Very anomalous gold in outcrop area
April 27, 2016
Dios acquires new Clarkie gold project in Opinaca area
MONTRÉAL, QUEBEC, CANADA –DIOS EXPLORATION acquires the new gold CLARKIE property with strong gold potential north of Eastmain Clearwater gold deposit and southeast of Eleonore Goldcorp gold mine and Cheechoo recent gold discovery in metasediments. A significant gold-bearing glacial train indicates an up-ice source area hosting folded Clarkie sediments, interpreted as equivalent (same age sediments) to those hosting Eleonore gold mine.
Other favourable features such as diorite intrusions, porous sediments, fold closures and northwest structures are good physical traps for gold noted on newly map-staked claims (70 square km) close to strategic regional Opinaca-LaGrande contact.
DIOS outlined this gold-in-till train (16 x 4 km) including 14 samples over 100 ppb gold and five samples over 600 ppb gold (from heavy mineral concentrates). DIOS’ team is looking forward to explore these high gold potential sediments this summer.
Recent DIOS’ Heberto Gold discovery came from searching the source of such a gold glacial sand dispersal train. The goldbearing Bohier tonalite along highway 167 was also discovered searching the source of yet another gold train delineated by Dios’ proprietary work data. This press release was prepared by Harold Desbiens, M.Sc. Geo 43-101 QP.
April 21, 2016
Dios hits 3.65 g/t gold over 13 meters within a 60 m true thickness grading 1.21 g/t gold in Heberto tonalite
MONTRÉAL, QUEBEC, CANADA –Management of DIOS EXPLORATION is very pleased to report first results received from 2016 recent drilling on wholly-owned HEBERTO. Hole 19 cut 3.65 grams gold per tonne over 13 m (71 m-84 m)in a 64 m true thickness interval grading 1.15 g/t gold from 68 to 132 m on HEBERTO.
Recent 2016 drilling targeted vicinities of HEBERTO gold showing and checked the N160 degrees goldbearing corridor over a 700 meter strike length. That goldbearing structure consists of several meters thick potassic altered shear zones with traces-4% pyrite (traces magnetite) in a large granodiorite/tonalite pluton. DIOS is looking for a significant worldclass oxidized IRG gold deposit. Enriched gold content in association with pyrite and magnetite confirm that model deposit.
This is promising because of pyrite and magnetite associated with gold on HEBERTO. The first gold zone in hole 19 (from 71m to 84m) has 3-5% pyrite-magnetite (hematite-quartz-biotite) stringers/veinlets and the second one from 92-128 m has potassic shears with 1-3% disseminated pyrite (magnetite). Gold zones can be followed in strike and dip. Hole 19 is located 50 m south of holes 2015-01 (2.13 g/t gold/22.9 m), 2015-09 (2 g/t gold/22 m) and 2015-10 (1.63 g/t gold/18.45 m). Hole 19 is also located 50 m north of hole 2015-06 (1.94 g/t gold/7.75 m) and 112 m west of hole 2015-01.
DIOS 2016 Heberto 1532 meter eight drill hole program tested 8 targets. Further assays and re-assays are pending and will be released in the coming weeks for other holes. HEBERTO major km scale gold system is located within a 5 X 8 km highly anomalous gold-in-outcrops area, 50 km south of Goldcorp’s Eleonore world class gold mine and 20 km west of Clearwater gold deposit, James Bay Eeyou Istchee, Quebec.
Samples were bagged and sent to ALS-Global laboratory in Val D’Or, Quebec: 616 samples (559.5 m of core) were sent for gold assays (Au-AA23) with 52 inserted blanks (certified barren quartz) for quality control. Technical data was reviewed by Harold Desbiens, M.Sc. Geo 43-101 QP.
To see the MD&A please click here.
A gold interest zone of a few sq. kilometers of homogeneous grayish granite (tonalite) with some sixty disseminated copper sulfide bearing samples.
A clear gold-silver-copper-bismuth association typical of gold porphyry deposits. The style of mineralization (disseminated, not vein-hosted) and metal association suggest potential for a low-grade bulk tonnage porphyry gold deposit.
Five main gold anomalies (including 30 samples exceeding the 99.8 percentile gold in humus) were outlined over a non magnetic 4.5 x 2 km tonalitic phase. The gold anomalies appears N-S to NNE oriented and extend from 300 to 1 500 meters. They are also located adjacent (and up-ice) of goldbearing metric floats grading up to 7.76 g/t Au and outcrops grading up to 4.93 g/t Au.
Sub-parallel to the gold anomalies, two 3 km-long copper humus anomalies are coincidental with the magnetic/non-magnetic tonalite contact and the non-magnetic tonalite/magnetic granodiorite contact. Assays from previous rock-sampling confirmed a good gold-copper correlation. These gold soil anomalies are located within one to two kilometres of the new #167 road.
Dios Exploration and its partner Osisko proceeded this fall with surface work on the AU33 West gold project (see October 24, 2012 post).
Dios Exploration recently reported good news after first assay results.
Ten trenches were dug up to test soil geochemical targets or to extend known gold mineralized occurrences.
The best results come from the Héberto occurrence, in a mylonityzed tonalite, a granite type. The results returned grades as follows :
It is important to note that analysis within the tonalite was realized withinan homogeneous rock and not in veins (eg. Quartz). This could suggest interesting gold mineralization tonnage.
Other anomalous results from 0.5 to 1.1 g/t in gold on brackets of 0.75 to 2.25 m were as well obtained on other trenches.
These trenches allowed a good exposure of the mineralized occurrences and a better understanding of the vectors in place controlling the mineralization.
Remember that Osisko is a major partner who can acquire 51% of the AU33 WEST property. This partner has to incur 5,000,000 $ in exploration and 700,000 $as payments over 5 years.
The work previously mentioned is part of this partnership and is funded 100% by Osisko
Later on, if Osisko desires, an additonnal participation of 9 % is possible with further work of 9,000,000 $ over 5 years. Another 10 % is as well available with the financing of a feasibility study.
Osisko is a worldwide mining corporation based in Montreal for aquisition, exploration, developpement, and exploitation of auriferous properties.
Some photos of the work (click to enlarge)
Dios Exploration announced on September 24th, that two backhoes were moved this Fall on AU 33 WEST Gold Project.
This is major work for this project.
The trenching work is taking place this fall. Detailed rock sampling was undertaken and rocks to be assayed. The results will soon be published…
Why all this agitation? Because Dios Exploration :
The best summer 2012 sampling results of rock outcrops and soils sustain such enthusiasm:
Geographically, the project is located a few hundred kilometers north north-east of Matagami. Geologically, it is located in the Opinaca Eastmain emerging gold camp , some 60 km away from the world class Eleonore gold deposit developed by Goldcorp.
Other recent information on AU33 West Gold Project:
We will keep you informed on the upcoming news about this project.
Recent exploration in a part of this project highlighted a gold and copper zone.
Works allowed targeting of a 2-3 km by 8 km sector of a tonalite (grey granite) phase with good gold potential.
The geological model applied is a porphyry-type, characterized by a gold-silver-copper-bismuth association.
It is the model wanted
The interesting minerals are gold and copper. The rock basement is a mildly mineralized tonalite.
This nonetheless offers excellent potential for a high tonnage gold mine, similar to the Malartic gold mine.
This mine, which has been exploited for many years, extracts rocks with average grade of 1 g/t.
On the 33 CARATS project, Dios discovered on surface the following:
Of the 60 analyzed samples containing disseminated copper sulfides, 26 had gold grades superior to 0.463 g/t.
The 33 CARATS project is wholly owned by Dios. At the moment, this project is one with the best mining potential. It is very promising and the future 167 road will cross through these claims.
To properly outline the more highly mineralized zone, 1 200 organic earth (humus) samples were already collected (soil-geochemistry).
Soils feed on proximal metals. Therefore it is possible to extrapolate analytical results from the rock basement.
If high concentrations are recurring, it could possibly outline excellent drilling targets.
According to precise planification to determine, these drillings could be done in 2013.
Summary of activities from April to June 2012
Exploration expenses totalling $420,069 on Shipshaw and Shadow properties, as follow:
Shipshaw (Niobium and Rare Earths):
Shadow (Diamond and Gold):
Au 33 West property (Gold):
Another project, entirely financed by Osisko. They realized two exploration campaigns with a field team of 6 people. A new soil survey was completed and a detailed rock sampling of outcrops located in the centre of the property where mineralized occurrences were discovered in 2011. Follow up is planned in the upcoming weeks.
CASH FLOW SITUATION
The working capital increased by $76,480 during the second quarter going from $1,802,567 as at March 31, 2012 to $1,879,047 as at June 30, 2012. The increase is mainly due to the reallocation from non-current investments to current investments and an option payment of $75,000 received during the quarter.
The Company considers the cash on hand sufficient for the known obligations. As at June 30, 2012, the Company did not have any debt or any financial commitments in the upcoming quarters.
Porphyric type gold 33 Carats project returns 60 tonalite samples with disseminated copper sulfides
33 CARATS: Upper Eastmain area, James bay, Northern Quebec
Located NW of the Eastmain gold mine, this project encloses granodioritic-tonalitic rocks with disseminated chalcopyrite (copper sulfide)-pyrite mineralization and quartz veins which show potential for gold porphyric mineralizations.
In July-August 2012, Dios completed a spectrometry and prospecting-mapping follow-up (325 rock samples with sixty disseminated copper sulfide bearing samples) targeting the tonalitic phase of Erasme Lake intrusive. There is a clear gold-silver-copper-bismuth association typical of gold porphyry deposits.
Dios has also just completed a soil sampling (1200 humus samples) in the same area to find drill targets.
Many tonalitic glacial boulders returning between 1.0 and 3.2 g/t Au discovered last Fall by Dios are located up ice of a gold in till train (252-2,090 ppb Au).
The Otish Mountains road which will go to the diamond Renard deposit passes through the prospective area of the soil grid.
14 KARATS: 50-75 km NE of 33 Carats
During the same period, Dios undertook prospecting-mapping on this project located between the Leran- Patamisk lakes.
It covers a volcano-sedimentary sequence at the contact of sub-provinces La Grande (equivalent) and Opinaca and up ice of the gold in tills (356, 534, 583, 642, 1160, 2230 ppb Au).
Almost 230 rock samples were grabbed and sent to laboratories and was also completed a glacial till sampling (69 samples) program.
SHADOW : Opinaca-Eastmain 1 – Lower Eastmain area, James bay, Northern Quebec
A summer exploration program on the southern part of this gold project was completed in the Eastmain-1 sector.
It comprises soil sampling (1300 humus samples) and prospecting-mapping (53 rock samples). It specifically targeted a volcano-sedimentary contact folded on the edge of a felsic intrusive, located up ice of many goldbearing tills (241, 983, 1120, 3510ppb Au).
LECARON: Shadow project adjacent
Dios plans other mapping-prospecting work on this gold project which will target more precisely a sector covering mafics volcanics up ice of gold tills (208, 236, 265, 285, 666, 921, 925, 1035 ppb Au) where 37 rock samples were taken in 2012.
A till sampling campaing (20 samples) was undertaken looking for other targets in the same area.
AU 33 WEST: same sector than Le Caron
Still in the same area, on this gold project, partner Osisko has completed a second year of soil samplings (140 samples of B horizon) and prospecting-mapping (364 rock samples with spectometry-K readings) which targeted porphyric mineralizations in the intrusive rocks.
More work is planned for the fall, results pending.
Rock samples were sent to the ALS-CHEMEX laboratories and IOS Géoscientifiques completed glacial till sampling in these area and also completed soil sampling for Dios.