Two new occurrences of anduoite, (Ru,Os)As-2, a rare platinum-group mineral
(PGM), are reported from chromitites, one from the Kapitanov deposit, Ukra
inian Shield, Ukraine, and the other from the Maja e Sukes deposit, Tropoja
ophiolitic massif, Albania. At Kapitanov, anduoite occurs as discrete, hom
ogeneous, euhedral crystals (6-9 and 1-2 mum) enclosed in two chromian spin
el grains devoid of fractures. At Maja e Sukes, one crystal of anduoite (3
mum in diameter) belongs to a complex polyphase assemblage of PGM comprisin
g sperrylite, hollingworthite and an unnamed sulfarsenide of Rh, Ir, Pd and
Ni. The chemical composition of anduoite is comparable in both deposits: (
Ru0.79-0.80Os0.10-0.11Ir0-0.03Rh0.03-0.04Pt0-0.01Pd0.01-0.02Ni0-0.04)(Sigma
0.98-0.01)(As1.98-2.01S0.01-0.02)(Sigma1.99-2.03) These examples of anduoit
e have a lower content of Ru than that described from the type locality in
Tibet. A magmatic origin is proposed.