| Property Name |
13536.pdf
|
| Location |
| NAD 83 |
50° 37' 59.00'' N, 127° 31' 36.00'' W
50.633056, -127.526667
UTM: Easting 604194, Northing 5610056, Zone 9 (North)
|
| NAD 27 |
50° 37' 59.48'' N, 127° 31' 31.23'' W
50.633189, -127.525343
UTM: Easting 604291, Northing 5609854, Zone 9 (North)
|
| NTS |
092L12E |
| BCGS |
092L063 |
|
| Mining Divisions |
Nanaimo |
| Mining Camp |
|
| Title |
|
| Report Year |
1985 |
| Number of Pages |
0 |
| Statements of Work |
n/a |
| Affidavit Date |
1985-02-18 |
| Off Confidential |
1986-02-18 |
| Claims |
BAR FR., BAY 55-56, BAY 58-60, COVE 18, COVE 20 |
| General Work Categories |
Drilling, Geochemical |
| Operators |
BHP-Utah Mines
|
| Owners |
|
| Authors |
Fleming, J.A.
|
| MINFILE Nos |
092L 135
|
| Commodities |
|
| Work Done |
| Drilling |
Diamond surface |
0 hole(s); 0.0 m |
|
Percussion |
0 hole(s); 0.0 m |
| Geochemical |
Sampling/assaying |
0 sample(s) |
|
| Keywords |
|
| Related Report(s) |
13346,
12271,
11366,
8150,
7427,
5265
|
| File(s) |
13536.pdf
|
| Geological Summary |
THE AREA IS UNDERLAIN BY THE UPPER TRIASSIC TO LOWER JURASSIC VOLCANIC AND SEDIMENTARY SUCCESSION OF THE VANCOUVER AND BONANZA GROUPS AND A DIS- CONTINUOUS CRETACEOUS SEDIMENTARY COVER. MIDDLE JURASSIC GRANODIORITIC STOCKS AND QUARTZ-FELDSPAR PORPHYRY DYKES CUT THE SUCCESSION. HYDROTHERMAL ALTERATION AND MINERALIZATION ARE ASSOCIATED WITH THE PORPHYRY DYKES IN THE BONANZA TUFFS. THE SUCCESSION DIPS GENTLY TO THE SOUTHWEST. FOUR PROMINENT FRACTURE DIRECTIONS ARE PRESENT ON THE PROPERTY AT 020, 060, 090, AND 130 DEGREES. THE DYKES ARE PRESENT ALONG THE 060 AND 130 DEGREES FRACTURE DIRECTIONS. DYKES AND SILLS IN THE AREA ARE BELIEVED TO BE CO-MAGMATIC WITH THE BONANZA VOLCANIC TUFFS.
|
