[1]
Fyffe, L.R. et al. 2009. Detrital zircon ages from Neoproterozoic and Early Paleozoic conglomerate and sandstone units of New Brunswick and coastal Maine: implications for the tectonic evolution of Ganderia. Atlantic Geoscience. 45, (Oct. 2009), Pages 110 – 144. DOI:https://doi.org/10.4138/atlgeol.2009.006.