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Oxygen isotope evidence for recycled crust in the source of EM-type ocean island basalts

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Abstract

The oxygen isotope compositions of fresh volcanic glasses from submarine volcanoes of 'enriched mantle' (EM-1 and EM-11) type appear to require the presence of subducted crustal components in the source of these lavas. These data confirm earlier inferences from trace elements and radiogenic isotopes, and also provide a rare opportunity to estimate the proportion of subducted material that reaches the source region of ocean island basalts.

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Authors and Affiliations

  1. Research School of Earth Sciences, Australian National University, Canberra, Australian Capital Territory, 0200, Australia

    Jon D. Woodhead

  2. NERC Isotope Geosciences Laboratory, Kingsley Dunham Centre, Keyworth, Nottingham, NG12 5GG, UK

    Peter Greenwood & Russell S. Harmon

  3. Geologische Institut der Universität Kiel, 40–60 Olshausenstrasse, 2300, Kiel, Germany

    Peter Stoffers

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  1. Jon D. Woodhead
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  2. Peter Greenwood
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  3. Russell S. Harmon
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  4. Peter Stoffers
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Woodhead, J., Greenwood, P., Harmon, R. et al. Oxygen isotope evidence for recycled crust in the source of EM-type ocean island basalts. Nature 362, 809–813 (1993). https://doi.org/10.1038/362809a0

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