Abstract
Chemical-optical and X-ray analysis of some perthite groups, from cristalline rock massifs, came into evidence that in perthites with the same order degree of Si/Al distribution, the observed variations of 2VX are strictly related to the Na content in the potassic phase; i.e. 2VX decreases when Ab mixed in the K-phase increases.
This fact suggests that for any Si/Al, distribution, not in equilibrium, exists a certain range of non equilibrium mixing between Or and Ab.
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Potenza Fiorentini, M. Non-equilibrium mixing in natural alkali feldspars. Contr. Mineral. and Petrol. 21, 1–8 (1969). https://doi.org/10.1007/BF00377415
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DOI: https://doi.org/10.1007/BF00377415