Scale 1:20 000
This Map
Location Map
River
EnaLake
ATHABASCA
DavyLake
BeaverlodgeLake
Tazin
Lake
RichardsLake
Engler
LakeHelmer
SquirrelLake
OldmanLakeNicholson
NevinsLake
Lake ForsythLake
RiouLake
LakeThicke
LakeBox
OmanLake
Lake
Picea
FontaineLake
Lake
74N-01
74N-08
74N-09
74O-04 74O-03 74O-02
74O-05 74O-06 74O-07
74O-12 74O-11 74O-10
74O-1574O-1474O-1374N-16
74K-16 74J-13 74J-14 74J-15
74N-10
74O-01
74O-08
74O-09
74N-07
74N-15 74O-16
74N-02
74J-1674K-15
-108°
-108°
-107°
-107°
59°59°
60°
Uranium City
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 herei n 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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Zs
Zp
Zp
Gbp
Map
Glg
Zp
Mq
Map
GbpZp
Mq
Zs
ZsMq
Mq
Mq
Zp
Zp
Et
Et
Zp
Zp
Zp
Map
Zs
Zp
Mq
Not Exposed
Zp
Zp
MFr-ps
Zs
Egt
Et
Zp
Mq
Zs
Et
Zs
Et
Et
Et
EgpMq
Glg
Egg
Glg
Etg
Egp
Map
Gdg
Mq
Gbp
Gbp
Mq
ZsEgg
Zs
Eqg
Mq
Mq
Gdg
Map
EggZp
Gbp
Zs
MqMap
Map
Map
Zs
Glg
MapZs
Map
Map
Map
Map
Map
Map
MapMq
Map
Map
Mq
Mq
Mq
Map
Map
Mq
Lake Athabasca
Egp
Zp
Zp
Zp
Mq
MFr-ps
MFr-ps
MFr-ps
Zp
Zp
Zp
Zp
Zp
Zp
Egt
Egt
Marian Lake
Lepus Island
Isle Brochet
Natukam Peninsula
Neil Bay
Point Creek
Dempsey Bay
Clark Islandpy
gm
gm
gm
gm
Fel
Fes
Fes
Feo
Feo
U-1565
U-1567
Fes
347000
347000
348000
348000
349000
349000
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000
107°36'0"W
107°36'0"W
59°24
'0"N
59°24
'0"N
0 0.5 1 1.5 20.25Kilometers
0 0.25 0.5 0.75 10.125Miles
Catalogue Number 2006- 4.2- (3.2)
Project M.123 of 2006 The area was mapped by K.E. Ashton (project leader), B.R. Knox, and K.M. Bethune, in the summer of 2006, with the assistance of J. Marcotte, B. McEwan, L. Richan, and A. Kaczowka. This map was printed from the geologist’s digital file. Geological data were processed using Pendragon Forms, Microsoft Access, and ArcView 9.1 software. Base maps were compiled from 1:50 000 scale digital topographic maps licensed from Saskatchewan Information Services Corporation. Grid coordinates are NAD 83 UTM zone 13. The map was processed overall using ArcView 9.1 software. The map is issued in a package with the Summary of Investigations 2006 Volume 2, Saskatchewan Geological Survey, and is available separately. This map accompanies the following publication: Ashton, K.E., Knox, B.R., Bethune, K.M., and Marcotte, J. (2006): Bedrock Geology along the Northern Margin of the Athabasca Basin West of Fond-du-Lac (NTS 74O/5, 6), South-Central Beaverlodge Domain, Rae Province (The Fond-du-Lac Project): in Summary of Investigations 2006 Volume 2, Saskatchewan Geological Survey, Sask. Industry and Resources, Misc. Rep. 2006-4.2. This map may be referenced as: Ashton, K.E., Knox, B. and Bethune, K.M. (2006): Bedrock Geology of the Western Fond-du-Lac Area, South-Central Beaverlodge Domain (Fond-du-Lac Project) (Part of NTS 74O/5 and /6) Central Sheet; 1:20 000 scale prelim. map with Summary of Investigations 2006 Volume 2, Saskatchewan Geological Survey, Sask. Industry and Resources, Misc. Rep. 2006-4.2.
Bedrock Geology of the Western Fond-du- Lac Area, South-Central Beaverlodge Domain (Fond-du-Lac Project) (Part of NTS 74O/5 and 6) Central Sheet at 1:20 000 scale Preliminary Geological Map (2006) by K.E. Ashton, B. Knox and K.M. Bethune
PALEOPROTEROZOIC ROCKS
ATHABASCA GROUP
Manitou Falls Formation, Raibl Member: sandstone and pebbly sandstone with MFr-ps thin mudstone beds: white to pink-red, planar and trough crossbedded, rare clay
intraclasts
----------------- Unconformity ---------------
------------ D4: N-trending open upright folds -------
POST-TECTONIC DYKES
Aplite dyke: pale pink, fine to medium grained (1 mm), massive, homogeneous, sharp contacts, NE trending, CI 3 (biotite-feldspar ± quartz ± amphibole); contains
centimetre-scale mafic-ultramafic inclusions; intruded into lamprophyre dyke
Felsite dyke: pale pink, light grey to pink-red weathering, grey to pink-red on fresh surface, aphanitic, generally straight sided but splay at ends, up to 2 m thick, NE
trending, local biotite and fluorite along internal fractures, commonly uraniferous
Granite dyke: pink and grey, medium grained with K-feldspar phenocrysts up to 1 cm long, massive to weakly foliated (locally oblique to dyke wall by up to 20),
homogeneous but several phases distinguished by grain size, straight sided but splay at ends, up to 50 m thick, NE trending, CI 5-15 (biotite-quartz-K-feldspar-plagioclase); intruded by some lamprophyres but intrusive into others
Lamprophyre dyke: pink to brown, fine to medium grained with phlogopite and rare
pyroxene/amphibole phenocrysts, massive to weakly foliated (igneous?), homogeneous to multi phase; sharp contacts, straight sided, up to 10 m thick (generally 1-2 m), mostly NE trending, CI 20-55 (phlogopite-pyroxene/amphibole-K-feldspar; locally contains decimetre-scale angular to rounded granitoid inclusions and centimetre-scale mafic-ultramafic inclusions; locally intruded into granite and felsite dykes
Granitic gneiss: >70% pink-white and grey, medium-grained leucogranite– Etg leucotonalite having CI <10 (pyroxene -quartz-feldspar ± biotite ± garnet), blue quartz
common; rest grey fine-grained layers and inclusions of granite -tonalite and granite-quartz monzonite - plagioclase-phyric gabbro units (Et and Eqp) up to 1 m thick; generally non-magnetic
Geological contact Bedding
Main S1 foliation (dip unknown , inclined, vertical) S2 foliation S3 foliation (dip unknown, inclined)
Dyke (inclined, vertical) Intersection lineation Lineation of unknown origin (mainly related to F2 and F3 folding)
Minor S fold (F2, F3, F4) Minor Z fold (F2, F3, F4)
Minor W fold (F2, F3) Minor symmetrical fold (F2, F3, F4) F2 axial plane F3 axial plane (inclined, vertical) F4 axial plane (inclined, vertical)
Lineament and possible brittle fault Approximate outline of positive aeromagnetic anomaly
Contour Interval: 50 feet Road Reef
Mineral Occurrence U-1563 - U occurrence with Saskatchewan Mineral Deposit Index number Pb-1571 - Pb occurrence with Saskatchewan Mineral Deposit Index number gm - gummite U stain py – pyrite Feo - oxide-facies iron formation Fes - sulphide facies iron formation Fel - silicate-facies iron formation
Note 1: The thickness of minor quartzite occurrences has been exaggerated to emphasize their stratigraphic importance. Note 2: All glacial data has been placed on a separate map in this volume entitled: Fond-du-Lac Project: Ice Flow Indicators, Western Fond-du-Lac Area, South-Central Beaverlodge Domain (Parts of NTS 74O/5 and 6), 1:50 000 scale, Preliminary Geological Map (2006), by J.E. Campbell, K.E. Ashton and B. Knox.
Symbols
-------------- D3: NE-trending folds ---------------- SYN-TECTONIC INTRUSIVE ROCKS
Pegmatitic granite dyke: pink, massive to foliated, straight sided, locally folded, CI <5 (biotite-quartz-feldspar ± garnet ± muscovite ± tourmaline), variably recrystallized
coarse biotite books -------------- D2: WNW-trending folds ----------------
------------- D1: gneissosity, partial melting -------
Garnetiferous leucogranite: white to pale pink, medium grained, homogeneous to Glg gneissic, minor psammopelitic schlieren; CI 1-10 (garnet-quartz-feldspar ± biotite);
non magnetic
MURMAC BAY GROUP (Ca. 2.33 Ga)
Pyribolite: black to brown, medium grained; homogeneous to layered, CI 40-60 Map (orthopyroxene-clinopyroxene-plagioclase-magnetite hornblende biotite);
variably magnetic, locally very high
Quartzite, minor psammite: quartzite white to pink, fine to medium grained, CI <10 Mq (quartz ± feldspar ± diopside ± biotite ± garnet ± cordierite); psammite grey-brown,
fine to medium grained, CI <10 (biotite chlorite-quartz-feldspar ± garnet ± sillimanite ± cordierite ± diopside); non-magnetic
--------------- Unconformity ------------------------
ARCHEAN AND PROBABLE ARCHEAN ROCKS
WEST-CENTRAL PLUTONIC ROCKS
Biotite-pyroxene gneiss: pink-brown and grey, fine to medium grained, gneissic Gbp due to partial melting and local compositional differences particularly at margins, CI
5-30, (biotite-pyroxene-quartz-feldspar ± garnet ± graphite); local diopsidite boudins, particularly near contacts; commonly injected by ~20% pyroxene granite sheets and intruded by pyribolite dykes up to 5 m thick; non-magnetic; (possibly altered basement to Murmac Bay Group)
Adair Bay pluton: pink and grey, medium grained, homogeneous to gneissic, Gab granitic to tonalitic, CI 10-35, (orthopyroxene-biotite-quartz-K-feldspar-plagioclase);
weakly magnetic
Foliated to gneissic granite-granodiorite: pink-light brown, medium to coarse Gdm grained with rarely preserved feldspar augen up to 2 cm long; homogeneous to well
layered due to injected leucosome and local strain gradients; CI 10-25, (pyroxene-biotite-quartz-plagioclase-K-feldspar ± garnet); intruded by mafic dykes; non-magnetic; (probably correlative with 2.6 Ga Dead Man Granite to west)
Garnetiferous diatexite/granite: white or pale pink and grey, medium grained,
Gdg homogeneous to locally gneissic with variably preserved melanosome and schlieren of psammopelitic to pelitic gneiss (Zp), CI 10-20 (garnet-biotite-quartz-feldspar ± orthopyroxene); (most derived by near-complete melting/homogenization of Zp, but some may be border phase of Gdm contaminated by adjacent Zp); non-magnetic
SUPRACRUSTAL ROCKS
Psammitic to psammopelitic gneiss, minor quartzite: white-pale pink and grey,
Zs fine to medium grained, CI 5-15 (biotite-quartz-feldspar ± garnet ± cordierite ± sillimanite ± graphite), commonly interbedded with minor psammopelite to pelite; non-magnetic
Psammopelitic to pelitic gneiss: white-pale pink and grey-brown to rusty, fine to
Zp coarse grained, well layered due to compositional variation and abundant leucosome, garnet up to 8 cm in diameter with abundant sillimanite, local decimetre-scale pods of garnetite, CI 10-30 (garnet-sillimanite-biotite-quartz-K-feldspar ± plagioclase ± cordierite ± graphite); (grades into garnetiferous diatexite/granite - Gdg); non-magnetic
EASTERN PLUTONIC COMPLEX
Garnet-pyroxene granite: pink-brown to grey, medium grained, foliated, Egg homogeneous to vaguely layered, CI 5-10 (garnet-pyroxene-biotite-quartz-feldspar-
ilmenite?), garnet locally up to 1 cm diameter, locally contains mafic layers (dykes or dioritic inclusions), minor hybrids; non-magnetic
Pyroxene granite: white-cream to pink-brown and grey, medium grained with rarely
Egp preserved feldspar augen up to 1 cm long, foliated, homogeneous, CI 10-20 (pyroxene-hornblende-biotite-quartz-plagioclase-K-feldspar); 25% injected pale pink-grey centimetre-scale granite leucosome; weakly magnetic
Granite-quartz monzonite and plagioclase-phyric gabbro: Granite-quartz
Eqp monzonite phase: pink and grey, coarse grained, homogeneous, CI 35 (hornblende-pyroxene-biotite-magnetite-plagioclase-K-feldspar-quartz), quartz blue, net veined by pyroxene granite sheets; Gabbro phase: brown to grey-black, medium grained with rarely preserved 1 cm long plagioclase phenocrysts, homogeneous, CI 30-50 (pyroxene-hornblende-biotite-magnetite-plagioclase ± quartz); injected by up to 70% granitic sheets; strongly magnetic
Garnetiferous quartzofeldspathic gneiss: pink, white, or grey, medium-grained,
Eqg homogeneous to gneissic with CI 2-20 (garnet-biotite-quartz-feldspar ± orthopyroxene ± graphite), garnet variably altered and weathered out, quartz commonly blue in east, centimetre-scale pods of red garnetite, commonly interlayered with granite-tonalite (Et) at metre scale; locally injected by pyroxene leucogranite sheets; non-magnetic
Garnetiferous granite-tonalite gneiss: white to pink and grey, medium to coarse
Egt grained, homogeneous to gneissic, CI 15-20, (garnet-biotite-quartz-feldspar ± pyroxene), quartz commonly blue, local black garnet-biotite melanosome and white-pink garnetiferous leucosome, rare fine-grained decimetre-scale garnetite layers and pods, intruded by garnetiferous granite sheets and mafic dykes; non-magnetic
Granite-tonalite, minor diorite-gabbro: pink-cream to white and brown-grey,
Et medium to coarse grained, homogeneous to gneissic, CI 10-25 (orthopyroxene- biotite-quartz-feldspar ± hornblende ± rare garnet), quartz generally blue; local metre-scale fine- to medium-grained intermediate to mafic inclusions; injected by up to 70% granitic sheets and rare metamorphosed mafic dykes; generally non-magnetic