The extent of U-series disequilibria produced during partial melting of the lower crust with implications for the formation of the Mount St. Helens dacites

The extent to which U-series disequilibria can be produced during partial melting of mafic lower crust is quantified using a simple batch melting model and both experimental and theoretical partition coefficients for U, Th and Ra. We show that partial melting of mafic lower crust can only produce sm...

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Detalhes bibliográficos
Principais autores: Berlo, K, Turner, S, Blundy, J, Hawkesworth, C
Formato: Journal article
Idioma:English
Publicado em: 2004