Solution behavior of reduced N-H-O volatiles in FeO-Na2O-SiO2-Al2O3 melt equilibrated with molten Fe alloy at high pressure and temperature

Physics of the Earth and Planetary Interiors

Volumn 214, Issue , 2013, Pages 14-24

  Kadik, Arnold A ^a   Litvin, Yuri A ^b   Koltashev, Vasily V ^c   Kryukova, Elena B ^a   Plotnichenko, Victor G ^c   Tsekhonya, Tatiana I ^a   Kononkova, Nataliya N ^a  

^a VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

^b INSTITUTE OF EXPERIMENTAL MINERALOGY   (Russian Federation)

^c FIBER OPTICS RESEARCH CENTER   (Russian Federation)

Author keywords

Early Earth's mantle; Iron; Magma ocean; Nitrogen; Oxygen and hydrogen fugacity

Indexed keywords

EARLY EARTH; EXPERIMENTAL CONDITIONS; EXPERIMENTAL STUDIES; FTIR; HIGH-PRESSURE AND TEMPERATURES; HYDROGEN ANALYSIS; HYDROGEN FUGACITY; HYDROGEN SOLUBILITY; MAGMA OCEAN; METALLIC MELTS; NITROGEN CONTENT; NITROGEN SOURCES; OXYGEN FUGACITY; SILICATE MELTS; SOLUTION BEHAVIOR;

FOURIER TRANSFORM INFRARED SPECTROSCOPY; HYDROGEN; IRON; IRON OXIDES; NITROGEN; PLATINUM; REDOX REACTIONS; SILICATES; SILICON; SODIUM; SOLUBILITY;

IRON ALLOYS;

ALLOY; EARLY EARTH; FUGACITY; HIGH PRESSURE; HIGH TEMPERATURE; HYDROGEN; IRON; MAGMA CHEMISTRY; MANTLE STRUCTURE; NITROGEN; OXYGEN; SILICATE MELT; SOLUBILITY; SPECIATION (CHEMISTRY); VOLATILE ELEMENT;

EID: 84872412207     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2012.10.013     Document Type: Article

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