Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/35082540.pdf
Reference25 articles.
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4. Murphy, M. D., Sparks, R. S. J., Barclay, J., Carroll, M. R. & Brewer, T. S. Remobilisation of andesite magma by intrusion of mafic magma at the Soufrière Hills Volcano, Montserrat, West Indies. J. Petrol. 41, 21–42 (2000).
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