Effects of fuid and melt density and structure on high-pressure and high-temperature experimental studies of hydrogen isotope partitioning between coexisting melt and aqueous fuid

American Mineralogist

Volumn 98, Issue 10, 2013, Pages 1754-1764

  Mysen, Bjorn ^a  

^a GEOPHYSICAL LABORATORY   (United States)

Author keywords

Aqueous fluid; Hydrogen isotopes; Hydrous melt; Pressure; Structure; Temperature; Vibrational spectroscopy

Indexed keywords

HIGH PRESSURE EFFECTS; HYDROGEN; ISOTOPES; PRESSURE; STRUCTURE (COMPOSITION); TEMPERATURE; TRAJECTORIES; VIBRATIONAL SPECTROSCOPY;

AQUEOUS FLUIDS; HIGH PRESSURE AND HIGH TEMPERATURE; HIGH TEMPERATURE AND PRESSURE; HYDROGEN ISOTOPE; HYDROTHERMAL DIAMOND ANVIL CELL; HYDROUS MELTS; INCREASING TEMPERATURES; TEMPERATURE AND PRESSURES; ALUMINO-SILICATE MELTS;

SILICATES;

ALUMINOSILICATE; DENSITY; EXPERIMENTAL MINERALOGY; HIGH PRESSURE; HIGH TEMPERATURE; HYDROGEN ISOTOPE; INFRARED SPECTROSCOPY; ISOTOPIC FRACTIONATION; ISOTOPIC RATIO; MELT; PARTITIONING; RAMAN SPECTROSCOPY; SOLUTION; SPECIATION (BIOLOGY); DIAMOND ANVIL CELL; EXPERIMENTAL STUDY; SPECTROSCOPY; UPPER MANTLE;

EID: 84885071526     PISSN: 0003004X     EISSN: 19453027     Source Type: Journal    
DOI: 10.2138/am.2013.4449     Document Type: Article

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