The mineralogical distribution of gold in samples from the Corvo orebody, i
n the Iberian Pyrite Belt of Portugal, was determined in a detailed study o
f a few hand samples of RT ("rubane tin") ore. In one sample, 42% of the go
ld occurs invisibly in pyrite I, pyrite TT, and arsenopyrite, with the bala
nce assumed to be carried by cassiterite, which makes up 56.5 wt.% of the s
ample. Extrapolation of these results to a sample of high-grade tin concent
rate (68.99 wt.% Sn) suggests that cassiterite in the concentrate contains
about 149 ppb Au, representing 88% of the total gold in the concentrate. Th
ese results have implications on the metallogeny of the Neves-Corvo volcano
genic massive sulfide deposit as well as on the metallurgical treatment of
the ores.