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• W2022888022 abstract "Apatite and silicate glasses share the same water content calibration curves in isotope modes where water was determined from the H⁻ intensity regardless of multicollection or peak jumping. In contrast, the slope of apatite significantly differs from that of silicate glasses in element mode where OH⁻ was counted for the water content." @default.
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• W2022888022 date "2015-01-01" @default.
• W2022888022 modified "2023-10-18" @default.
• W2022888022 title "Measurements of water content and D/H ratio in apatite and silicate glasses using a NanoSIMS 50L" @default.
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• W2022888022 doi "https://doi.org/10.1039/c4ja00417e" @default.
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