Lu–Hf garnet dating and the timing of collisions: Palaeoproterozoic accretionary tectonics revealed in the Southeastern Churchill Province, Trans‐Hudson Orogen, Canada-Reference-Cited by-同舟云学术

Lu–Hf garnet dating and the timing of collisions: Palaeoproterozoic accretionary tectonics revealed in the Southeastern Churchill Province, Trans‐Hudson Orogen, Canada

Published:2021-03-18 Issue:8 Volume:39 Page:977-1007
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Godet Antoine¹^ORCID,Guilmette Carl¹^ORCID,Labrousse Loic¹²,Smit Matthijs A.³,Cutts Jamie A.³,Davis Donald W.⁴,Vanier Marc‐Antoine⁵

Affiliation:

1. E4m Département de géologie et de génie géologique Université Laval Québec QC Canada

2. Sorbonne Université CNRS‐INSU Institut des Sciences de la Terre Paris ISTeP UMR 7193 Paris France

3. PCIGR Department of Earth, Ocean and Atmospheric Sciences University of British Columbia Vancouver BC Canada

4. Department of Earth Sciences University of Toronto Toronto ON Canada

5. Bureau de la connaissance géoscientifique du Québec Québec QC Canada

Funder

Ministère de l'Énergie et des Ressources Naturelles

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

British Columbia Knowledge Development Fund

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12599

Reference141 articles.

1. Timing of collision of the Sino-Korean and Yangtse cratons: U-Pb zircon dating of coesite-bearing eclogites

2. Lu–Hf geochronology and trace element distribution in garnet: Implications for uplift and exhumation of ultra-high pressure granulites in the Sudetes, SW Poland

3. Garnet Geochronology: Timekeeper of Tectonometamorphic Processes

4. Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy

5. Models of large, hot orogens containing a collage of reworked and accreted terranesThis article is one of a series of papers published in this Special Issue on the themeLithoprobe — parameters, processes, and the evolution of a continent.

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