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-List Of Titles -A refractory mantle protolith in younger continental crust, east-central China : age and composition of zircon in the Sulu ultrahigh-pressure peridotite

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/10128

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Title
A refractory mantle protolith in younger continental crust, east-central China : age and composition of zircon in the Sulu ultrahigh-pressure peridotite
Related
Geology, Vol. 34, Issue 9, p.705-708
DOI
10.1130/G22569.1
Publisher
Geological Society of America
Date
2006
Author/Creator
Zheng, Jianping
Author/Creator
Griffin, W. L
Author/Creator
O'Reilly, Suzanne Y
Author/Creator
Yang, J. S
Author/Creator
Zhang, R. Y
Description
Zircons have been extracted from garnet peridotite and its wall rock (gneiss), which was intersected by the pre–pilot hole of the Chinese Continental Scientific Drilling project (CCSD-PP1) in the Sulu ultrahigh-pressure (UHP) metamorphic belt. The peridotitic zircons record early Mesozoic UHP metamorphism (²⁰⁶Pb/²³⁸U age of 223.5 ± 7.5 Ma), but their Hf isotope compositions indicate that the protolith of the peridotite is at least Mesoproterozoic in age (minimum depleted-mantle ages [TDM] of 1.4 Ga). Zircons from the gneiss also reflect the Mesozoic metamorphism, with a cluster of ²⁰⁶Pb/²³⁸U ages at 224.5 ± 11.5 Ma; a trail of discordant grains indicates a protolith age older than 800 Ma, consistent with TDM model ages of younger than 1.2 Ga. The peridotitic zircons have trace-element patterns similar to kimberlitic and/or carbonatitic zircons, while those from the gneiss have affinities with zircons from syenites/monzonites. The differences suggest that the metasomatic agents that affected the peridotitic zircons were derived from the asthenospheric mantle rather than from subducted continental crust. The strong depletion of the CCSD-PP1 peridotite in basaltic components, and the relatively unradiogenic Hf isotopic compositions (e.g., −16.3 to ~−13.8 εHf) of the peridotitic zircons, indicate that the peridotitic body is a fragment of refractory Archean mantle that experienced Mesoproterozoic metasomatism and represents a tectonic intrusion into younger crust.
Description
4 page(s)
Subject Keyword
peridotitic zircon
Subject Keyword
Hf isotope
Subject Keyword
trace element
Subject Keyword
U-Pb dating
Subject Keyword
Sulu UHP terrane
Subject Keyword
China
Resource Type
journal article
Organisation
Macquarie University. National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC)

Identifier
http://hdl.handle.net/1959.14/10128
Identifier
ISSN:0091-7613
Identifier
mq-rm-2006000154
Language
eng
Reviewed
Reviewed
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Citation Format
E-mail Address
Subject
"Geology"
 
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