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Crystal-chemical controls on the partitioning of Sr and Ba between plagioclase feldspar, silicate melts, and hydrothermal solutions

Abstract:

The isothermal (750°C) experiments of Lagache and Dujon (1987) reveal that the partitioning of Sr between plagioclase feldspar and hydrothermal solutions is a funtion of the anorthite (An) content of the plagioclase, indicating that crystal chemistry may exert a powerful influence on trace element partitioning. In order to compare these results with those on trace element partitioning between plagioclase and silicate melts we have compiled from the literature a large dataset of experimental a...

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Authors


Blundy, JD More by this author
More by this author
Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Journal:
Geochimica et Cosmochimica Acta
Volume:
55
Issue:
1
Pages:
193-209
Publication date:
1991
DOI:
ISSN:
0016-7037
URN:
uuid:cf596ac8-122f-49a6-9560-d53f24ae44f2
Source identifiers:
177554
Local pid:
pubs:177554
Language:
English

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