Abstract
THE relatively sharp step in the 87Sr/86Sr ratio within basalts midway along the Reykjanes Ridge may reflect the breakdown of titaniferous phlogopite during variable fusion of an essentially homogeneous phlogopite-lherzolite upper mantle, extending beneath both Iceland and the submarine parts of the Mid-Atlantic Ridge.
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FLOWER, M., SCHMINCKE, HU. & THOMPSON, R. Phlogopite stability and the 87Sr/86Sr step in basalts along the Reykjanes Ridge. Nature 254, 404–406 (1975). https://doi.org/10.1038/254404a0
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DOI: https://doi.org/10.1038/254404a0
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