New data on golddistribution in the zonal metamorphic complex of andal
usite-sillimanite type are presented. The gold content in the metapeli
tic rocks of the Northern Priladozhye are corresponding to the average
gold content in the similar rocks from other regions of the world. Th
e lowest gold content is peculiar to the rocks of high temperature fie
ld of the amfibolitic facies. Host minerals and mineral phases of maxi
mal gold content are revealed. The redistribution of gold in main rock
forming minerals in the process of progressive metamorphism is demonst
rated. The dependence of gold content in biotite and stoichiometry of
the mineral is established, the latter being concerned as one of gold
concentrators.