Sulfur mass-independent fractionation in subsurface fracture waters indicates a long-standing sulfur cycle in Precambrian rocks
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DOI: 10.1038/ncomms13252
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Cited by:
- O. Warr & C. J. Ballentine & T. C. Onstott & D. M. Nisson & T. L. Kieft & D. J. Hillegonds & B. Sherwood Lollar, 2022. "86Kr excess and other noble gases identify a billion-year-old radiogenically-enriched groundwater system," Nature Communications, Nature, vol. 13(1), pages 1-9, December.
- Elliott P. Mueller & Juliann Panehal & Alexander Meshoulam & Min Song & Christian T. Hansen & Oliver Warr & Jason Boettger & Verena B. Heuer & Wolfgang Bach & Kai-Uwe Hinrichs & John M. Eiler & Victor, 2024. "Isotopic evidence of acetate turnover in Precambrian continental fracture fluids," Nature Communications, Nature, vol. 15(1), pages 1-9, December.
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