Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China: Hf and O isotopes in zircon-Reference-Cited by-同舟云学术

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Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China: Hf and O isotopes in zircon

Published:2013-03 Issue: Volume:366 Page:71-82
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Wang Xiao-Lei,Zhou Jin-Cheng,Wan Yu-Sheng,Kitajima Kouki,Wang Di,Bonamici Chloe,Qiu Jian-Sheng,Sun Tao

Funder

National Natural Science Foundation of China

973 project of China

US National Science Foundation

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference58 articles.

1. Coupled elemental and isotopic analyses of polygenetic zircons from granitic rocks by ion microprobe, with implications for melt evolution and the sources of granitic magmas;Barth;Chem. Geol.,2010

2. Igneous zircon: trace element composition as an indicator of source rock type;Belousova;Contrib. Mineral. Petrol.,2002

3. Zircon U–Pb isotope, δ18O and trace element response to 80m.y. of high temperature metamorphism in the lower crust: sluggish diffusion and new records of Archean craton formation;Bowman;Am. J. Sci.,2011

4. Two contrasting granite types: 25 years later;Chappell;Aust. J. Earth Sci.,2001

5. 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;Chen;Geochim. Cosmochim. Acta,2011

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