Gakkel Ridge plagioclase and olivine mineral and melt inclusion analyses
Bennett, Emma N
Jenner, Frances E
Cashman, Katharine V
Lissenberg, C Johan
The depth of crystallisation within mid-ocean ridge magma plumbing systems can be constrained using the volatile content of melt inclusions. Here the volatile-, trace- and major-element compositions of both olivine- and plagioclase-hosted melt inclusions from the Gakkel Ridge (Arctic Ocean) are presented. Host mineral major elements are also presented and were used to undertake melt inclusion post-entrapment crystallisation corrections.
How to cite this dataset:
Bennett, E. N., Jenner, F. E., Millet, M., Cashman, K. V., Lissenberg, C. J., 2019. Gakkel Ridge plagioclase and olivine mineral and melt inclusion analyses, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/111315.
DOI Creation Date:
Bennett, E., Jenner, F., Millet, A-B., Cashman, K., Lissenberg, C., 2019, Deep roots for mid-ocean ridge volcanoes revealed by plagioclase-hosted melt inclusions, Nature, 572 (235-239)
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Arctic Ocean, Gakkel Ridge
User Contributed Keyword(s):
Volatiles, melt inclusions, trace element, ultra-slow spreading ridge, Gakkel Ridge
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