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Creaser, Robert A., Heaman, Larry M., Erdmer, Philippe (1997) Timing of high-pressure metamorphism in the Yukon – Tanana terrane, Canadian Cordillera: constraints from U – Pb zircon dating of eclogite from the Teslin tectonic zone. Canadian Journal of Earth Sciences, 34 (5) 709-715 doi:10.1139/e17-057

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Reference TypeJournal (article/letter/editorial)
TitleTiming of high-pressure metamorphism in the Yukon – Tanana terrane, Canadian Cordillera: constraints from U – Pb zircon dating of eclogite from the Teslin tectonic zone
JournalCanadian Journal of Earth Sciences
AuthorsCreaser, Robert A.Author
Heaman, Larry M.Author
Erdmer, PhilippeAuthor
Year1997 (May 1)Volume34
Issue5
PublisherCanadian Science Publishing
DOIdoi:10.1139/e17-057Search in ResearchGate
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Mindat Ref. ID482964Long-form Identifiermindat:1:5:482964:9
GUID0
Full ReferenceCreaser, Robert A., Heaman, Larry M., Erdmer, Philippe (1997) Timing of high-pressure metamorphism in the Yukon – Tanana terrane, Canadian Cordillera: constraints from U – Pb zircon dating of eclogite from the Teslin tectonic zone. Canadian Journal of Earth Sciences, 34 (5) 709-715 doi:10.1139/e17-057
Plain TextCreaser, Robert A., Heaman, Larry M., Erdmer, Philippe (1997) Timing of high-pressure metamorphism in the Yukon – Tanana terrane, Canadian Cordillera: constraints from U – Pb zircon dating of eclogite from the Teslin tectonic zone. Canadian Journal of Earth Sciences, 34 (5) 709-715 doi:10.1139/e17-057
In(1997, May) Canadian Journal of Earth Sciences Vol. 34 (5) Canadian Science Publishing
Abstract/Notes Zircon from eclogite near Last Peak in the Teslin tectonic zone yielded a U–Pb isotopic age of 269 + 2 Ma (2σ), the first precise age for such a rock in the Yukon –Tanana terrane of the Canadian Cordillera. Both the morphology and geochemistry of the eclogitic zircons indicate a metamorphic origin, and the U – Pb age therefore constrains the timing of peak high-pressure metamorphism in this rock. The U – Pb age demonstrates for the first time that an Early Permian high-pressure metamorphic event occurred in rocks now making up the Teslin tectonic zone, and possibly elsewhere in the Yukon – Tanana terrane. This U – Pb age provides a new geochronologic "pin" in the evolution of the Yukon – Tanana terrane prior to its Mesozoic accretion to the North American continental margin and, combined with recent 40Ar/39Ar muscovite data, indicates that high-pressure metamorphism at this time was a relatively short-lived event.


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