Rapid differentiation of mafic to intermediate magma constrained by Ra–Th disequilibrium and the size of magma chamber beneath Hekla volcano, Iceland
Author:
Funder
Rannis
Clervolc
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00410-024-02148-7.pdf
Reference41 articles.
1. Baldridge SW, McGetchin TR, Frey FA (1973) Magmatic evolution of Hekla, Iceland. Contrib Mineral Petrol 42:245–258. https://doi.org/10.1007/BF00371589
2. Baxter RJM, Maclennan J, Neave DA, Thordarson T (2023) Depth of magma storage under Iceland controlled by magma fluxes. Geochem Geophys Geosystems 24:e2022GC010811. https://doi.org/10.1029/2022GC010811
3. Berlo K, Turner S, Blundy J, Hawkesworth C (2004) 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 Contrib Mineral Petrol 148:122–130. https://doi.org/10.1007/s00410-004-0590-2
4. Blake S, Rogers N (2005) Magma differentiation rates from (226Ra/230Th) and the size and power output of magma chambers. Earth Planet Sci Lett 236:654–669. https://doi.org/10.1016/j.epsl.2005.05.035
5. Blundy JD, Wood BJ (2003) Mineral-melt partitioning of uranium, thorium and their daughters. Rev Mineral Geochem 52:59–118. https://doi.org/10.2113/0520059
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