Determining the 17O/16O ratio of water using a water–CO2 equilibration method: Application to glacial–interglacial changes in 17O-excess from the Dome Fuji ice core, Antarctica
Determining the 17O/16O ratio of water using a water–CO2 equilibration method: Application to glacial–interglacial changes in 17O-excess from the Dome Fuji ice core, Antarctica
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