Uranium Series, Rates of Basaltic Melt Generation and Transport
Author:
Pietruszka Aaron J.
Publisher
Springer Netherlands
Reference19 articles.
1. Bourdon, B., Turner, S., and Dosseto, A., 2003. Dehydration and partial melting in subduction zones: constraints from U-series disequilibria. Journal of Geophysical Research, 108, 2291, doi:10.1029/2002JB001839. 2. Bourdon, B., Ribe, N. M., Stracke, A., Saal, A. E., and Turner, S. P., 2006. Insights into the dynamics of mantle plumes from uranium-series geochemistry. Nature, 444, 713–717. 3. Chabaux, F., and Allègre, C. J., 1994. 238U-230Th-226Ra disequilibria in volcanics: a new insight into melting conditions. Earth and Planetary Science Letters, 126, 61–74. 4. Condomines, M., and Sigmarsson, O., 1993. Why are so many arc magmas close to 238U-230Th radioactive equilibrium? Geochimica et Cosmochimica Acta, 57, 4491–4497. 5. Dosseto, A., and Turner, S., 2013. Reappraisal of uranium-series isotope data in Kamchatka lavas: implications for continental arc magma genesis. In Gomez-Tuena, A., Straub, S. M., and Zellmer, G. F. (eds.). Orogenic Andesites and Crustal Growth. London: Geological Society. Special Publications, Vol. 385,
http://dx.doi.org/ 10.1144/SP385.5
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