UPDATED : MAY 17^th 2021

PROJECT

Dollier

STATUS

Exploration drilling to explore extensions of the Dollier Gold Deposit.

COMMODITIES

Gold (including copper, silver and zinc concentrations)

LOCATION

30 km south-south-east of Chibougamau, Quebec (Figure 1)
Township : Dollier
Map sheet SNRC 32G09
Latitude : 49° 41′ 5″ N
Longitude : 74° 7′ 17″ W

CLAIMS STATUS

The property consists of 40 map staked contiguous cells (Figure 2) covering an area of 2,228 hectares.

OWNERSHIP

Cartier Resources has 100% ownership.

ROYALTIES

No royalties outstanding.

KEY POINTS

• Dollier Gold Deposit is composed of three zones (Figure 5) : Delinel Zone, North Delinel Zone and South Delinel Zone ;
• 40 drill holes for a total of 5 859 m were completed on Dollier Gold Deposit ;
• Best Results Figure and Table.

UPDATED : November 5^th 2015

CHARACTERISTICS OF THE CENTRAL AREA

• The Central Area of the property includes the Dollier Gold Deposit that is composed of three zones (Figure 5)  (Delinel, North Delinel and South Delinel). The characteristics are the following : Orientation : N065°- N245°, Dip of 70° south-south-east (Figure 6), Plunge : 65° south-south-west, Inter-zones distance : 50 m and Mineralisation: Disiminated to massive pyrite-pyrrhotite (Pictures 1 and 2) with localy disiminated chalcopyrite ;
• Best drilling intersections are presented in the Best Results Table and on Figure 9 ;
• Drill holes were drilled to 260 m depth on the Dollier Gold Deposit and potential remains open along strike and at depth (Figures 5, 7, 8 and 9) ;
• 40 holes totaling 5,859 m were carried out on the three gold zones Delinel, North Delinel and South Delinel (Falconbridge Cooper, 1976, Cartier, 2011 and 2014) ;
• The central part of the property has 46 holes totaling 6,911 m (Falconbridge Copper, 1976 ; Cartier, 2011 ) ;
• Ten trenches totaling 4,017 m2 (Cartier, 2009-10) show the deformation corridor and mineralised zones (Pictures 3 and 4). The best results are 9.2 g/t Au over 1.1 m including 3.9 g/t Au over 3.2 m (Delinel) and 3.6 g/t Au over 1.1 m (Delinel North) ;
• Delinel Gold Zone is associated with altered sericite marked enrichment K2O (Figure 8) ;
• The three mineralised zones are conductive and chargeable (EM and IP surveys, 2009-10) ;
• 131 chargeability anomalies were identified and grouped into 15 separate zones (IP survey, Cartier, 2010) ;
• 36 electromagnetic anomalies were generated by the helicopter EM survey (Cartier, 2009) (Figure 4).

CHARACTERISTICS OF THE EASTERN AND WESTERN SECTORS

The eastern and western sectors of the property include 5 holes totaling 665 m (Falconbridge Cooper, 1976; Cartier, 2011) ;

86 electromagnetic anomalies were generated by the helicopter EM survey (Cartier, 2009; Figure 4).

HISTORIC WORK

1972

Questor Surveys Ltd completes an INPUT MK V regional aerial survey for the MRNF ;

1974

Rio Tinto Canadian Ltd completes aerial magnetic and electromagnetic surveys. Exploratech Ltd realises a ground magnetic survey totaling 16 km for Falconbridge Copper Ltd ;

1975

Falconbridge Copper Ltd completes a ground electromagnetic survey with RADEM receptor of 83 km. Many conductive zones were outlined ;

1976

Falconbridge Copper Ltd completes 5 drill holes on the conductive zones totaling 466 m. The best result (74A-12) was obtained, on the west shore of the Delinel Lake, 1.10 g/t Au over 2.4 m in an amphibolitic rock containing 15% pyrite ;

1997

Explorateurs-Innovateurs de Québec Inc. completes a beep-mat prospecting survey.

PROPERTY ACCESS

The Dollier property is located 61 km south-south-east of the town of Chibougamau (Figure 1). The access is afforted using road number 167 which links Chibougamau to the Lac Saint-Jean and by a network of forestry roads that cross the property.

GEOLOGICAL SETTING

The property is located within the eastern part of the Abitibi subprovince which is itself included in the Superior province. It is located in a NE-SO oriented volcanic rock pile which belongs to the Roy Group, along the Palmer-Tippecanoe deformation corridor. The geology of the area has been defined by Pilote et al. (1996) and Roy et al. (2006) (Figure 3). The rocks have been regionally folded and metamorphosed to the amphibolite grade. The rock layers are parallel to the regional schistosity and have a nearly sub-vertical dip.

On the Dollier property, most rocks are volcanics of mafic to felsic composition and have affinities ranging from tholeitic (Obatogamau Formation) to calc-alcaline (Waconichi Formation). Along the southern limit of the property, the Boisvert tonalitic pluton cuts the volcanic units. In this area, volcanics have gneissic and migmatitic textures and they are cut by tonalitic dykes.

WORK COMPLETED BY CARTIER

2006-07

• Staking of Dollier property ;
• Beep-mat prospecting survey, 61 grab samples and 44 lithogeochemistry and alteration samples were collected ;

2008

• Beep-mat prospecting survey, 60 grab samples were collected ;
• Discovery of several outcropping massive sulphide horizons ;

2009

• Beep-mat prospecting survey, 43 grab samples were collected, 72 channel samples and 2 lithogeochemistry and alteration samples ;
• 3 trenches for a total of 1,746 m², 231 channel samples collected (best channel returned 9.2 g/t Au over 1.1 m) and 16 lithogeochemistry and alteration samples. Structural and geological mapping.
• Discovery of Delinel and North Delinel Zones ;
• 1/10 000 aerial photo coverage the property area ;
• 530 km heliborne Mag-EM survey ;

2010

• Beep-mat prospecting survey, 41 grab samples, 21 channel samples and 4 lithogeochemistry and alteration samples were collected ;
• 7 trenches for a total of 2,271 m², 241 channel samples were collected and 11 lithogeochemistry and alteration samples. Structural and geological mapping.
• Outline of Delinel and North Delinel Zones ;
• 24 km of cutting line, 20 km IP survey with 50 and 100 m line spacing, dipole-dipole array (a = 25 m and n = 1 to 6) ;

2011

• 29 drill holes for a total of 3,275 m to test the Delinel and Delinel North, 2,555 core samples for metals assaying and 488 lithogeochemistry and alteration, best interval for the Delinel Zone returned 13.3 g/t Au over 1.2 m and best interval for the North Delinel Zone returned 11.2 g/t Au over 0.3 m ;

2014

• 13 holes totaling 3,470 m, 29 mineralised intersections cuted over lengths varying from 23.0 to 0.6 m, best value on the Delinel Zone = 25,1 g/t Au over 1.0 m, best value on the North Delinel Zone = 5.0 g/t Au over 1.0 m. The following samples were collected : 1,300 for Au, 71 for Zn, Cu, Ag, 17 for multi-elements and 100 for lithogeochemistry and alteration.

WORK PLANNED

CENTRAL PART OF PROPERTY

Prospecting and stripping

• Beep-mat survey along the chargeability zones defined by the IP anomalies (Figure 5) ;
• Mechanical stripping on the best targets identified by surveys.

Drilling SEEEKING A PARTNER TO DRILL

• Drilling to explore the depth extensions of the Dollier Gold Deposit (Figure 9).

EASTERN AND WESTERN SECTORS OF THE PROPERTY

Geophysic surveys :

• 50 km line cutting, 50 km of IP survey and 65 km of magnetometer survey to identify new mineralised zones (Figure 4).

Prospecting and stripping

• Beep-mat survey along IP anomalies chargeability trends ;
• Trenching program on best targets.

Main results

• Zone aurifère Delinel Section longitudinale Download
• Meilleurs résultats Download
• Figure 1 - Property Location Download
• Figure 2 - Claims Map Download
• Figure 3 - Local Geology Download
• Figure 4 - EM & Mag Surveys Download
• Figure 5 - Plan and Longitudinal Section Dollier Gold Deposit Download
• Figure 6 - Transversal Section Delinel Gold Zone Download
• Figure 7 - Longitudinal Section Delinel Gold Zone Download
• Figure 8 - Longitudinal Section Au & K Correlation Download
• Figure 9 - Delinel Gold Zone Longitudinal Section Download
• Picture 1 - Massive Pyrite Delinel Gold Zone Download
• Picture 2 - Massive Pyrite & Pyrrhotite Delinel Gold Zone Download
• Picture 3 - Stripping Delinel Gold Zone Download
• Picture 4 Stripping Delinel Gold Zone Download

Other documents

• Delenel Gold Zone Longitudinal Section Download