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structure of FeS (NiAs) remains when the O atoms are added to form Fe[SO
4
] and
persists, in FeLi[PO
4
], when the Li atoms are present. Through this dissection, it is
evident that the structures are not a mere set of spheres, mainly dominated by their
size, but atoms arrange in a concerted manner so that each atom provokes (influ-
ences) the formation of the structures of the others, always leading to structures of
recognizable simpler compounds.
The phase transition triphylite
! b
-FeLi[PO
4
] can now be understood by the
need of a PbO-type
NiAs transition in the [FeP] subarray. Once again, we can
state that cations govern the structures and that they undergo their own phase
In view of this, we feel necessary to claim again for the statement of Won-
dratschek, Merker and Schubert [
12
] heading this article. The principle seems to
be the EZKC.
!
Acknowledgements I am indebted to my colleagues David Santamar
´
a-P
´
rez and Javier Garc
´
a
for their patient reading of the manuscript and valuable suggestions.
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¼