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Callinex Mines Inc V.CNX

Alternate Symbol(s):  CLLXF

Callinex Mines Inc. is a Canada-based company, which is advancing its portfolio of base and precious metals rich deposits located in established Canadian mining jurisdictions. The Company's projects include Flin Flon Area - Pine Bay, Flin Flon Area - Flin Flon, Nash Creek and Superjack, Point Leamington, and others. It owns a 100% interest in the approximately 6,795 hectares Pine Bay project. At Pine Bay project, the Company is focused on the advancement of the high-grade Rainbow Deposit and Descendent Deposit. Its Nash Creek project is located in the volcanogenic massive sulfide (VMS) rich Bathurst Mining District of New Brunswick. Its 100% owned Point Leamington Deposit in Newfoundland is located in one of the richest VMS and Gold Districts in Canada. Its Flin Flon project covers approximately 2,455 hectares. Its other properties include Gossan Gold, Sneath Lake property, Moak Lake property, Herblet Lake property, Headway property, Headway North claim, and the Island Lake properties.


TSXV:CNX - Post by User

Bullboard Posts
Post by lookin2retireon Nov 23, 2016 11:40am
213 Views
Post# 25502449

Drilling to the North East

Drilling to the North EastA second step-out drill hole, PBM-018, will commence when one of the drill rigs becomes available. PBM-018 will be located approximately 115m along strike to the northeast of hole PBM-017 and is designed to intersect the Cabin VMS Horizon at a similar depth.

In addition to the planned step-out drilling campaign, Callinex will also extend PBM-010, a drill hole recently completed by Callinex and located approximately 300m along strike to the northeast and 400m above the new discovery. This is one of the only holes drilled deeper than 315m near and/or along the Cabin VMS Horizon to the northeast of the new VMS discovery. PBM-010 encountered four separate copper intersections down to an approximate hole depth of 370m (See news release dated April 25, 2016). The intervals, which are interpreted as stringer-type mineralization, were spatially associated with semi-massive sulphides (primarily pyrite) and frequently with narrow black chlorite veins that collectively represent immediate footwall rocks to the Cabin VMS Horizon. This hole further indicates that a favorable VMS environment occurs to the northeast of the new discovery where very few deep holes have been completed.
Bullboard Posts