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Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas

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Kamenetsky,  V. S.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Elburg,  M.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Kamenetsky, V. S., Elburg, M., Arculus, R., & Thomas, R. (2006). Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas. Chemical Geology, 233(3-4), 346-357.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0014-88A0-E
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