Abstract
THE island of Réunion is situated some 375 miles to the east of Madagascar in the Indian Ocean. The isotopic composition of strontium (Table 1) has been determined in a suite of rocks ranging from basalts to quartz-bearing syenites. The investigation was undertaken to see whether or not variations in the isotopic composition of strontium were present in a wide range of rock types situated in an oceanic environment.
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References
Hamilton, E. I., Nature, 206, 251 (1965).
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HAMILTON, E. Isotopic Composition of Strontium in a Variety of Rocks from Réunion Island. Nature 207, 1188 (1965). https://doi.org/10.1038/2071188a0
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DOI: https://doi.org/10.1038/2071188a0
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