The natural reaction muscovite+chlorite+chloritoid=andalusite+biotite+ quartz+H20 and a new petrogenetic grid
Geosciences Journal(2000)
Abstract
The univariant KFMASH reaction, chlorite+chloritoid+muscovite=andalusite+biotite+quartz+H2O, occurs in a low pressure (1–2 kbar) thermal aureole, defining a new biotite isograd. The Mg/Fe+Mg ratios of chlorite, chloritoid
and biotite in the reaction are 0.14, 0.04, and 0.12, respectively. The univariant equilibrium is generated from a low pressure
invariant point involving the phase chlorite, chloritoid, biotite, aluminosilicate, and staurolite that are added to the petrogenetic
grid of Harte and Hudson (1979). This addition eliminates the unrealistic stability field of cordierite+staurolite in Harte
and Hudson grid.
Two other univariant reactions, terminal reactions of chlorite and muscovite, are also observed in the aureole. The three
univariant reactions separate the aureole into four zones, chlorite-chloritoid zone, andalusite-biotite-chlorite zone, andalusite-biotite-cordierite
zone, and K-feldspar zone.
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Key words
low pressure
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