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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: The responses of the four main substitution mechanisms of H in olivine to H2O activity at 1050 °C and 3 GPa

Fig. 2

Variation in water concentration with XH2O in H2O–NaCl fluids for the four different point defects. The calculated water contents are based only on the principal absorbance bands from each experiment, as discussed in the “Methods” section of the text. The best fit curves are from least squares non-linear regression with weighting of both variables according to the standard deviations in Tables 2 and 3

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