Mineral-scale Sr isotope variation in plutonic rocks – a tool for unraveling the evolution of magma systems.

Isotope ratios of elements such as Sr, Nd, Pb and Hf can be used as tracers of magmatic sources and processes. Analytical capabilities have evolved so that isotope ratios can now be analysed in situ, and isotopic tracers can therefore be used within single minerals to track the changing magmatic env...

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Bibliographic Details
Published in:Transactions of the Royal Society of Edinburgh: Earth Sciences
Main Authors: Davidson, J.P., Font, L., Charlier, B.L.A., Tepley, F.J. III
Format: Article in Journal/Newspaper
Language:unknown
Published: Cambridge University Press 2006
Subjects:
Cooling histories
Crystal isotope stratigraphy
Differentiation
Feldspars
Isotope ratios
Dais
Antarc*
Antarctica
Online Access:http://dro.dur.ac.uk/12241/
http://dro.dur.ac.uk/12241/1/12241.pdf
https://doi.org/10.1017/S0263593300001504

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