APATITE AS A MONITOR OF VOLATILE ACTIVITY IN METAMORPHISM: THE HP/UHT BARRO-ALTO COMPLEX, GOIAS, BRAZIL AS AN EXAMPLE
Apatite is ubiquitous in metamorphic rocks. It has been used to infer a variety of intensive/extensive properties including composition of metamorphic fluids, as a measure of distance from intrusions in contact environments, and to document the ingress of hydrothermal fluids. In spite of these varied uses, there are no data that relate Ap chemistry to metamorphic grade for a series of rocks of similar lithology over a wide range of P-T conditions. Here we report initial results of a study aimed in part to document this relationship, which has the potential to record changes in relation to the volatile phase during metamorphism.
The Barro Alto complex (BA) is
one of a group of three layered mafic-ultramafic complexes that make up part of
the Neoproterozoic Brasilia Belt. The BA was metamorphosed to high-pressure (~
8 kbar) and ultra-high temperature (>980oC) during the Brasiliano
Orogeny [Moraes & Fuck, 2000], with metamorphic grade decreasing through
the BA and into the amphibolite facies volcano-sedimentary Juscelândia Sequence
to the NW. Within the upper layered series of the BA, with increasing
metamorphic grade, F in Ap increases (0.49 -> 0.95 pfu; all analyses by
EPMA), whereas Cl (0.013 -> b.d.) and OH (0.42 -> 0.05; calc.) both
decrease. Similarly, Fe, Mn, Sr, S and Y decrease, whereas Si increases, with
metamorphic grade. Cathodoluminescence reveals zoning with discrete cores in
some Ap, but the chemical origin of the zoning is not within the sensitivity of
the EPMA; a second kind of zoning is present in Ap, and consists of
increases in F, Fe, S and Sr toward grain edges, with concomitant decreases in
Cl, Y and Mg, but these trends may be contradictory. Where Ap is present as
inclusions in Grt, it has elevated F, OH, Fe, Sr and Si relative to matrix Ap.
In migmatite, Ap in melanosome has higher F (0.64 vs. 0.49 pfu), and lower Cl
(0.010 vs. 0.016) and OH (0.36 vs. 0.49). The trends in halogen concentrations
in Ap (increase in F/Cl and F/OH, in conjunction with a decrease in Cl/OH)
suggest: 1) Ap growth in the presence of a volatile undersaturated environment,
followed by a volatile saturated environment, 2) down temperature
crystallization of Ap (with Cl and F in a constant concentration reservoir), 3)
changing stability of other halogen-bearing phases (e.g. Bt or Hb) during the prograde/retrograde
path, or 4) influx of volatiles from an external source.