Abstract
The isotopic composition of gallium in six iron meteorites and a terrestrial standard were measured using a solid source mass spectrometer. Isotopic abundances of meteoritic and terrestrial gallium agree to within 0.11 per cent. The concentration of gallium in 21 iron and 5 stone meteorites and in 13 standard rocks was determined using the method of isotope dilution. In general, the agreement between this work and other published data is excellent.
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