Abstract
The coherent solvus and coherent spinodal for sanidine-high albite are reasonably well known from experimental studies. These relations together with experimental coarsening rates can be used to interpret the thermal histories of rapidly cooled cryptoperthites which are characterized by a coherent, lamellar microstructure. The lamellar spacing (λ) is largely dependent on the rate of cooling during the first 70°C after the sample has crossed the coherent spinodal; the compositional difference of the lamellae (∆C) is more dependent on the lower temperature history of these cryptoperthites.
The rate of change of both ∆C and λ is controlled by interdiffusion of the alkali ions. The diffusion path is normal to the lamellar boundary for the change of ∆C, whereas it is complex and much longer for lamellar coarsening. Hence even though both processes depend on alkali diffusion rates, lamellar coarsening is much slower. Experimental diffusion data indicate that alkali interdiffusion is anisotropic, independent of water pressure to at least 2 kbar, and independent of confining pressure to 15 kbar however, it is not known to what extent other components or impurities affect these rates. Ansvers to these questions, together with modeling of coarsening rates using diffusion data, are important areas of further research.
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Yund, R.A. (1984). Alkali Feldspar Exsolution: Kinetics and Dependence on Alkali Interdiffusion. In: Brown, W.L. (eds) Feldspars and Feldspathoids. NATO ASI Series, vol 137. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-6929-3_8
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