preliminary geological map (2010) by c. normand · mx undifferentiated murmac bay group rocks:...
TRANSCRIPT
BMq Quartzite: gray to white, medium grained; massive; > 90% quartz, < 3% hornblende, trace pyrite and garnet; apparent thickness up to 160 metres; MS=0.1-10.
BMm Amphibolite: salt and pepper, fine to medium grained; homogeneous, massive
to finely layered; 50-70% hornblende; MS=0.3-11. Unassigned Domain Ug Undifferentiated granitic rocks: Older component: light orange grey,
yellowish, medium grained; homogeneous, weakly to moderately foliated; 25% quartz, 15-20% biotite, common amphibolite inclusions; MS=1.6-15. Younger component: creamy white, coarse grained; massive to rarely foliated; 30-40% quartz; CI< 10; MS=0.3-9.4. Minor grey, coarse grained, massive to weakly foliated monzonite present as inclusions in older component; 7-10% quartz, 26% biotite, 4% hornblende; MS=2-9.5. Minor orange to brick red, medium- to coarse-grained hornblende quartz syenite.
SUPRACRUSTAL ROCKS AND DERIVED DIATEXITES
Murmac Bay Group
Mx Undifferentiated Murmac Bay Group rocks: interlayered grey, fine- to
medium-grained, finely-laminated, biotite-muscovite psammitic gneiss, 0.5-5% pyrite, 0-10% garnet, 0-7% round feldspar porphyroblasts up to 1 cm in diameter; massive, medium grained quartzite layers up to 1 m thick; schistose, garnet- and pyrite-rich rusty pelitic layers up to 2 m thick; up to 30% interlayered amphibolite; migmatization most commonly absent to moderate with < 50% leucosome; rare diatexites in contact with amphibolite; MS=0.2-30, avg=5.
Mm Amphibolite: salt and pepper, medium grained; massive and homogeneous,
occasional compositional layering; 40-50% hornblende, rare garnet < 2 cm in diameter with thin feldspar-hornblende reaction rims; coarse-grained feldspar-clinopyroxene veins common; MS=0.02-54, avg=3.8.
1 Magnetic Susceptibility in 10-3 SI units 2 Colour Index
Zp Pelitic gneiss and diatexite: light grey, cream to pink, salt and pepper weathering, medium to coarse grained; strongly foliated; commonly intrudes and contains sub-rounded blocks and fragments of fine- to medium-grained intermediate rock; medium- to course-grained amphibolite boudins and schlieren and quartz-rich layers are common; <20% garnet 0.5-1 cm in diameter, 0-5% sillimanite ± graphite; MS=0.1-153, avg=5.
ZMx Undifferentiated Murmac Bay Group rocks: Mafic volcanic component:
shades of black, grey, green; strong compositional layering, includes alternating fine- to coarse-grained amphibolite with up to 25% cm size garnet (CI=70-90), medium-grained feldspar-rich intermediate rock (CI=25-35), medium- to coarse-grained porphyritic rock, and medium-grained epidosite; MS=0.06-12.4, avg=3.4. Sedimentary component: light grey medium- to coarse-grained granitic garnet diatexite, medium- to coarse-grained leucocratic white feldspathic gneiss, garnet and magnetite rich iron formation, sillimanite-pyrite-graphite-rich psammopelite, and rare coarse grained 50 cm thick quartzite layers; MS=0.4-153.
Beaverlodge Domain Bsu Mylonitic rocks of unknown origin: dark brown to reddish tan, very fine
grained, cherty fracture surfaces; layered, locally ultramylonitic; unknown precursor; MS=0.8-5.4.
INTRUSIVE ROCKS
Blg Leucogranite: grey pink, medium to coarse grained; homogeneous, massive to
very weakly foliated; 30% quartz, 40-50% K-feldspar; CI=5-7; MS=1.1-5.2. Bgn Granitic gneiss: grey pink, medium grained; strongly foliated; 20-25% biotite;
MS=1.5-14.
SUPRACRUSTAL ROCKS AND DERIVED DIATEXITES
Murmac Bay Group BMx Undifferentiated Murmac Bay Group rocks: interlayered fine- to medium-
grained massive pyroxene-rich rock; purplish grey green medium-grained biotite and garnet rich rock; creamy grey coarse grained garnet diatexite; grey medium- to coarse-grained strongly- foliated biotite-muscovite psammopelite, 50% quartz, 30% biotite, 1-7% garnet; red feldspathic gneiss, 7-25% biotite, < 5% quartz, 0.5-3% pyrite; MS=0.3-14.
BMp Psammitic and pelitic rocks: grey, medium to coarse grained, foliated to
schistose quartzo-feldspathic gneiss layers up to 2 m thick dominate and contain up to 25% cm-scale garnet commonly replaced by micaceous material; muscovite locally abundant; interlayered with 20 cm to 6 m thick quartzite layers; grey-pink biotite-chlorite gneiss; minor 1-20 m thick rusty, schistose, biotite-chlorite-sillimanite-pyrite-graphite layers; up to 30% by volume foliation-parallel 2-5 mm thick quartz layers; MS=0.1-16.
Zemlak Domain
UNDIFFERENCIATED FAULT ROCKS Zsu Mylonitic rocks of unknown origin: hues of red, brown and green; very fine
grained, fresh surfaces saccharoidal to cherty; locally ultramylonitic; unknown precursor; low MS1; later cataclastic overprint with chloritic alteration.
Zsa Altered fault rocks of unknown origin: white to grey, ghost textures; strongly
cataclastic to mylonitic; feldspathic; metasomatic replacement product of amphibolite and other unknown precursors; >20% epidote in amphibolite precursor; low MS.
INTRUSIVE ROCKS
Zlg Leucogranite: pink to greyish pink, rarely red, medium to coarse grained;
massive to foliated to mylonitic; comprises variations with <5% mainly biotite and magnetite (MS=13-40), 5-8% pyribole (MS<20), and 35% equant smoky grey feldspar.
Zg Granitic gneiss: pink to greyish pink, medium to coarse grained; 5-40%
biotite, <8% hornblende, 0-5% magnetite, <3% garnet near contacts with unit Zp; MS=0.1-33, avg=8.3.
Zgd Granodioritic gneiss: dark grey, medium to coarse grained; wispy to streaky
texture; lineated with stretched clots of mafic minerals; hornblende ≥ biotite, rare orthopyroxene, 15-30% quartz; CI2=15-30; MS=0.5-44, avg=10.
Ztgd Tonalitic to granodioritic gneiss: grey to pinkish-grey, medium to coarse
grained; massive to layered; weakly foliated to ultramylonitic; tonalitic rocks comprise 10-25% hornblende and biotite and are locally intimately interlayered with amphibolites and granites, MS=10-37; granodioritic rocks contain up to 5% K-feldspar phenocrysts <5 cm long, MS=7-84; locally contains uniformly interlayered granitic pink medium- to coarse-grained leucosome and grey to dark grey, salt and pepper-textured, medium-grained, equigranular melanosome; <3% garnet near contacts with unit Zp.
Zlg-Ztgd Mixed units Zlg and Ztgd.
ROCKS OF UNKNOWN ORIGIN
Za Amphibolite: salt and pepper, medium to coarse grained; massive to
compositionally layered; local retrograde biotite along foliation planes, pyroxene present in coarse-grained veins and felsic layers in high strain zones, locally up to 20% garnet <3 cm in diameter; CI=35-80; MS=0.02-54, avg=6.
Zint Intermediate rocks: salt and pepper, fine to medium grained, typically
homogeneous and massive with local compositional cm- to m-scale layering; comprises tabular bodies <200 m thick commonly cut by coarse-grained feldspar-clinopyroxene veins; 15-25% hornblende, <7% biotite (locally up to 25%), <15% quartz; CI=15-35; MS=0.1-65, avg=14.
Ztgd-Zint Mixed units Ztgd and Zint.
SUPRACRUSTAL ROCKS AND DERIVED DIATEXITES
74N09
74N16
74O12
74O1374N15
74N08
74N10
74O0574O11
74N07 74O06
74O14
108°W
108°W
60°N60°N
28
22
25
32
72
36
65
78
82
45
44
51
47
80
85
41
50
41
70
75
51
38
30
89
45
54
35
75
65
45
56
4751
45
76
89
80
7460
45
62
60
60
2879
58
55
8489
30
40
13
33
72 80
82
65
78
45 5268
65
5041
5767
65
76 68
38
79
27
74
70
74
1568
78
8076
45
18
85
6040
Zlg
Ztgd
Zp
Ztgd
Ztgd
Zlg
Ztgd
Zg
Ztgd
Zint
Zlg-Ztgd
Zlg-Ztgd
Zg
Zg
Zlg-Ztgd
Zg
Zg
Zg
Zint
Zint
Zlg-Ztgd
Zg
Zp
Za
Zint
Zint
Zg
Zlg-Ztgd
Zint
Ztgd
Ztgd
Zp
Zp
Zp
Zp
Ztgd
Zlg
Zlg
Zlg
Zlg
Zlg
Zlg
Ztgd
Ztgd
Ztgd
Zint
RA2010-03
RA2010-02
RA2010-01Oshowy Lake
Hoidas Lake
Matheson Lake
341000
341000
342000
342000
343000
343000
344000
344000
345000
345000
346000
346000
347000
347000
348000
348000
349000
349000
6647
000
6647
000
6648
000
6648
000
6649
000
6649
000
6650
000
6650
000
6651
000
6651
000
6652
000
6652
000
6653
000
6653
000
107°45'W
107°45'W
107°50'W
107°50'W
Although the Ministry o f Energy and Resources has exercised all reasonable care in the compilation, interpretation, and production of this item, it is not possible to ensure total accuracy, and all persons that rely on the information contained herein do s o at their own risk. The Ministry of Energy and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in or derived from, this item.
43
44
42
6087
70
8630
3242
65
82
80
80
75
66
82
48
69
60
49
67
657262
83
7572
79
70
7670
78
61
64
62
75
83
78
60
48
80
50
50
44
55 69
70
54
68
58
50
84
65
63
74
7168
70
48 65
65
85
48
Zsu
Ztgd
Ztgd
Zlg
Ztgd
Ztgd
ZMx
Za
ZMx
Za
Zlg
Zsu
Za
Zint
Zint
ZMx
Ztgd
Zlg
Ztgd
Zsu
Zsu
Ztgd
RA2010-18
RA2010-17
RA2010-16RA2010-15
306500
306500
307000
307000
307500
307500
308000
308000
308500
308500
309000
309000
6631
500
6631
500
6632
000
6632
000
6632
500
6632
500
6633
000
6633
000
6633
500
6633
500
108°25'W
108°25'W
59°47'N
59°47'N
20
36
60
68
7478
45
7750
5660
7954
7864
7170
71
75
6469
80
7672
67
78
48
63
40
7850
58
69
7660
66
6851 76
7162
7285
70
80
78
7563
6565
83
85
72
48
706860
67
64
86
7678
85
52
78
72 57
76
604939
42
59
43
7143
56
62
71
70
Ztgd
Za
Zgd
Zg
Zgd
Zlg
Zg
Zlg-Ztgd
Ztgd
Zgd
Zg
Zp
Zp
Ztgd
Zlg
Zp
Zlg-Ztgd
Zp
ZintZgd
Zp
Zlg-Ztgd
Zlg-Ztgd
Zint
Zint
Ztgd
Zgd
Za
Za
Ztgd
Ztgd
RA2010-18RA2010-17
RA2010-16RA2010-15
RA2010-14
RA2010-13RA2010-12
RA2010-11
RA2010-10
RA2010-09
RA2010-08 RA2010-07
RA2010-06
RA2010-05
307000
307000
308000
308000
309000
309000
310000
310000
311000
311000
312000
312000
313000
313000
314000
314000
315000
315000
316000
316000
6634
000
6634
000
6635
000
6635
000
6636
000
6636
000
6637
000
6637
000
6638
000
6638
000
108°20'W
108°20'W
108°25'W
108°25'W
59°50'N
59°50'N
8
29
11
31
31
12
43
46
22
17
76
72
5880
80
68
72
52
79 50
76
55
63
70
15
75
55
62 78 70
58
60
80
62
68
54
78
86
71
72
59
7571
76
55
59
81
80
60
75
89
72
80
70
58
56
54
56
7646
64
70
55
45
52
80
75
6254
49
54
43
79
50
31
4343
58
68
48
65
66
80
37
80
74
Ztgd
Ztgd
Mx
Zlg-Ztgd
Mx
Mx
Mx
Zlg
Za
Ug
Ug
Zint
ZlgZtgd-Zint
Za
Zsa
Zp
Mm
Za
Za Mm
Zlg-ZtgdZint
ZaZa
Zint
Zlg-Ztgd
Zlg-Ztgd
Ztgd
Zsa
RA2010-04
107°55'W
107°55'W
59°50'N
59°50'N
333000
333000
334000
334000
335000
335000
336000
336000
337000
337000
338000
338000
339000
339000
6635
000
6635
000
6636
000
6636
000
6637
000
6637
000
6638
000
6638
000
6639
000
6639
000
6640
000
6640
000
16
21
22
31
32
32
35
35
36
42
43
43
45
45
45
46
46
46
47
48
48
48
49
49
50
51
51
52
52
52
53
54
55
57
58
58
58
59
60
60
60
61
61
61
62 62
64
64
65
65
65
65
66
68
69
70
70
70
70
72
72
75
75 76
77
78
78
78
78
80
80
81
82
8284
86
88
55
65
78
46
32
78
Bmp
BMx
Bgn
Blg
BMq
BMq
BMqBSu
BMm
BMmBmp
Bmp
Bmp
Bmp
Bmp
Bmp
RA2010-30
RA2010-29
RA2010-28
RA2010-27
RA2010-26
RA2010-25
RA2010-24
RA2010-23RA2010-22
RA2010-21
RA2010-20
RA2010-19
Edworthy Lake
108°W
108°W
108°2'W
108°2'W
108°4'W
108°4'W
59°40'N
59°40'N
327500
327500
328000
328000
328500
328500
329000
329000
329500
329500
330000
330000
330500
330500
331000
331000
6618
000
6618
000
6618
500
6618
500
6619
000
6619
000
6619
500
6619
500
6620
000
6620
000
6620
500
6620
500
Easting Northing Total counts per second % K ppm U ppm Th
RA2010-01 343573 6649939 1150 6.3 3.7 181RA2010-02 345884 6650996 1300 5.7 8.5 164.5RA2010-03 345726 6653069 3800 5.0 6.1 674.5RA2010-04 336893 6639395 3200 7.0 123.3 201.7RA2010-05 313555.8 6637678 1200 4.6 3.6 218
2100 3.0 5.2 336.41500 7.5 28.4 118.41910 3.0 5.2 304.62840 3.0 11.2 475.21500 3.6 4.6 223.32800 2.5 19.9 500.18500 4.0 50.8 1895
RA2010-07 312980.1 6636684 1380 6.4 2.9 194.5RA2010-08 312715.5 6636666 1250 2.4 6.9 184.5RA2010-09 313716.5 6636405 2160 5.9 5.8 347.5RA2010-10 313051.3 6638313 1000 4.5 4.8 139.1RA2010-11 312964.2 6638225 1260 3.4 2.7 204.6RA2010-12 308774.9 6635649 1250 2.3 1.2 202.4RA2010-13 309899 6635747 4300 3.0 17.3 771.7RA2010-14 310031.4 6635864 2000 4.4 23.4 285.2
1530 3.8 34.9 170.11350 4.9 32.3 121.11080 4.7 18.1 120.81200 4.1 32.3 110.62100 4.7 95.2 103.5
RA2010-16 308221.3 6633453 1500 7.5 28.4 118.41000 5.4 17.1 88.82200 5.9 38.9 229.4
RA2010-18 307735.8 6633487 1510 5.9 54.4 64.7RA2010-19 329322.7 6618834 1550 3.6 5.2 242.2RA2010-20 329444.5 6618655 1260 6.5 5.5 174RA2010-21 329275.3 6618415 4550 3.2 19.5 815.7RA2010-22 329248.9 6618249 43600 >90 2038 >10000RA2010-23 329265.7 6618273 4200 4.1 29.6 690.9RA2010-24 329259.5 6618137 30900 57.9 759.9 >10000RA2010-25 329233 6618141 46600 >90 2262 >10000RA2010-26 327693.4 6618738 1800 3.6 8.7 298.5RA2010-27 329373.8 6619885 1830 5.0 5.7 289RA2010-28 329209.4 6618241 52000 >90% 4099 >10000RA2010-29 329213.2 6618222 23100 27.0 293 6131RA2010-30 329242.8 6618116 53500 >90% 4503 >10000
Spectrometry
Alce
s Lak
e
RA2010-15 307952.4 6633417
313080.2 6637556
6633515
Area Radiometric anomaly #
McNu
tt Lak
e
Location*
Osho
wy
Lake
RA2010-06
Ena L
ake (
Nadir
Bay
)
RA2010-17 307801.3
Zsu
Zsa
Zg
Zgd
Ztgd
Za
Zint
Zp
Ug
Ztgd-Zint
Bsu
Blg
Bgn
BMx
BMp
BMq
BMm
Mx
Mm
Zlg
Zlg-Ztgd
ZMx
Scale 1:10 0000 0.5 10.25
Kilometers0 0.40.2
Miles
Alces Lake
Symbols Geological contact
S1 foliation (dip unknown, inclined, vertical) S3 foliation (dip unknown, inclined, vertical) Dyke (inclined granitic, inclined mafic, unknown dip mafic) Stretching lineation (third generation, generation unknown)
Intersection lineation (third generation)
Minor S fold (third generation) Minor Z fold (third generation)
Minor symmetrical fold (third generation) Axial plane (third generation)
Fault or lineament (probable brittle-ductile fault) Shear zone Radiometric anomaly with ID # (see table) High strain zone Granulite facies metamorphic grade Glacial striae Sand Swamp Contour (50 feet) Reef
The area was mapped by Charles Normand, in the summer of 2010, with the assistance of Andrew Masurat and Devin Anderson. This map was printed from the geologist’s digital file. Geological data were processed using Microsoft Access, and ArcView 9.3 software. Base maps were compiled from CanVec 1:50 000 scale digital cartographic maps produced by Natural Resources Canada. Grid coordinates are NAD83 CSRS98 UTM zone 13. The map was processed overall using ArcView 9.3 software. The map is issued in a package with the Summary of Investigations 2010 Volume 2, Saskatchewan Geological Survey, and is available separately from http://www.er.gov.sk.ca/geo-reports. This map accompanies the following publication: Normand, C. (2010): Bedrock Geology of the Oshowy Lake – Buchanan Lake Area and Investigation of the REE Mineralization Potential in the Ena Lake, Bear Lake and Alces Lake Areas; in Summary of Investigations 2010 Volume 2, Saskatchewan Geological Survey, Sask. Ministry of Energy and Resources, Misc. Rep. 2010-4.2. This map may be referenced as: Normand, C. (2010): Bedrock Geology of the Oshowy Lake, Buchanan Lake, Ena Lake, Bear Lake and Alces Lake Areas (Parts of NTS 74N16, 74O13 and 74N09); 1:10 000 and 1:20 000 scale prelim. maps; with Summary of Investigations 2010, Volume 2, Saskatchewan Geological Survey, Sask. Ministry of Energy and Resources, Misc. Rep. 2010-4.2.
Legend
Bedrock Geology of the Oshowy Lake, Buchanan Lake, Ena Lake, Bear Lake and Alces Lake Areas (Parts of NTS 74N16, 74O13 and 74N0 9) at 1:10 000 and 1:20 000 scale Preliminary Geological Map (2010) by C. Normand
NAD83(CSRS98) UTM zone 13N
Lake Athabasca
Ena Lake
Catalogue Number 2010-4.2-(3)
12
3
4
5
Buchanan LakeScale 1:20 000
0 1 20.5Kilometres
0 10.5Miles
4
Oshowy LakeScale 1:20 000
0 1 20.5Kilometres
0 10.5Miles
3Ena LakeScale 1:20 000
0 1 20.5Kilometres
0 10.5Miles
1
5
Location Map
RA2010-01
(values recorded from a hand-held RS-230 spectrometer)Radioactive Anomalies
Ena Lake(Nadir Bay)
Bear Lake
McNutt
Lake
Alces Lake
Buchanan Lake
Bear LakeScale 1:10 000
0 0.5 10.25Kilometres
0 0.40.2Miles
2