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A reduction in 87Sr/86Sr during basalt alteration

Abstract

HYDROTHERMAL alteration of basalts on the ocean floor has been reported to cause a general increase in the 87Sr/86Sr ratio of the basalts1,2. Results are presented here from Mull in the British Tertiary province which suggest strongly that hydrothermal alteration in such discrete magmatic centres may actually cause a reduction in the 87Sr/86Sr ratios of some basalts. Preliminary data indicate that the 143Nd/144Nd ratios are unaffected.

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HAWKESWORTH, C., MORRISON, M. A reduction in 87Sr/86Sr during basalt alteration. Nature 276, 381–383 (1978). https://doi.org/10.1038/276381a0

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  • DOI: https://doi.org/10.1038/276381a0

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