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Aluminium saturation index determines whether a rock is metaaluminous or peraluminous, the peraluminous rocks contain aluminous minerals including muscovite, garnet sillimanite and ...

  • A.Cordierite
  • B.Coesite
  • C.Covanzite
  • D.Comingtonite

Answer: A

The missing mineral is Cordierite.

A peraluminous rock has more alumina than is needed to make feldspars, so the excess forms aluminous minerals: muscovite, almandine garnet, the aluminosilicates sillimanite and andalusite, and cordierite, a magnesium-iron aluminosilicate typical of S-type granites and pelitic rocks.

Coesite is a high-pressure form of silica with no aluminium. Cummingtonite (spelt 'Comingtonite' in the paper) is a magnesium-iron amphibole, not an aluminous mineral, and 'Covanzite' is not one of the minerals used to define peraluminous rocks.

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