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Sulfur isotope ratios in co-existing galena and sphalerite from broken hill, New South Wales

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In 15 out of 16 sphalerite-galena pairs, there has been a relative concentration of the heavier sulfur isotope in the sphalerite. Comparison of results from many areas suggests that fractionation decreases with increasing metamorphic grade. Applications to geologic thermometry may be significant.

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Economic Geology

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