GSA Annual Meeting, November 5-8, 2001

Paper No. 0
Presentation Time: 1:30 PM-5:30 PM

PRE-OBDUCTION STRUCTURES OF THE THETFORD MINES OPHIOLITIC COMPLEX (TMOC), QUEBEC : IMPLICATIONS FOR OCEANIC CRUST FORMATION AND PGE MINERALISATION


SCHROETTER, Jean-Michel, Centre geoscientifique de Quebec, Institut national de la recherche scientifique, CP7500, 880, chemin St Foy, Quebec, QC G1V 4C7, Canada, PAGÉ, Philippe, Centre Geoscientifique de Quebec, Institut National de la Recherche Scientifique, CP 7500, 880 Ste-Foy, Ste-Foy, QC G1V 4C7, Canada, TREMBLAY, Alain, INRS-Géoressources, Quebec Geoscience Ctr, 880 Chemin Sainte-Foy, P.O. Box 7500, Sainte Foy, QC G1V 4C7, Canada and BÉDARD, Jean H., Centre Geoscientifique de Quebec, Geol Survey of Canada, CGQ, CP7500, 880 Ste-Foy, Ste-Foy, QC G1V 4C7, Canada, ppage@rncan.gc.ca

The TMOC is divided into two different petrologic and structural units, a NW mantle-dominated massif (Thetford Mines unit) and a SE crustal-dominated massif (Mont Adstock unit). Three types of tectonic fabrics can be identified, pre-, syn- and post-obduction. Post-obduction structural features consist of NE-trending Acadian open folds and reverse faults, Late Silurian- Early Devonian backfolds and normal faults such as the Saint-Joseph fault (SJF).The TMOC occurs in the hanging wall of the SJF. Structures attributed to ophiolite obduction onto the Laurentian Margin consist mainly of a metamorphic sole and related structures at the base of the mantle section. Pre-obduction structures show two different sub-vertical orientations, NS and NW-trending. There are underlined by sheared dunite (mylonite), and the NS-trending set, appears to control the emplacement of mafic-ultramafic bodies into the cumulates. In the upper part of the crust, NS-structures are associated with doleritic dykes, fault breccias, upwardly decreasing throws suggest that they are syn-oceanic grow faults. A Pt-Pd survey shows that chromite-bearing as well as pyroxene-bearing rocks are good prospects for PGE exploration. The greatest PGE concentrations are encountered in discordant chromitite bodies but non-negligible grades have been found in the pyroxenite, near the contact with gabbroic units, and in the bedded chromitite-bearing dunite.