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Geochemical Journal, Vol. 9, pp. 107 to 111, 1975 107 NOTE Hydrogen extractions from silicate minerals by sodium carbonate fusion and its application to deuterium analyses of fluid inclusions in some olivines TETSURO SUZUOKI1, YOSHIMASU KURODA2 and SADAO MATSUO3 Marine Department, Japan Meteorological Agency, Otemachi, Chiyoda-ku, Tokyo 100 Japan1, Department of Geology, Shinshu University, Matsumoto, 390 Japan2 and Department of Chemistry, Tokyo Institute of Technology, O-okayarna, Tokyo 152 Japan3 (Received May 26, 1975) Abstract -Fluid inclusions in olivine were extracted in vacuum by a sodium carbonate fusion method. In the present study, bulk hydrogen content and D/H ratio of the inclusion were measured. The results showed that a consistent value of dD was obtained with a standard deviation of ±2%o, when the absolute amount of hydrogen extracted was more than 40umol (0.9ml STP H2). On the other hand, when the absolute amount of extracted hydrogen was less than 40umol, dD value of the extract fluctuated, probably being affected by the contamination in the whole procedure.