These acoustic features are typical for lava flows and effusive volcanism as recognized at other submarine volcanoes 48,49 , implying that they are primarily formed by effusive eruptions, producing dense deposits of strongly attenuating lithologies 49 , as would be expected for the Reykjanes Ridge given the mafic nature of the magmatism 15,19,20,21,27
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10.1038/s41598-017-04413-1 120
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