DATA REPOSITORY ITEM: METAMORPHIC-AGE DATA AND TEXTURES

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Berman et al. - page 1 DATA REPOSITORY ITEM: METAMORPHIC-AGE DATA AND TEXTURES This data repository contains details of pressure (P) - temperature (T) and age methods and data (Tables DR1, DR2, DR3). Figures DR1 DR5 illustrate representative textural relationships. Additional descriptive material is given by Berman et al. (2002a) for sample # 3 and by Berman et al. (2002b) for samples # 14 and 15. Thermobarometric methods Selected mineral compositions for pressure (P) temperature (T) estimates were determined using a Cameca SX-50 electron microprobe located at Geological Survey of Canada (Ottawa), employing four spectrometers, a range of natural and synthetic standards, and matrix corrections after Pouchou and Pichoir (1985). Analytical conditions for all phases were 20 kv accelerating voltage, with a 10 na beam current. A 10 µm beam spot was used for feldspars and a more focused beam (~3 µm) for all other minerals. Pressure-temperature estimates were obtained using the TWEEQU software (Berman 1991; http://gsc.nrcan.gc.ca/sw/twq_e.php) with its version 1.02 database. U-Pb SHRIMP analytical methods U-Pb analyses of monazite were performed in situ with selected targets cored (3 mmdiameter) from thin sections and mounted in epoxy together with pre-polished laboratory standard monazites (GSC monazite z3345; 207 Pb/ 206 Pb TIMS age = 1821.0 ± 0.6 Ma (2s); GSC monazite z2908, 207 Pb/ 206 Pb TIMS age = 1795 ± 2 Ma (2 s); Stern and Berman (2000). Details of these procedures are given by Rayner and Stern (2002), and analytical protocols for monazite are described in detail by Stern and Sanborn (1998) and Stern and Berman (2000). Analyses were conducted using an O 2- primary beam, with a spot sizes between 7 and 15 µm. Ten masses were sequentially measured over 7 scans with a single electron multiplier and a pulse counting system with deadtime of 24 ns. Moderate energy filtering was used to minimize a known isobar at mass 204. Off-line data processing was accomplished using customized in-house software (Stern, 1997). Pb/U ratios were calibrated with GSC monazite standard z3345. Since all the analyses in this study were concordant to slightly discordant, ages are based on weighted mean 207 Pb/ 206 Pb of individual analyses. Age estimates and error calculations were calculated using Isoplot/Ex version 2.2 (Ludwig, 2002).

Berman et al. - page 2 REFERENCES Berman, R.G., 1991, Thermbarometry using multiequilibrium calculations: a new technique with petrological applications: Canadian Mineralogist, v. 29, p. 833-856. Berman, R., Davis, W.J., Aspler, L., and Chiarenzelli, 2002a, SHRIMP U/Pb ages of multiple metamorphic events in the Angikuni Lake area, western Churchill Province, Nunavut: Current Research of the Geological Survey of Canada, v. 2002-F3, p. 1-9. Berman, R.G., Davis, W.J., Ryan, J.J., and Tella, S., 2002b, In-situ U/Pb SHRIMP geochronology of Barrovian facies-series metasedimentary rocks in the Happy lake and Josephine River supracrustal belts: implications for the Paleoproterozoic architecture of the northern Hearne domain, Nunavut: Current Research Geological Survey of Canada, v. 2002-F4, p. 1-14. Holland, T.J.B., and Blundy, J.D., 1994, Non-ideal interactions in calcic amphiboles and their bearing on amphibole-plagioclase thermometry: Contributions to Mineralogy and Petrology, v. 116, p. 433-447. Kretz, R., 1983, Symbols for rock-forming minerals: The American Mineralogist, v. 68, p. 277-279. Ludwig, K.R., 2002, Isoplot/Ex, version 2.2, A geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication No. 1a, 53p. Pouchou, J.L., Pichoir, F., 1985, PAP correction procedure for improved microanalysis. In: J.T. Armstrong (Ed.), Microbeam Analysis. San Francisco Press, San Francisco, pp. 104-106. Rayner, N. M., Stern, R.A., 2002, Improved Sample Preparation Method for SHRIMP Analysis of Delicate Mineral Grains Exposed in Thin Sections. Current Research, Geological Survey of Canada, Paper 2002-F10. Stern, R.A., 1997, The GSC sensitive high resolution ion microprobe (SHRIMP): analytical techniques of zircon U-Th-Pb age determinations and performance evaluation. In. Radiogenic Age and Isotopic Studies: Report 10. Geological Survey of Canada, Current Research 1997-F, pp. 1-31. Stern, R.A., Berman, R.G., 2000, Monazite U-Pb and Th-Pb geochronology by ion microprobe, with an application to in situ dating of an Archean metasedimentary rock. Chemical Geology, v. 172, 113 130.

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Berman et al. page 7 #14 2 mm #15 a S 1 St S 2 Grt St St 1 mm Figure DR1. SEM images of porphyroblast-fabric relationships in samples 14 and 15: (a) S2 is axial planar to folded S1 fabric that is included in syn-s2 staurolite and garnet (b) S2-parallel kyanite and elongate garnet, indicating syn-s2 growth b Qz Qz Grt S2 Ky 0.30 a Grt A Grt B Grt C #15.95 0.20 Fe/(Fe + Mg).85 X Sp, X Grs 0.10 0 0.20 0.15 0.10 0.05 0 b incl. 465 m incl. Porphyroblast B 700m incl. 225 m Porphyroblast A Relative Position Fe/(Fe + Mg) Figure DR2. Electron microprobe composition profiles across garnet porphyroblasts in samples #15 (grains A-C) and #14 (grains A and B). The occurrence of more calcic (X An = 0.35-0.38) plagioclase inclusions in garnet than matrix plagioclase (X An = 0.24-0.27) suggests increasing P during garnet growth on a clockwise P-T path. Mn and Fe enrichment of garnet rims is caused by retrograde reequilibration. X Sp X Grs X Grs X Sp incl. 575 m 500m #14.75.65.85.75.65 Fe/(Fe + Mg)

DR2007225 Berman et al. page 8 #14 #15 M5 Qz Qz 100 mm Ky Grt M1 1 mm a 200 mm 20 mm b Figure DR3. SEM images of elongate monazite inclusions in S2-parallel (a) kyanite and (b) biotite, supporting syn-s2 growth of monazite. Insets show location of SHRIMP analyses #c-5.1 (a) and #c-1.1 (b) of Table DR3. 0.5 mm Grt Qtz Figure DR4. Photomicrograph showing metapelite sample #11 with peak assemblage garnet-staurolite-sillimanite-biotite-plagioclase-quartz. 10 mm Figure DR5. Secondary electron image of zircon inclusion in biotite of sample #11. Cathode luminescent imaging shows no zoning within this zircon grain. SHRIMP pits show position of analyses giving ~1.9 Ga metamorphic age of two rims with Th/U < 0.003, and ~2.3 Ga age of core with Th/U = 0.68. The high Th/U of the zircon core supports its interpretation as a detrital grain of igneous origin. High Th/U zircon cores for this sample range in age between 2.7 to 2.3 Ga.

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