SHRIMP U-Pb dating of zircon from the Xugou UHP eclogite, Sulu terrane, eastern China

International Geology Review
By: , and 

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Abstract

clogites, together with garnet clinopyroxenites, occur as lenses within the Xugou garnet peridotite body in the southern Sulu ultrahigh-pressure (UHP) terrane. Combined cathodoluminescence (CL) imaging and SHRIMP U-Pb dating of zircon from two Xugou mafic eclogites provide added constraints on the timing of UHP metamorphism in this area. Zircons from both samples show subrounded to rounded shapes and patchy CL patterns without inherited igneous cores, indicating that they are metamorphic zircons. SHRIMP U-Pb analyses of these zircons yielded apparent U-Pb ages of 214-280 Ma, with a weighted mean age of 237 ± 8 Ma, which is consistent with previous reported UHP metamorphic ages from eclogite pods and country-rock gneisses. The Xugou mafic lenses may have formed by partial melting of the enclosing peridotites in the mantle before subduction (Zhang et al., 2003); then these eclogites, together with the host peridotites, were tectonically emplaced into the subduction zone and subjected to UHP metamorphism at 237 ± 8 Ma.

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Publication type Article
Publication Subtype Journal Article
Title SHRIMP U-Pb dating of zircon from the Xugou UHP eclogite, Sulu terrane, eastern China
Series title International Geology Review
DOI 10.2747/0020-6814.47.8.805
Volume 47
Issue 8
Year Published 2005
Language English
Publisher Taylor & Francis
Description 10 p.
First page 805
Last page 814
Country China
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