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Nickel—tungsten pressure effect

The effect of oxygen pressure on the solubihties of siderophile elements in silicate melt has been understood for many years due to metallurgical interest, and has been known to the geological community since early work of Newsom and Drake (1982, 1983) on tungsten and phosphorus. Although there was a brief exploration of the possibility of zero valence dissolution of nickel and possibly cobalt at low /o (Colson, 1992 ... [Pg.1128]

See other pages where Nickel—tungsten pressure effect is mentioned: [Pg.421]    [Pg.43]    [Pg.408]    [Pg.206]    [Pg.404]    [Pg.169]    [Pg.400]    [Pg.400]    [Pg.183]    [Pg.1139]    [Pg.27]    [Pg.439]    [Pg.269]    [Pg.217]    [Pg.261]    [Pg.544]    [Pg.106]    [Pg.306]   
See also in sourсe #XX -- [ Pg.197 ]



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Nickel-tungsten

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