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-Reference-Cited by-同舟云学术

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

Published:2004-07-15 Issue:1 Volume:148 Page:122-130
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Berlo K.,Turner S.,Blundy J.,Hawkesworth C.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-004-0590-2.pdf

Reference36 articles.

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2. Bingen B, Demaiffe D, Hertogen J (1996) Redistribution of rare earth elements, thorium, and uranium over accessory minerals in the course of amphibolite to granulite facies metamorphism: the role of apatite and monazite in orthogneisses from southwestern Norway. Geochim Cosmochim Acta 60:1341–1354. DOI: 10.1016/0016-7037(96)00006-3

3. Blundy J, Brooker R (2004) Trace element partitioning during partial melting and crystallisation of hydrous basalt in the lower crust.

4. Blundy J, Wood B (1994) Prediction of crystal-melt partition coefficients from elastic moduli. Nature 372:452–454. DOI: 10.1038/372452a0

5. Blundy J, Wood B (2003) Mineral-melt partitioning of uranium, thorium and their daughters. In: Bourdon B, Henderson G, Lundstrom C, Turner S (eds) Uranium series geochemistry. Rev Miner Geochem 52:59–123

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