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extent in inter-digitated gabbro-clinopyroxenite units. The West Zone only has
limited exposure by underground workings, and consists of multiple mineralized units
which are separated spatially; the basal gabbro unit, the upper clinopyroxenite unit,
and a second basal unit which lies to the west of one of the several westerly shallow
dipping north-easterly trending cross-faults.
The sill that hosts the mineralized West Zone appears to have a gabbroic margin on
both its north and south contacts. The marginal gabbro magmatic zones are up to
110 m thick. They host the nickel-copper massive sulphide mineralization that forms
the higher grade portions of the various mineralized zones of the Wellgreen deposit.
The clinopyroxene magmatic zones, which range up to 100 m in thickness, host
disseminated nickel-copper sulphides and minor net-textured and semi-massive
sulphide lenses (Figure 7.5).
Prophecy Platinum Corp. 7-7 1193460500-REP-R0001-02
Wellgreen Project Preliminary Economic Assessment,
Yukon, Canada