RE: Help!!!
The ReMac property occurs in a series of carbonate hosted base metal deposits and prospects exposed over a distance of some 4 Km referred to as the Reeves-Red Bird corridor. The most significant mineralization is hosted by dolomitized limestone of the Reeves Member of the Lower Cambrian Laib Formation. The base metal zones are in the form of elongated lenses typically 100-200m long, 5-25m wide and extend over 1000m down plunge (before faulting).
Historic mining records indicate extraordinary continuity in size and grade over these dimensions. There are four, and possibly five, known zones of mineralization, typically striking E to ENE, dipping 50-60º S and plunging 45-60º W. The zones have been offset by a number of east dipping normal faults that repeat them several times to produce a series of distinct zinc deposits.
There is the potential to develop significant mineral resources on the property. In 1999 a report by R.D.Westervelt indicated a historical sulphide resource of 443,000 tons grading 5.35% Zn and 2.45% Pb remaining in a zone immediately below the previous Annex mine workings. This sulphide resource represents a portion of the total sulphide potential based on the current geological model, which suggests that normal faulting has brought the major sulphide units closer to surface, thereby providing prime exploration targets. In addition there is significant resource potential in all the oxide zones recognized on the Reeves and Red Bird properties.
It should be noted that the historical sulphide resource estimate is not compliant with