DOS Dios Exploration Inc

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 Heberto 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/

FOR FURTHER INFORMATION PLEASE CONTACT: 
Marie-Jose Girard, M.Sc. Geo
President & CEO
mjgirard@diosexplo.com
(514) 923-9123

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