very interesting @mode1971, just skimmed the 2011 Anglo report on the Dido tenement EMP15915, confirms exactly what Peter has reported.
brief extract from one section of the report
Current drilling has to date only tested two of the known mafic-ultramafic intrusions in the area. Whilst the diamond drilling program did not intercept economic Ni-Cu-PGE sulphide mineralisation, the results are considered to be very significant in that:
The drilling confirmed that the “right rocks” are in the region – the presence of troctolites, pyroxenites, **bronorites and other mafic rocks are also associated with large scale NiCu-PGE magmatic sulphide ore-bodies like Voisey’s Bay.
The other interpreted mafic-ultramafic intrusions in the region are likely to have similar lithologies.
The presence of sulphides, evidence of wall rock contamination and magma mixing (as indicated by magmatic vari-textures) is extremely encouraging as they are key features of other magmatic Ni-Cu-PGE ore systems.
Similarly, the geochemistry indicates that some magmas are nickel depleted, indicating that sulphide trapping and accumulation is likely to have occurred somewhere in the region.
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