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{WQd}
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{WQd}
{Qm}
(Qm)
{Mzd}
[Mzd]
{MQm}
{WQd}
(PGd)
{Qm}
[Di]
80
{Qm}
{G}
[WAm]
{G}
{G}
[WAm]
(G)
[WAm]
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{Qdi}
Qmg
Qmg
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PARKER LAKE SHEAR ZONE
81
76
73
75
78
79
80
8085
77
75
77
80
80
78
76
80
67
85
70
65
69
80
81
78
73 73
76
80 75 80
80
80
82
78
7580
85 85
85
85
8085
80
80
73
85
8185
85 80
80 80
80
80
75
85
85
73
75
80
75
75
80
80
8268
75
81 8280
80
82
82
82
77
78
85
80
75
79
68
73
85
85
7368
85
70
50
76
6870
60
75
81
80
69
80
70
80
80
80
85
80
60
77
80
78
85
7478
85
80
8580
8280
80
79
75
80
75
85
80
85
65
75
65
75
80
76
80
80
76
79
77
7176
72
68
73
52
80
7571
80
77
80
85
85
76
50
80
75
77
80
8280
85
79
77
78
87
80
85
77
81
78
55
60
7070
68
70
65
75
70
72
69
72
80
7580
75
70
75
66
75
74
70
70
65
75
77
65
70
70
68
79
85
7577
76
78
76
7780
76
76
76
82
81
74
7580
8578
80
83
85
80
85
76
80
80
85
74
81
65
78
43
75
85
80
80
80
73
80
87
75
59
77
70
75 80
78
84
85
85
85
8573
78
7178
8173
85
78
80
78
70
80
79
71 85
81
85
71
75
67
80
75
75
67
82
76
85
79
7546
85
76
85
75
79
5473
78
74
82
77
81
79
79
70
75
81
82
80
75
74
74
82
8175
76
77
78
74
75
85
75
81
85
80
78
75
86
63
75
80
70
70
78
82
82
77
7080
75
73
75
59
7185
72
56
86
85
55
8285
85
80
85
78
81
8580
85
82
7679
72
71
73
8169
77
78
71
72
79
62
71
76
69
62
59
77
61
54
5668
8064
51
82
82
80
85 75
85
85 75
85
75
83
85
75
75
75
78
80
86
78
80
73
75
85
85
85
8084
85
80
85
82
80
70
85
86
8462
78
8077
77
77
74
71
80
85
85
86
78
80
83
75
85
82
85
857380
8085
85
62
84
70
5865
76
59
85
80
75
81
80
8180
76
7870
80
78
78
8080
85
80
8881
7678
83
79
75
85
85
81
72
37
85
80
74
80
80 75
7880
70
74
85
75 78
80
85
85
82
85
80
75
75
80
8068
8580
80
85
86
78
85
80
85
8085
74
79
6178
808575
78
70
80
80
82
85
56
68
59
30
34
70
47
80
63
64
52
10
59
83
85
77
77
76
78
80
80
80
75
83
72
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82
66
85
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71
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80
80
52
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70
73
80
72
63
78
53
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82
83
52
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85
85
80
81
80
80
82
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65
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38
76
76
8583
83
80
78
73
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78
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81
81
85
80
85
70
81
75
80
71
69
77
7275
85
72
78
7575
80
82
81
80
76
85
87
80
74
85
75
85
62
80
82
8585
77
85
8080
8576
80
82
79
80
85
5468
706970
69
70
74
80
RM0201-182
RM0201-177
RM0201-171
RM0201-138
RM0201-129
RM0201-128
RM0201-113
RM0201-091
RM0201-089
RM0201-083
RM0201-049
RM0201-046
RM0201-041
RM0201-027
RM0201-026RM0201-024
RM0201-021
RM0201-013
RM0201-005
RH0201-601
RH0201-502
RM0201-178
RM0201-142
RM0201-036
RM0201-032
RH0201-600
RH0201-540
PQd
Not Mapped
Mz
Qm
MQm
Agr
Qm
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LLg
WDi
WDi
Gl
LLg
Qm
Gd
Mzd
QmWGa
Qmg
G
Qm
PQd
PQd
G
G
WGa
Not Mapped
PGd
WDi
LLg
WDi
G
Mf
WDi
Gdg
(G)
WDi
WDi
Not Mapped
Gl
Ppd
Qmg
Gl
WDi
WQd
Gdg
G
Mz
WDi
G
Qm
Qm
Mz
WGa
Gl
WDi
Gd
WGa
Gd
Mzd
Ps
Gdg
Psp
LGa
G
Gd
PQd
LDi
Qm
WDi
G
WGa
WGa
PGd
CRG
Gd
Ppd
Qm
LGa
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Gd
MQm
Gd
Qm
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Gd
Mz
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MQm
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MQm
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WGa
PQd
Gl
WDi
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Gl
Psp
WAm
PAm
WDi
WQd
WDi
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WGa
Ps
Gdg
WGa
MQm
WUp
WQd
WAm
MQm
Psp
MQm
WGa
WQd
WGa
WUp
MQm
WDi
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WAm
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WDi
PUp
WUp
PAm
WAm
WGa
WAm
PAm
WDi
MQm
WGa
PAm
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PAm
WDi
WAm
WAm
WDi
Gd
WDi
2566–8 Ma (8)
2566–2 Ma (7)120
110
py, po
mag, po, py, cpy
py, cpy
py, mag, cpy
po, py, cpy, az
py, po, cpy, sph, mag
434
427
404
394
386
391
391401
401
402
401
435
425
413
426
404
408
426
402
426
365
Robson Lake
Warner Lake
Wathaman River
562000
562000
563000
563000
564000
564000
565000
565000
566000
566000
567000
567000
568000
568000
569000
569000
570000
570000
571000
571000
572000
572000
573000
573000
574000
574000
575000
575000
576000
576000
577000
577000
578000
578000
579000
579000
6327
000
6327
000
6328
000
6328
000
6329
000
6329
000
6330
000
6330
000
6331
000
6331
000
6332
000
6332
000
6333
000
6333
000
6334
000
6334
000
6335
000
6335
000
6336
000
6336
000
6337
000
6337
000
6338
000
6338
000
6339
000
6339
000
�Scale 1:20 000
64E-02 64E-0164E-03
64E-04
64E-07 64E-0864E-06
64E-05
64E-10 64E-0964E-1164E-12
64E-1664E-1564E-1464E-13
74H-01
74H-08
74H-09
74H-16
This Map
Reindeer
Lake
104
104
102
102
5858
5757
Location Map
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Although the Department of Industry 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 who rely on the information contained herein do so at their own risk. The Department of Industry 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.
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Catalogue Number 2002-4.2-(2.3 )
Project M.138 of 2002 The area was mapped by Ralf O. Maxeiner and Rebecca Hunter, in the summer of 2002, with the assistance of Shawna Leatherdale, Vance Hachkewich, and Jason Craven.
a were processed using Pendragon Forms, Microsoft Access, and ArcView 3.2 software. Base maps were compiled from 1:50 000 scale digital topographic maps licensed from Saskatchewan Information Services Corporation. UTM coordinates are NAD83 zone 13. The map was processed overall using ArcView 8.2 software. The map is issued in a package with the Summary of Investigations 2002 Volume 2, Saskatchewan Geological Survey, and is available separately. This map accompanies the following publication: ���������������� �������������������������������������������������������������������� �!�����"�����������#����"�!!��$��%�&�'������������������(���!�����"������������)����������"��'�$��"����&������$���������������������*�����+,��������������������� ����������������������� ����������������-�������������$��%������������������������ �!����� �����$�.�/� �0����!����'������0������������*�����%�12"�3,4+,�#�5��������������*����!�!�*������"�!!��$��%�&�'������������������(���!�����"������������)����������"��'�$��"����&������$���������������������*�����+,��
0 0.5 1 1.5 20.25Miles
0 1 2 30.5Kilometers QUATERNARY
Glacial Till, fluvioglacial sand, gravel, glaciolacustrine clay --------------------------------------------------- Unconformity ----------------------------------------------------------- PRECAMBRIAN1
Wathaman Domain
Megacrystic quartz monzonite (~1.860 Ga2): pink to pinkish grey, medium to coarse grained3, weakly foliated to mylonitic; locally cataclastic, commonly megacrystic with up to 3 cm long microcline phenocrysts; locally with 20-40 cm thick layers of pink fine-grained mylonitic granite; up to 50% K-feldspar; 20 to 30% plagioclase; and 10 to 20% quartz; 5 to 15% biotite, hornblende and/or epidote; MS4 is high and variable Wollaston Domain
Courtenay Lake Formation (~2.076 Ga5)
Quartzofeldspathic rock: pink to light pinkish grey, fine to medium grained, granoblastic, homogeneous, strongly foliated; locally gneissic; with abundant quartz veins; deformed equivalent of unit CFa and/or Gf; up to 40% K-feldspar; 20-30% quartz; plagioclase, biotite, muscovite, magnetite; high to very high MS (5-15) Quartzite: light grey to beige, fine grained, granoblastic, moderately to strongly foliated, bedded; minor layers of pebble conglomerate and feldspathic psammite; up to 10% plagioclase and K-feldspar; magnetite, biotite, muscovite – garnet; very high MS Amphibolite: dark green to greenish black; fine grained, weakly to moderately foliated; locally amygdaloidal and/or plagioclase porphyritic; rarely pillowed; locally with intercalations of garnetiferous quartz-eye dacite and biotite-hornblende-bearing intermediate volcaniclastic rock; also with minor fine- to medium-grained microdiorite; up to 70% plagioclase; 35-50% actinolite; biotite, magnetite – garnet – tourmaline – anthophyllite – pyrite; very high MS (50-100) Feldspathic arenite6: light pink to light grey, fine grained, weakly to moderately foliated; schistose, bedded, with local cross-bedding, rare pebbly beds; up to 50% K-feldspar, up to 30% quartz, plagioclase, biotite, muscovite, magnetite; very high MS (20-30) Cobble conglomerate: light pink to pink, poorly sorted, well foliated; fine-grained matrix of feldspathic psammite; strongly flattened pebbles and boulders of leucogranite, vein quartz, amphibolite, and pink fine-grained felsic rock; granules of quartz and feldspar; medium to thickly bedded; interbedded with feldspathic psammite; K-feldspar, plagioclase, quartz, biotite, muscovite, magnetite; very high and variable MS (10-30) Peter Lake Domain
Monzonitic Intrusive Suite
Monzonite: grey to pinkish grey, medium to coarse grained, homogenous, moderately to strongly foliated; locally mylonitic; commonly with 1-2 cm long K-feldspar megacrysts; gradational into monzodiorite, syenite and quartz monzonite; cut by granite pegmatite dykes; 30-60% microcline; 30-40% plagioclase; up to 10% biotite; up to 10% hornblende; up to 5% quartz; – epidote; high to very high MS Monzodiorite: light pink to pink, medium to coarse grained, homogenous, moderately foliated; locally plagioclase megacrystic; gradational into monzonite, diorite and quartz monzodiorite; plagioclase, K-feldspar; up to 10% biotite; up to 5% epidote; quartz – hornblende; variable MS Quartz monzonite: light pink to pink, medium to coarse grained, homogeneous, weakly to strongly foliated; locally mylonitic; commonly with up to 3 cm long K-feldspar megacrysts; 30-40% microcline; 20-30% plagioclase; 5-10% quartz; 10-15% biotite; up to 5% hornblende and/or epidote; – carbonate; moderate to very high MS Quartz monzonite gneiss: pink to grey, fine to coarse grained, moderately to strongly foliated; gneissic layering; in part megacrystic; 30-40% microcline; 20-30% plagioclase; 5-10% quartz; 10-15% biotite; up to 5% hornblende; variable MS Intrusive Rocks of undetermined affinity
Granite pegmatite: pink, coarse to very coarse grained, massive to weakly foliated; microcline, quartz, plagioclase, biotite – muscovite – magnetite; low MS Pb beryliferous pegmatite Amphibolite: greenish black to black, very fine to fine grained; plagioclase, hornblende – biotite – epidote – riebeckite; in part derived from mafic dykes; moderate to very high MS Fluoritic syenogranite (2.086 Ga7): salmon pink to moderate orange pink, medium to coarse grained, equigranular, homogeneous, massive to weakly foliated; locally mylonitic; locally cut by quartz veins, mafic dykes and granitic pegmatite dykes; 40-50% microcline; 30% quartz; 10-20% plagioclase; 5-10% biotite; magnetite, monazite, apatite, zircon – chlorite – muscovite – fluorite; high MS Leucogranite: pink to brick red, fine to medium grained, equigranular, leucocratic, massive to weakly foliated; cut by mafic dykes; 30-40% microcline; 20-30% quartz; 20-30% plagioclase; <5% biotite; magnetite; high MS Glq quartz and/or feldspar porphyritic Granite, Syenogranite: light pink to moderate pink, coarse grained to very coarse grained, massive to weakly foliated; 30-40% microcline; 20-30% quartz; 20-30% plagioclase; 10-15% biotite – hornblende; magnetite; low to moderate MS
Granite (2.566 Ga7): salmon pink to brick red, coarse grained, homogenous, massive to weakly foliated; locally mylonitic; in part megacrystic; gradational into granodiorite and quartz monzonite; intruding older quartz monzonite; 25-40% microcline; 15-30% quartz; up to 30% plagioclase; 5-10% epidote; up to 5% biotite; high to very high MS Seriate syenogranite: mottled pink to grey, medium to very coarse-grained, equigranular to seriate, homogeneous, massive to weakly foliated; 30-50% microcline; 25-30% quartz; 20% plagioclase; 5-15% biotite; low to high MS Megacrystic/augened granite: pink to moderate orange pink, coarse to very coarse grained, megacrystic, homogeneous, moderately to strongly foliated; locally mylonitic; with 1-2 cm long pink microcline phenocrysts ; cut by mafic dykes and granite pegmatite; 30-40% microcline; 30% quartz; 20-30% plagioclase; 10-15% biotite; magnetite – fluorite; high MS Hornblende-biotite granite: pink, medium to coarse-grained, equigranular, homogeneous, massive to weakly foliated; 30-50% microcline; 25-30% quartz; 20% plagioclase; 5-10% hornblende; 5-10% biotite; low to high MS Granitic gneiss: grey to yellowish brown, fine to medium grained, equigranular, moderately foliated; gneissic layering; K-feldspar, plagioclase, quartz, biotite, hornblende, magnetite; very high MS Granodiorite: light pink to light pinkish grey, medium grained, moderately to strongly foliated; locally megacrystic; plagioclase; 20-30% quartz; 15-20% microcline; 5-10% biotite; 5-10% hornblende; high MS Granodiorite gneiss (?2.580 Ga8): grey to pinkish grey, fine to medium grained, moderately foliated; gneissic layering; cut by mafic dykes; 50% plagioclase; 20-30% microcline; 5-10% hornblende; 5% biotite; monazite; moderate MS Quartz diorite: light to medium grey, medium to coarse grained, equigranular, homogenous, weakly foliated; cut by granite pegmatite; locally associated with blue quartz-bearing granodiorite; up to 60% plagioclase; 10-20% quartz; up to 15% hornblende; 5-10% biotite; up to 10% K-feldspar; epidote; magnetite; very high MS Diorite: black and white, medium grained, equigranular, homogeneous, massive to weakly foliated; locally gradational into quartz diorite; plagioclase; 10-20% hornblende; up to 10% biotite; – epidote – quartz; low to moderate MS Combe Lake Intrusive Suite
Diorite: black and white, medium grained, homogeneous, equigranular, moderately to strongly foliated; 50-70% plagioclase; 15-35% hornblende; up to 10% biotite – epidote – titanite – pyrite; moderate MS Gabbro: black and white, medium grained, homogeneous, equigranular, moderately to strongly foliated; locally grading into ultramafic rocks; 30-50% plagioclase; 35-50% hornblende; up to 10% biotite – epidote – pyrite – magnetite – pyrrhotite – chalcopyrite; high to very high MS Warner Lake Gabbroic Suite
Diorite: mottled black and white to grey, medium to coarse grained, equigranular, massive to strongly foliated; locally mylonitic; gradational into quartz diorite and gabbro; cut by less deformed quartz monzonite and granite; 50-60% plagioclase; 15-35% hornblende and/or biotite; up to 5% quartz; epidote – magnetite – carbonate – chlorite – pyrite; moderate MS Gabbro: speckled black and white, dark grey to greenish black, medium grained, equigranular, massive to strongly foliated; commonly heterogeneous and mylonitic; rare igneous layering; locally gradational into ultramafic rock; locally cut by dioritic and monzonitic rocks; 35-60% hornblende, up to 60% plagioclase; epidote, biotite, magnetite – serpentine – pyrite – pyrrhotite – chalcopyrite; moderate MS, locally high MS Quartz diorite: mottled grey to black, coarse grained, homogeneous, equigranular, moderately to strongly foliated; up to 50% plagioclase; 20% hornblende; 15% quartz; 10% biotite; up to 10% K-feldspar; epidote; variable MS Pyroxenite: dark green to greenish black, coarse to very coarse grained, homogenous, massive to strongly foliated; grading into actinolite schist where more deformed; locally gradational into gabbro; variably recrystallized; up to 90% amphibole (actinolite and/or hornblende); and/or up to 60% clinopyroxene; <10% plagioclase; biotite, chlorite, epidote, pyrite, pyrrhotite; moderate MS Amphibolite: dark green to dark grey, fine to medium grained, equigranular, strongly foliated; possibly derived from units WGa and WDi; in part possibly of supracrustal origin; 40-60% hornblende and/or actinolite; up to 50% plagioclase; biotite, quartz, epidote, chlorite – carbonate – pyrite; moderate MS Love Lake Leucogabbro (? 2.562 Ga2)
Leucogabbro: light bluish grey to grey, medium to coarse grained, homogenous, equigranular, massive to weakly foliated; locally with abundant subangular mafic to ultramafic xenoliths; in part gradational into gabbro, anorthosite, or diorite; up to 80% plagioclase (labradorite); up to 25% hornblende; up to 10% relict clinopyroxene; up to 5% magnetite, pyrite – epidote – quartz – actinolite – biotite – ilmenite – hematite; 15-25% mafic mineral content; very high MS (50-100) Diorite: speckled black and white, dark grey, medium grained, equigranular, homogenous, weakly foliated; up 70% plagioclase; 15-25% hornblende; up to 10% biotite; epidote – quartz – pyrite – magnetite; low MS Gabbro and Melagabbro: dark greenish grey to greenish black, medium to coarse grained, massive to weakly foliated; 40 to 80 percent amphibole (hornblende and/or actinolite); up to 50 percent plagioclase; relict clinopyroxene; magnetite – orthopyroxene – epidote – biotite – microcline – pyrite – pyrrhotite; variable MS, locally very high
Anorthositic rock: light bluish grey to white; medium grained, homogeneous, massive to weakly foliated; grading into leucogabbro and diorite; locally with centimetre-scale rhythmic igneous layering between leucogabbro and anorthosite; up to 90% plagioclase; up to 15% hornblende; up to 5% biotite; 5-15% mafic mineral content; up to 5% relict clinopyroxene; very high MS Ultramafic rock: dark green to black, fine to medium grained, weakly foliated; in part derived from pyroxenite; up to 95% hornblende and or tremolite-actinolite; up to 5% plagioclase, serpentine, magnetite – chlorite – olivine; variable MS Parker Lake Gneisses
Quartz diorite gneiss: composite unit of dioritic to granodioritic orthogneisses; light grey, pinkish grey to dark grey, fine to coarse grained, heterogeneous, inequigranular, locally porphyroclastic, moderately to strongly foliated; commonly with gneissic layering on centimetre to decimetre scale; with fine-grained amphibolitic and psammitic layers; locally homogenous diorite, quartz diorite or granodiorite; commonly with later leucogranite, quartz monzonite and pegmatitic granite sheets; plagioclase, quartz, microcline, hornblende, biotite, 5-20% mafic mineral content; MS variable from low to very high Granodiorite to tonalite (2.566 Ga8): light pinkish grey to grey, medium to coarse grained, homogenous to heterogeneous, strongly foliated; interlayered with quartz dioritic components of PQd and xenoliths of amphibolite; cut by granite pegmatite and aplite; plagioclase; 15-30% quartz; 5-20% microcline; 5-10% hornblende; 5-10% biotite; zircon with secondary overgrowth; epidote, titanite; low MS Amphibolite, Gabbro: black to greenish black, fine to medium grained, heterogeneous, strongly foliated; locally ultramafic; cut by granodioritic and granitic veins; plagioclase; 35-60% amphibole (hornblende and/or actinolite); biotite; variable MS Ultramafic rock: black to dusky green, fine grained but knobbly weathering due to originally coarse-grained texture, homogenous, massive to weakly foliated; recrystallized pyroxenite; 80-90% actinolite after pyroxene; 10% biotite; plagioclase, sericite; low MS Supracrustal Rocks
Campbell River Group Quartzite: interbedded succession of pebbly feldspathic wacke, subarenite, quartz arenite, and argillite; light grey to black, very fine grained to fine grained, weakly foliated; locally schistose; fining-upward succession; primary bedding features indicate younging to the north and include ripples, cross-bedding, ball and pillow structures, and scouring; locally with blue quartz granules; quartz, microcline, plagioclase, biotite, muscovite – andalusite Felsic volcanic rock: light grey to beige, fine grained, well foliated; layered; includes tuff breccia, feldspar porphyry and aphanitic components; quartz veins; up to 50% plagioclase; 20-30% quartz; up to 15% K-feldspar; 5-10% biotite; muscovite – garnet – epidote; low MS Migmatitic psammopelite-pelite: white to medium grey, fine to medium grained, heterogeneous, granoblastic, moderately to strongly foliated; gneissic; migmatitic with 10-20% locally derived tonalitic leucosome; in part agmatitic with leucosome intruding intercalated amphibolite; compositionally variable from pelitic to psammitic; locally layered with intercalations of ferruginous psammite and silicate-facies iron formation; up to 60% plagioclase; up to 40% quartz, 10-30% biotite; – garnet – cordierite – graphite – magnetite; variable MS Diatexite: white to light grey, medium to coarse grained, leucocratic, homogeneous to gneissic, weakly to moderately foliated; tonalitic in composition; with up to 5% psammopelitic paleosome; up to 60% plagioclase; 25-30% quartz; up to 5% K-feldspar; biotite; generally low MS Psammitic gneiss: medium grey to buff, very fine to fine grained, moderately foliated; locally layered; in part migmatitic; intruded by diorite, granodiorite and/or granite pegmatite; up to 50% plagioclase, up to 40% quartz, 5-10% biotite; up to 10% K-feldspar; – hornblende – muscovite – carbonate – epidote; low MS Psg with intercalations of conglomerate Amphibolite: greenish black to dark grey, very fine to fine grained, moderately to strongly foliated; locally layered, feldspar phyric and/or with epidote pods; possibly of volcanic origin; cut by tonalitic and granitic veins and dykes; up to 60% plagioclase; 35-50% hornblende; up to 10% biotite; – epidote – quartz – magnetite – pyrite; variable MS Mfp feldspar porphyritic; possibly of subvolcanic origin Mfh hornblende porphyroblastic 1 the prefix meta- has been omitted as all rocks have been metamorphosed 2 e.g. Corrigan, D., Maxeiner, R.O. and Harper, C.T. (2001): Preliminary U-Pb
Results from the La Ronge-Lynn Lake Bridge Project; in Summary of Investigations 2001, Volume 2, Saskatchewan Geological Survey, Sask. Energy Mines, Misc. Rep. 2001-4.2, p111-115.
3 grain size limits: very fine (<0.5 mm); fine (0.5-1mm); medium (1-5 mm); coarse (5-10 mm); very coarse (> 1cm)
4 MS: magnetic susceptibility outcrop average (in 10-3 SI); readings are grouped into very low (< 0.10), low (0.10 to 0.49), moderate (0.50 to 0.99), high (1.00 to 10), and very high (> 10.00) categories; averages are given in brackets were appropriate.
5 Ansdell, K.M., MacNeil, A., Delaney, G.D., and Hamilton, M.A. (2000): Rifting and development of the Hearne craton passive margin: age constraints from the Cook Lake area, Wollaston Domain, Trans-Hudson Orogen, Saskatchewan (extended abstract); GeoCanada 2000, May 29-June 2, Calgary, Canada, compact disc.
6 the term arkose is discontinued and replaced with ’feldspathic ; see: Maxeiner, R.O., Gilboy, G.F. and Yeo, G.M. (1999): Classification of metamorphosed clastic sedimentary rocks: a proposal; in Summary of Investigations 1999, Saskatchewan Geological Survey, Sask. Energy Mines, Misc. Rep. 99-4.1, p89-92.
7 Annesley, I.R., Madore, C., and Krogh, T.E. (1992): U-Pb geochronology of some granitoids from the Peter Lake Domain: a summary; in Summary of Investigations 1992, Saskatchewan Geological Survey, Sask. Energy Mines, Misc. Rep. 92-4, p168-171.
8 Bickford, M.E., Rayner, N.M., and Stern, R.A. (2002): The exotic origin of the Sask craton, Trans-Hudson Orogen revealed by new SHRIMP zircon U-Pb ages; GAC-MAC Joint Annual Meeting, Saskatoon, Saskatchewan, Abstracts Volume 27, p10.
Legend
MQm
CQf
CQz
CAm
CFa
CCg
Mz
Mzd
Qm
Qmg
P
Am
Gf
Gl
G
Agr
Gs
Gm
Gh
Gg
Gd
Gdg
Qdi
Di
BDi
BGa
WDi
WGa
WQd
WUp
WAm
LLg
LDi
LGa
LAn
LUp
PQd
PGd
PAm
PUp
CRG
Fv
Psp
Ppd
Ps
Mf
Symbols
Geological contact: defined to approximate High strain zone Fault Outcrop examined Felsenmeer, Blockfield, Boulderfield Glacial striae Mineral occurrence: az - azurite, cpy - chalcopyrite, fl - fluorite, il - ilmenite, mag - magnetite, mal - malachite, po - pyrrhotite, py - pyrite, ru - rutile, sph - sphalerite Sample location with available geochemistry (see report) Approximate sample location of historical geochronology data with footnote reference (see report for details) Bedding: top unknown, top known, overturned Main foliation (1st and 2nd generation) (schistosity, gneissosity): dip unknown, inclined, vertical 3rd generation foliation: inclined, vertical Fold axial plane (inclined): age unknown, 1st generation and 2nd (tight to isoclinal) generation, 3rd generation (ENE trending, upright, close to tight), 4th generation (NNE trending, open) Fold axial plane (vertical): age unknown, 1st generation and 2nd (tight to isoclinal) generation, 3rd generation (ENE trending, upright, close to tight), 4th generation (NNE trending, open) Small ductile shear (inclined): sense unknown, sinistral, dextral Small ductile shear (vertical): sense unknown Small brittle fault (inclined): sinistral, dextral Small brittle fault (vertical): sinistral, dextral Fracture: inclined, vertical Lineation (unknown age): unknown type, stretching lineation Fold axis (symmetry unknown): age undefined Fold axis (symmetrical): age undefined Fold axis (s-fold): age undefined Fold axis (z-fold): age undefined Traverse path in poorly exposed areas Esker Muskeg Contour line (contour interval 10 metres) Spot elevation (metres) Gravel pit Campground Fishing lodge Microwave tower Highway (digitized from 2000 airphotos) Highway Km marker Trail {XX} - indicates that an area contains minor proportion of
rock XX (XX) - indicates that an area is intruded by rock XX [XX] - indicates that an intrusive rock contains xenoliths
of rock XX
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RM0201-113
2566–8 Ma (8)
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