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Hydrothermal alteration of alkali-feldspar and plagioclase commonly results into the formation of quartz and white mica in the form muscovite or paragonite which are collectively termed sericite due to sericitization (Que and Allen 1996).Equation
The growth of Ab porphyroblasts could result from destabilisation of jadeite through reactions such as Jd + Qz = Ab, or paragonite, present in some rocks of ChMC (Willner et al., 2012).