely used methods for the investigation
of the timing of crustal processes. One main limitation of the application
of U-Pb geochronology to metamorphism is the lack of direct links between
the age measured and the conditions at which the dated minerals formed.
In this respect, dating metamorphic reactions that can be placed in pressure-temperature
space is particularly appealing.
One metamorphic reaction between U-Pb minerals that has been widely reported
is the mutual replacement of allanite and monazite (figure 1 and 2).
With the recent set-up of a protocol for accurate dating of allanite
by SHRIMP ion microprobe (Gregory et al. 2007) it has become possible
to date this reaction in-situ. We applied this method to the two geological
settings where allanite-monazite reactions are most commonly documented.
1) Monazite replacing allanite is observed in prograde greenschist to
amphibolite facies metamorphism of metapelites in the Central Alps (Fig.
1). Petrographic observations and thermobarometric calculations allow
placing the reaction at T = 560-580°C, whereas initial allanite formation
occurred at T = 430-450°C. In-situ SHRIMP U-Th-Pb dating of allanite
(31.5 ± 1.3 and 29.2 ± 1.0 Ma) and monazite (18.0 ± 0.3 and 19.1 ± 0.3
Ma) constraints the time elapsed between 430-450°C and 560-580°C, which
implies an average heating rate of 15-8 °C/My (Janots et al., in press).
2) During subduction-related metamorphism, the replacement of monazite
by allanite is associated to increasing pressure. This is observed in
the silvery micaschists of the Gran Paradiso Massif, Western Alps where
microstructural relationships among major and accessory minerals indicate
the following prograde sequence of U-Th bearing accessory minerals: florencite
-> monazite -> allanite (Fig. 2). Thermobarometric calculations
indicate that the allanite-bearing peak assemblage was stable at P =
2.3 ± 0.4 GPa and T = 570 ±30 °C, while monazite formed earlier at pressures
over 2.0 GPa. SHRIMP dating of allanite yielded 34.5 ± 0.8 Ma, interpreted
as the age of the high-pressure metamorphic peak. Prograde monazite yielded
an age of 37.5 ± 0.9 Ma, implying a minimum duration of ~3 Ma for the
Alpine subduction event (Gabudianu Radulescu et al., in press).
Figure 2.
Gregory C, Rubatto D, Allen C, Williams IS, Hermann J, Ireland T (2007)
Allanite micro-geochronology: a LA-ICP-MS and SHRIMP U-Th-Pb study. Chemical
Geology 245:162-182
Janots E, Engi M, Rubatto D, Berger A, Gregory C, Rahn M (in press) Metamorphic
rates in collisional orogeny from in situ allanite and monazite dating.
Geology
Gabudianu Radulescu I, Rubatto D, Gregory C, Compagnoni R (in press)
The age of HP metamorphism in the Gran Paradiso Massif, Western Alps:
a petrological and geochronological study of "silvery micaschists". Lithos