The region of the concentration magnetic phase transition in a CuxZn1-xCr2S
e4 chalcogenide spinel in which the substituted ion concentration x smoothl
y varies from 0.1 to 0.2 with a step of 0.02 is thoroughly investigated. An
anomalous behavior of the Curie temperature is observed. This anomaly is a
ssociated with the nucleation of ferromagnetically ordered microregions in
the vicinity of Cr ions with an intermediate valence and subsequent long-ra
nge magnetic ordering at a critical Cu concentration in the range 0.12 < x(
c) < 0.14. The possible coexistence of ferro- and antiferromagnetism in the
same temperature range is revealed. (C) 2001 MAIK "Nauka/Interperiodica".