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. 2001 May 1;411(6835):293–296. doi: 10.1038/35077056

Figure 2. Modal percentages of minerals and fluid composition.

Figure 2

Modal percentages of minerals (left ordinate and solid lines) and fluid composition (right ordinate and dashed line) are shown for the average marine sediment bulk composition (‘GLOSS’ in ref. 8) along the high-temperature geotherm shown in Fig. 1. Phase abbreviations as in Fig. 1. The vertical line at ∼770 °C marks the quartz–coesite equilibrium.