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Granite system water-saturated

Puziewicz J, Joharmes W (1990) Experimental study of a biotite-bearing granitic system under water-saturated and water-undersatrrrated conditions. Contrib Mineral Petrol 104 397-406 Radoslovich EW (1960) The structrrre of muscovite, KAl2(Si3Al)Oio(OH)2. Acta Crystallogr 13 919-932 Radoslovich EW (1961) Strrface symmetry and cell dimertsions of layer lattice silicates. Nature 191 67-68 Radoslovich EW, Norrish K (1962) The cell dimensiorts and symmetry of layer-lattice silicates. I. Some stractural consideratiorrs. Am Mineral 47 599-616... [Pg.95]

Experiments by Schairer (1950), Hamilton and MacICeime (1965), Taylor and MacKenzie (1975) and Morse (1969) have determined the positions of the nepheline syenite minima at pressures of 1 atm, 1 kb, 2 kb and 5 kb, respectively, ill the water-saturated system. These data are presented in Figure 3.25 as QFW normative wt %, in a projection from H2O onm the anhydrous base of the system, the plane nepheline-lralsUite-stUca. Unfike the granite system, the jposition of the... [Pg.86]

See other pages where Granite system water-saturated is mentioned: [Pg.1680]    [Pg.1688]    [Pg.84]    [Pg.86]    [Pg.162]    [Pg.1678]    [Pg.1688]    [Pg.286]    [Pg.108]   


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