Metamorphic growth and recrystallization of zircons in extremely 18O-depleted rocks during eclogite-facies metamorphism: Evidence from U–Pb ages, trace elements, and O

Metamorphic growth and recrystallization of zircons in extremely 18O-depleted rocks during eclogite-facies metamorphism: Evidence from U–Pb ages, trace elements, and O–Hf isotopes

Published:2011-09 Issue:17 Volume:75 Page:4877-4898
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Chen Yi-Xiang,Zheng Yong-Fei,Chen Ren-Xu,Zhang Shao-Bing,Li Qiuli,Dai Mengning,Chen Lu

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference93 articles.

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4. Ilmenite as a source for zirconium during high-grade metamorphism? Textural evidence from the Caledonides of Western Norway and implications for zircon geochronology;Bingen;J. Petrol.,2001

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