Summer Program on DIOS AU33WEST Gold Project
13 June 2014 - 1:39AM
Marketwired
Summer Program on DIOS AU33WEST Gold Project
MONTREAL, QUEBEC--(Marketwired - Jun 12, 2014) - Dios
Exploration Inc. (TSX-VENTURE:DOS) plans to undertake field work
(including prospecting, mapping, trenching) on wholly-owned
AU33WEST gold property, a few km from the Eastmain-1 hydropower
facilities, James Bay area, Quebec.
Main target focus will be the extent of the Héberto gold showing
that assayed up to 5 g/t Au over some 5 meters in diamond saw
track-sampling. This gold showing is coincidental with a weak
induced polarization conductor (chargeability) north-south striking
along the margin of a sub-circular magnetic anomaly, itself
included within a larger low magnetic structure. Several gold soil
anomalies are also coincidental with induced polarization
conductors. A structurally-controled oxidized IRG (Intrusion
Related Gold) model is proposed for the AU33WEST gold
project.
A felsic (tonalite-granodiorite) intrusive complex hosts several
gold porphyry-type showings (grading from 1.77 to 23 g/t Au in grab
samples) within a 5,0 by 2,0 km area at the head (up-ice) of a
significant gold glacial dispersal train. The gold mineralization
appears as 1-5% pyrite as disseminations and fracture fillings that
are associated with potassic alteration and/or silicification. It
appears structurally controlled by zones of shearing and foliation
along two main orientations (N160 and N080E).
Recent compilation of the AU33W data show good correlation
between gold and presence of pyrite, (of chalcopyrite) and/or
magnetite-hematite (oxidized system) located at the margins of
intrusions. The intrusions are interpreted from total field &
vertical gradient magnetics and geological mapping. These
associated mineralizations are enclosed within large halos of
potassic feldspar, silica, epidote, magnetite-biotite and hematite
alterations. The juxtapposition of structural measurements and
magnetic data suggests the presence of buried intrusive domes
within the mineralized and altered area which is mainly developped
along a north-south structural vector in the plutonic domain. The
concentration of sulfidic mineralization along the margins of
distinctive magnetic intrusions is also coincidental with higher
potassium content (ground spectrometry).
This news release was prepared by M. J Girard, M.Sc. Geo, the
Qualified Person (43-101).
Neither the TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in the policies of the TSX
Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
www.diosexplo.com
http://blog.diosexplo.com/
Marie-Jose Girard, M.Sc. GeoPresident &
CEOmjgirard@diosexplo.com(514) 923-9123
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