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Figure 3a. Optical stereomicrograph of a millimeter sized geode within
the granophyre from Cuasso al Monte. (a) The large orange crystals
forming most of the mineral association are K-feldspar; lamellar
translucent crystals as in the lower left are albite (which also forms
overgrowths on K-feldspar); the translucent mineral with botryoidal
appearance at the center is fluorite and the translucent, faceted grain
above fluorite is quartz; dark crystals are chamosite and anatase in granular
aggregates. Chamosite forms lamellar, black-greenish grains.
By Capitani, Mugnailoi, and Gentile. http://dx.doi.org/10.2138/am-2017-6242