Tectono-Metamorphic Evolution of the Snowcap Assemblage, Yukon-Tanana Terrane, West-Central Yukon
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Quantitative and qualitative analyses of Snowcap Assemblage metapelitic rocks of the Yukon-Tanana terrane (YTT) in west-central Yukon results in the identification of three phases of metamorphism and deformation through garnet crystallization modeling coupled with garnet age dating. A first Permo-Triassic metamorphic event (ca. 245 Ma), associated with a heating event occurring during the emplacement of Permian granitoids, reached low P amphibolite facies metamorphic conditions. The second metamorphic event dated at the Jurassic (ca. 197-188 Ma) reached peak P-T conditions of 7 kbar and 650-685 °C with a heating rate of 20 °C/My and is followed by a dwell period at T > 600 °C. This event follows typical Barrovian-type metamorphism and is interpreted to be associated with the accretion of the YTT onto Laurentia. The third metamorphic event, post-Jurassic in age, reached peak P-T conditions of 6 kbar and 580 °C with a heating rate of 20 °C/My.
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Copyright © 2017 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner.
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morneau-tectonometamorphicevolutionofthesnowcapassemblage.pdf | 2023-05-05 | Public | Download |