A Zn isotope perspective on the rise of continents

Zinc isotope abundances are fairly constant in igneous rocks and shales and are left unfractionated by hydrothermal processes at pH 

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Bibliographic Details
Published in:Geobiology 2013-05, Vol.11 (3), p.201-214
Main Authors: Pons, M.-L., Fujii, T., Rosing, M., Quitté, G., Télouk, P., Albarède, F.
Format: Article
Language:English
Subjects:
Carboxylic Acids - analysis
Chromatography, Ion Exchange
Evolution, Planetary
Ferric Compounds - chemistry
Geologic Sediments - analysis
Mass Spectrometry
Oceans and Seas
Phosphates - analysis
Seawater - chemistry
Zinc Isotopes - analysis
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Description
Summary:Zinc isotope abundances are fairly constant in igneous rocks and shales and are left unfractionated by hydrothermal processes at pH 
ISSN:1472-4677
1472-4669
DOI:10.1111/gbi.12030