A geochemical study of the behaviour of zirconium in bauxites develope
d on alkaline rocks in southern Brazil is presented. Zirconium, genera
lly considered as an immobile element during weathering, shows an impo
rtant mobility conditioned to the original Zr bearing parent mineral.
In the two areas (Pocos de Caldas and Lages) zircon is rare and the zi
rconium bearing parent minerals are complex weathered silicates as ''g
iannettite'', eudyalite, astrophyllite, etc. Since the first stages of
weathering, zirconium is partially leached of from the bauxite profil
e and the remaining Zr is incorporated in secondary phases of the baux
ite (amorphous ferric oxydes and aluminous goethite). Copyright (C) 19
96 Elsevier Science Ltd & Earth Sciences & Resources Institute