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Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: Evidence for magmatic digestion and erosion of Pleistocene hyaloclastites

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Gurenko,  A.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Bindeman, I., Gurenko, A., Sigmarsson, O., & Chaussidon, M. (2008). Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: Evidence for magmatic digestion and erosion of Pleistocene hyaloclastites. Geochimica et Cosmochimica Acta, 72(17), 4397-4420.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0014-849F-5
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