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Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: An in situ experimental study of Zr4+ transport capacity of water-rich fluids in the temperature and pressure range of the deep crust and upper mantle

Fig. 7

Temperature-dependence of the equilibrium constant, K (4), for equilibrium (4) for the compositions indicated. Regression coefficients are shown in Tables 2 and 3. Average pressure is that calculated from the regression line in Fig. 2. For actual pressure, see Table 1. Horizontal error bars represent calculated pressure uncertainty (±110 MPa; see text)

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