Abstract
The mineralogical distribution of gold in samples from the Corvo orebody, in the Iberian Pyrite Belt of Portugal, was determined in a detailed study of a few hand samples of RT ("rubane tin") ore. In one sample, 42% of the gold occurs invisibly in pyrite I, pyrite TT, and arsenopyrite, with the balance assumed to be carried by cassiterite, which makes up 56.5 wt.% of the sample. Extrapolation of these results to a sample of high-grade tin concentrate (68.99 wt.% Sn) suggests that cassiterite in the concentrate contains about 149 ppb Au, representing 88% of the total gold in the concentrate. These results have implications on the metallogeny of the Neves-Corvo volcanogenic massive sulfide deposit as well as on the metallurgical treatment of the ores.
Original language | English |
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Pages (from-to) | 1347-1360 |
Number of pages | 14 |
Journal | Canadian Mineralogist |
Volume | 36 |
Publication status | Published - 1998 |