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File Created: 31-Mar-1989 by Gary V. White (GVW)
Last Edit:  11-Dec-1989 by Larry Jones (LDJ)

Summary Help Help

NMI
Name HIREN LAKE, MOUNT COPELAND Mining Division Revelstoke
BCGS Map 082M018
Status Showing NTS Map 082M01W
Latitude 051º 07' 00'' UTM 11 (NAD 83)
Longitude 118º 26' 04'' Northing 5663777
Easting 399600
Commodities Nepheline Syenite Deposit Types R13 : Nepheline syenite
Tectonic Belt Omineca Terrane Monashee
Capsule Geology

Nepheline syenite and syenite gneisses crop out in a 6 kilometre band on the southern blank of Mount Copeland, 15 kilometres northwest of Revelstoke. The rock consists of orthoclase with subordinate nepheline and albite and small amounts of amphibole, pyroxene and magnetite. It has a banded texture and contains both fine and coarse- grained zones. The Mount Copeland syenites are exposed in a large antiformal structure and have been subjected to more than one phase of folding. The contacts appear gradational. Three main alkaline rock units have been defined; a basal nepheline syenite gneiss, overlain by alkaline amphibolite, which is in turn overlain by calcareous and saturated syenites. The alkaline rocks intrude micaceous quartzites and calcsilicate gneisses of the Frenchman Cap autochthonous cover sequence. The metasedimentary succession has been correlated with a similar succession in the Perry River and Mount Grace areas. Based on these correlations, it appears that the gneisses at Mount Copeland lie stratigraphically beneath the Mount Grace extrusive carbonatite.

Thirty-four samples collected from the deposit were analysed with the following results:

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Major oxides Weight (per cent)

SiO2 51.30 - 61.26

Al2O3 17.27 - 24.38

Fe2O3 0.84 - 8.21

CaO 0.04 - 9.61

Na2O 2.74 - 8.76

K2O 7.49 - 10.14

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These analyses indicate the rocks are a potential source of

feldspathic material although most samples are high in iron. To

better evaluate the material, two 20 kilogram samples, low in iron,

were sent to CANMET for processing. At CANMET they were crushed, run

through a dry magnetic separator (-10 + 100 mesh) and a mica-iron

float produced with the following results:

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Magnetic Separation (Weight, per cent) Magnetic Nonmagnetic -100 Mesh Sample 1 40.0 51.0 9.0 Sample 2 23.4 66.3 10.3

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Flotation Concentrate/float tails

(Weight, per cent) Slimes Mica-Iron Magnetic Nonmagnetic

Sample 1 15.6 27.9 19.1 36.5

Sample 2 20.0 3.8 28.6 46.6

The nonmagnetic concentrates were then analysed with the

following results:

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Major oxides Separation Floatation (Weight, per cent) 1 2 1 2 SiO2 56.20 47.1 54.80 50.70 Al2O3 19.20 20.50 18.30 21.10 Fe2O3 0.50 1.23 0.19 0.41 CaO 1.27 1.60 0.98 0.80 Na2O 6.58 6.02 6.44 5.48 K2O 8.40 9.45 8.76 10.57

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Full liberation is achieved at less than 100 mesh. Samples

processed by CANMET contain high levels or iron and titanium which

could not be reduced below 0.19 per cent and 0.40 per cent

respectively. This makes it difficult to produce nepheline syenite

meeting market specifications.

Bibliography
EMPR FIELDWORK 1978, pp. 25-30; *1988, pp. 485-486
EMPR OF *1987, pp. 59-62
GSC BULL 239
GSC P 80-1A, pp. 47-51; 81-1A, pp. 33-36
EG Vol. 81, pp. 1374-1386

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