It has been reported as forming alteration pseudomorphs of chiastolite along with muscovite and paragonite.
2.
The margarite in this occurrence forms preferentially along the dark graphite rich inclusions with the chiastolite crystals.
3.
The nodules consist of iron minerals, carbon substances and mica; as the metamorphic temperature rises, minerals such as andalusite or chiastolite increasingly occur.
4.
There are several theories regarding the formation of the chiastolite cross, however the most widely accepted theory, proposed by Frondel in 1934, suggests that there is a selective attachment of impurities at the rapidly growing corners of andalusite crystals.
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