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dios exploration inc (DOS) Details

Dios Exploration Inc., a mineral research company, operates as a mining exploration and evaluation company in Canada. It focuses on exploring gold, uranium, diamonds, and a carbonatite with rare earth and niobium metals. The company holds interests in various properties comprising 5,300 mining claims covering approximately 2,750 square kilometers in the areas of central Quebec and the Otish Mountains. Dios Exploration Inc. is based in Montreal, Canada.

dios exploration inc (DOS) Top Compensated Officers

Chairman, Chief Executive Officer, President ...
Total Annual Compensation: C$145.0K
Chief Financial Officer and Director
Total Annual Compensation: --
Compensation as of Fiscal Year 2013.

dios exploration inc (DOS) Key Developments

Dios Exploration Inc., Annual General Meeting, Jun 25, 2014

Dios Exploration Inc., Annual General Meeting, Jun 25, 2014., at 10:30 US Eastern Standard Time. Location: Marriott Château Champlain, Huronie Room. Agenda: To present to shareholders the financial statements of the Corporation for the year ended December 31, 2013, as well as the auditors' report; to elect the Corporation's directors; to appoint the auditors and to authorize the Board of Directors to establish the auditors' remuneration; to pass a resolution reconfirming the Shareholders' Rights Plan; and to transact such other business that may properly come before the meeting.

Dios Exploration Inc. Updates on Fall-Winter Work on DIOS 33 Carats Gold

Prospecting, geological mapping and soil sampling by helicopter over the last two years by DIOS EXPLORATION delineated a highly prospective area for gold within a felsic intrusive, at the head of a gold-in-till dispersal train on wholly-owned 33 CARATS project, along road 167 north of the town of Chibougamau, Quebec, 40 km south of the Renard diamond deposit and 6 km northwest of the Eastmain Mine gold deposit (1.0 million tons grading 15.3 g/t Au, 15.1 g/t Ag and 0.27% Cu). DIOS' Bohier tonalite hosts numerous porphyry-type gold-silver-copper-bismuth showings associated with a magnetic low. The head of the gold glacial train points to the low magnetic anomaly within the Bohier tonalite (a 3.5 by 1.5 km area). First gold-bearing tonalite outcrops were discovered in summer 2012. With recent road access this Fall, a first drill program was undertaken to locate the source of some mineralized boulder trains and to drill-test some surface showings within the Bohier tonalite on dry ground accessible from the road. A total of nine exploratory diamond drill holes totaling 1332 m were completed on 33 CARATS SOUTH claims. The drill program specifically targeted weak to high magnetic lineaments within the magnetic low. Drilling was divided into two parts, with a two km area between the two remaining untested due to lack of access, focusing first on the northern part of the low magnetic anomaly within the tonalite, where 10 metric intervals greater than 100 ppb Au were intersected in three different holes: 13-01, 03 & 04. The best cut returned 1.14 g/t Au, 2 g/t Ag & 0.12% Cu over 3.0 m (210.35-204.35 m) in hole 13-01. Wide zones of potassic (biotite- potassic feldspars) and propylitic (epidote) alteration were intersected in holes 13-01 & 03. The second part of the drill program targeted the Shower Cap area some two km to the south, located at the southern limit of the low magnetic anomaly. Hole 13-07 was drilled directly underneath the Shower Cap showing to a total depth of 111 m and returned 3 intervals greater than 1.0 g/t Au: 1.38 g/t Au, 1.7 g/t Ag & 0.15% Cu over 0.5 m (19.00-19.50 m), 1.09 g/t Au, 1.2 g/t Ag & 0.13% Cu over 1.5 m (25.25-26.75 m) and 1.3 g/t Au over 1.0 m (100.00-101.00 m). The company recalled the Bohier tonalite hosts numerous showings associated with porphyry-type mineralization in outcrops (up to 4.93 g/t Au, 6.8 g/t Ag & 0.477% Cu) and in metric boulders (up to 7.76 g/t Au, 17.8 g/t Ag & 1.5%). A two km long area within the heart of the magnetic low could not be drill tested this fall. During the drill campaign, further prospecting & geological mapping was also conducted in the vicinities of the drilling sites. About 100 m west of Shower Cap, a metric tonalite boulder returned this year 7.63 g/t Au, 16.5 g/t Ag, 0.64% Cu & 72 g/t Bi. Some 500 m west of Shower Cap, another similar mineralized boulder (found in 2012) returned 6.11 g/t Au, 3.7 g/t Ag, 0.35% Cu. Mineralization comprises disseminated traces-1% PY-CPY-MC associated with 2% (mm up to 4 cm wide) quartz veins, hosted within a moderately silicified non-magnetic tonalite. The presence of these boulders indicates that a 500 x 500 m area located north of Shower Cap between drill holes 13-07 & 13-08 remains highly prospective. The whole area is non-outcropping and covered with swamps. About 100 m south of drill holes 13-01 & 02, a metric boulder returned this year 5.62 g/t Au, 7,3g/t Ag, 1,48% Cu, 4g/t Bi & 94 ppm Mo within a silicified tonalite. The source of this boulder is under a swampy area that was not tested during the 2013 drill campaign because of the field conditions. Another metric boulder located approximately 350 m south graded 7.33 g/t Au, 14.5 g/t Ag, 0.63% Cu & 74 g/t Bi.

Dios Exploration Inc. Reports the Completion of the First Nine Holes Drilled for Gold Totaling 1,332 Meters on 33 Carats Gold Porphyry Project

Dios Exploration Inc. reported the completion of the first nine holes drilled for gold totaling 1,332 meters on wholly-owned road-acessible 33 CARATS gold porphyry project, north of the town of Chibougamau, James Bay, QC. This fall prospecting program also uncovered new mineralized outcrops of tonalite with disseminated chalchopyrite and as in-fillings in association with hematization zones some 500 m farther away than the last known mineralized otucrops. Several mineralized boulders were also discovered down-ice. Holes were drilled over approximately a 2.5 km north-south length and over 500 m east-west. A significant biotitisation zone (potassic alteration targeted for by this drilling for such a gold deposit) some two km by 300-400 m was defined and interpreted. Biotite alteration is intense and pervasive and can be disseminated or in veinlets. Epidote alteration can also be noted in association with hematization zones. Propylitisation zones are typical of porphyry deposits. Detailed core logging is completed and core split in two already sent to ALS-Chemex laboratory, Val d'Or for assaying, results pending. Several drill holes intercepted multiple several meter zones of mineralized tonalite with disseminated copper sulfides (up to 1 % chalcopyrite), 1 to 2 % pyrite (iron sulfide) (gold indicators in this gold porphyry context), as well as silicified zones and hematized ones, and furthermore, chalcopyrite stringer zones, biotite stringer zones, and carbonated zones in places.


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