The Argyle-Wolf (Creek vein) occurrence is located near the junction of Sheep and Waldie Creeks on the Argyle (L.10155) and Wolf (L.3856) Crown grants.

The area is underlain by sedimentary rocks of the Cambrian Laib Formation and Ordovician Active Formation, which have been intruded by granodioritic rocks of the Cretaceous Anstey Pluton.

Locally, as defined by drilling in holes 88-2 and 88-3, the Creek vein comprises a steeply south dipping, quartz-pyrite-pyrrhotite vein. Other drill holes in the area (88-1 and 88-6) intersected narrow quartz-pyrite veins and zones of shattered quartz with up to 20 per cent pyrite-pyrrhotite.

In 1988, IMCO Resources Ltd. completed eight diamond drill holes, totalling 1114.6 metres, on the Argyle (L.10155) and Wolf (L.3856) Crown grants area. Drill holes 88-2 and 88-3 are reported to have yielded intercepts of 27.42 and 14.26 grams per tonne gold over 0.61 metres each, respectively (Lane, R.A. (2017-08-17): NI 43-101 Technical Report on the Sheep Creek Project). The exact location of these drill holes is not known.