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Decoupling of Zr-Hf during contact metamorphic anatexis of metabasalts and timing of zircon growth, Sudbury, Canada. GeologyGeology. 2017.
Preliminary results from transect mapping in the Abitibi greenstone belt and Pontiac Subprovince, Rouyn-Noranda area, Quebec.; 2017.
Evolution of the Sudbury igneous complex southern metamorphic aureole and controls on anatexis. Vol PhD. Laurentian University; 2017.
Decoupling of Zr-Hf during contact metamorphic anatexis of metabasalts and timing of zircon growth, Sudbury, Canada. GeologyGeology. 2017;46:159-162.
Sulfur K-edge XANES analysis of natural and synthetic basaltic glasses: Implications for S speciation and S content as function of oxygen fugacity. Geochimica et Cosmochimica ActaGeochimica et Cosmochimica Acta. 2010;74:5926-5938.
Sulfur content at sulfide saturation in oxidized magmas. GeologyGeology. 2009;37:415-418.
40Ar/39Ar ages of CAMP in North America: Implications for the Triassic–Jurassic boundary and the 40K decay constant bias. LithosLithos. 2009;110:167-180.
Structural Controls on Gold Mineralization at the Burnt Timber Mine, Lynn Lake Greenstone Belt, Trans-Hudson Orogen, Manitoba. Exploration and Mining GeologyExploration and Mining Geology. 2006;15:89-100.
Geology of the shear-hosted Burnt Timber deposit, Lynn Lake, northern Manitoba. Vol MSc. Laurentian University; 2005.