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Figure 1.9 Approximate location of metamorphic facies and of some important reactions
in the PT diagram.
1 analcime + quartz (low temperature) = albite + H 2 O (higher temperature)
2 laumontite + 2 quartz + H 2 O (low pressure) = lawsonite (high pressure)
2' upper limit of stability of lawsonite that is replaced at higher temperature by epidote
3 calcite (low pressure) = aragonite (high pressure)
4 albite (low pressure) = jadeite + quartz (high pressure)
5 andalusite (low pressure) = kyanite (high pressure)
6 andalusite (low temperature) = sillimanite (high temperature)
7 kyanite (low temperature) = sillimanite (high temperature)
8 muscovite + quartz (low temperature) = potassium feldspar + silicate of alumina + H 2 O (high
temperature)
9 solidus of granitic rock (water saturated)
10 solidus of an olivine tholeiite à (water saturated)
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