The structures of two components of the decomposed solid solution of an alk
ali feldspar are refined. These structures exhibit at least two specific fe
atures: (1) the complete phase separation into pure K and pure Na phases an
d (2) an anomalous distribution of Al atoms over four crystallographically
independent positions of silicon-aluminum tetrahedra in the Na-component (d
ifferent from its usual distribution). To explain the results obtained, the
ideas of synergetics are invoked (the geological history of the specimen i
ncludes a powerful explosion, which threw out the material from the volcano
to the Earth's surface).