Published online by Cambridge University Press: 14 March 2018
The results are presented of some recent feldspar studies that relate the fundamental concepts of order-disorder series to petrological problems. New diagrams have been prepared with coordinates ‘optical properties-chemical composition-structural state’. From direct observations made on natural minerals some conclusions have been reached about the sequence in which the solid-state transformations of ordering, unmixing, and twinning occur in feldspars.
A study has been made of the geological distribution of different structural types of alkali feldspars in single intrusive bodies (Tertiary granite, Palaeozoic syenite, Pre-cambrian charnockite), in magmatic complexes, and in different complexes of the Ukrainian Shield and the Caucasus Geosynclinal Province.
page 298 note 1 See references in papers of the Feldspar-Symposium in Cursillos y eonferencias, Instituto ‘Lucas Mallada', 1961, Fasc., Madrid
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page 299 note 7 In labradorites it is only possible to observe one optic axis by inclining the universal stage when the trace of the (010) cleavage is visible and the twins are not superposed.
page 300 note 1 C. Burri and E. Wenk, Feldspar-Symposium, Cursillos y conferencias, Instituto 'Lucas Mallada', 1961, Fasc. 8, :Madrid.
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page 302 note 1 The common axis of the individual indicatrices may, of course, beα,β,or γ;ά,β́,γ ́,,α ́,and a’all lie in the plane normal to this common axis.
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