| Property Name | Chutine 14216.pdf
 
 | 
            
                | Location | 
                        
                            | NAD 83 | 57° 40' 59.00'' N, 131° 40' 07.00'' W 57.683056, -131.668611 UTM: Easting 340894, Northing 6396557, Zone 9 (North) |  
                            | NAD 27 | 57° 40' 59.39'' N, 131° 40' 00.80'' W 57.683165, -131.666889 UTM: Easting 340991, Northing 6396354, Zone 9 (North) |  
                            | NTS | 104G12E |  
                            | BCGS | 104G062 |  | 
            
                | Mining Divisions | Liard | 
            
                | Mining Camp |  | 
            
                | Title | Geochemical Report on the Chutine 1, 2, 3 Mineral Claims (Conover Creek), Liard Mining Division | 
            
                | Report Year | 1985 | 
            
                | Number of Pages | 38 | 
            
                | Statements of Work | n/a | 
            
                | Affidavit Date | 1985-02-28 | 
            
                | Off Confidential | 1986-02-28 | 
            
                | Claims | CHUTINE 1-3 | 
            
                | General Work Categories | Geochemical | 
            
                | Operators | Brinco Mining Limited 
 | 
            
                | Owners |  | 
            
                | Authors | Graf, Chris 
 | 
            
                | MINFILE Nos | 104G  009,
                            104G  029 | 
                
                    | Commodities |  | 
                
                    | Work Done | 
                                
                                    | Geochemical | Rock | 0 sample(s) |  
                                    |  | Soil | 0 sample(s) |  | 
                
                    | Keywords |  | 
                
                    | Related Report(s) |  | 
                
                    | File(s) | 14216.pdf 
 | 
                
                    | Geological Summary | JURASSIC AGE ANDESITES AND SILTSTONES SHOW A LARGE ALTERATION ZONE OF DISSEMINATED PYRITE ALONG A REGIONAL SHEAR ZONE. THE ROCKS ARE ALTERED TO PYRITE-SERICITE-QUARTZ SCHIST. MINERALIZATION CONSISTS MAINLY OF QUARTZ-CARBONATE VEINS WITH AURI-ARGENTIFEROUS GALENA, CHALCOPYRITE, AND SPHALERITE. |