Taltson basement gneissic rocks: U–Pb and Nd isotopic constraints on the basement to the Paleoproterozoic Taltson magmatic zone, northeastern Alberta

• Published in: Canadian Journal of Earth Sciences
• Main Authors: McNicoll, Vicki J, Thériault, Réginald J, McDonough, Michael R
• Format: Article in Journal/Newspaper
• Language: English
• Published: Canadian Science Publishing 2000
• Subjects: Buffalo Head; Northwest Territories
• Online Access: http://dx.doi.org/10.1139/e00-034; http://www.nrcresearchpress.com/doi/pdf/10.1139/e00-034

The Taltson magmatic zone is a 300 km long, northerly trending belt of Archean to Paleoproterozoic granitic basement gneiss, amphibolite, supracrustal gneissic rocks, and voluminous Paleoproterozoic magmatic rocks underlying northeastern Alberta and the southwestern portion of the Northwest Territor...