Journal of Petrology Advance Access originally published online on November 3, 2006
Journal of Petrology 2007 48(2):271-302; doi:10.1093/petrology/egl060
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Polymetamorphic Evolution of the Trans-Hudson Orogen, Baffin Island, Canada: Integration of Petrological, Structural and Geochronological Data
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada, K1A 0E8
RECEIVED MAY 26, 2005; ACCEPTED SEPTEMBER 21, 2006
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Supracrustal units metamorphosed at mid-crustal conditions within the Paleoproterozoic Trans-Hudson Orogen are preserved within an obliquely exposed continental collision zone on Baffin Island (Canada). Early granulite-facies assemblages yield thermobarometric data and phase diagram information that define a steep, compressive PT path segment. These assemblages are bracketed between ca. 1849 and 1835 Ma, and are interpreted to result from (1) heat advection by an 1865 +4/2 to 1848 ± 2 Ma Andean-type granitic batholith, and (2) a ca. 1845 Ma crustal thickening event associated with accretion of an intra-oceanic arc terrane. A subsequent regional metamorphic event is characterized by the growth of retrograde, upper amphibolite-facies assemblages that define a clockwise, decompressive PT path. Mineral growth is bracketed between 1820 ± 1 and 1813 ± 2 Ma, and is localized within deformation zones associated with the 1820 +4/3 to 1795 ± 2 Ma collision of the Rae and Superior cratons. The metamorphic history of Baffin Island supports a progressive change from plate-margin to intraplate processes within an evolving convergent orogen during the Paleoproterozoic that is similar to those documented in younger collisional belts.
KEY WORDS: polymetamorphism; geochronology; Paleoproterozoic; Trans-Hudson Orogen
Corresponding author. Telephone: (613) 995-4935. Fax: (613) 943-5318. E-mail: mstonge{at}nrcan.gc.ca
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