cue 1:100 000 geological series map - microsoft · felsic volcanic rock, including andesite, dacite...
TRANSCRIPT
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118°0'
118°0'
117°50'
117°50'
117°40'
117°40'
117°30'
117°30'
27°0' 27°0'
27°10' 27°10'
27°20' 27°20'
27°30' 27°30'
W.A.
Qld
N.T.
S.A.
N.S.W.
Vic.
Tas.
A.C.T
ñBRtg-gm
ñPOg-f
ñSDcr-mgg
ñAN-mg
ñPOm-bñGLw-bk
ñGLw-bk
ñTU-mgñPOm-b
ñANct-gtl
ñSDB-mg
ñANC-mg
ñAN-mg
ñSDB-mg
ñgYMU
ñBRga-gm
ñPOw-mhs
ñPOg-fa
ñPOm-b
ñPOm-b
ñTU-mg
ñJUcl-mgms
ñPOm-mb
ñPOm-mb
ñPOm-mb
ñPOm-b
ñTU-mg
ñAN-mg
ñGLw-f
ñPOm-mukt
ñJU-mgms
ñBRtg-gm
ñSDY-xony-any
ñPOw-mhs
ñJU-mgms
ñPOg-fñTU-mg
ñPO-xmb-mf
ñANgn-odñPOw-sf
ñSDB-mg
ñPOw-sf
ñSDY-xony-any
ñGLr-s
ñAN-mg
ñPOm-mb
ñGLr-s
ñPOg-f
ñANC-mg
ñPOm-mb
ñmapsYMU
ñANC-mg
ñSDY-xony-any
ñPOg-mfs
ñANC-mg
ñANC-mg
ñmusYMU
ñGLr-ssq
ñJU-mgms
ñPOc-xmtq-mi
ñSDB-mgñPOc-xmtq-mi
ñANC-mg
ñPOm-mhszq
ñANC-mg
ñJU-xmgn-mws
ñPOc-xmtq-mi
ñAN-mg
ñPOw-cib
ñSDY-xony-any
ñSDY-od
ñPOm-b
ñPOw-fr
ñmoaYMU
ñPOm-mb
ñPOm-mb
ñGLw-b
ìod
ìod
ìod
ìod
ìod
ìod
ìod
ìod
ìod
zqñPOc-mi
ñPOw-cib
ñPOw-cib
ìod
ìod
ìod
ñBRga-gmñBRtg-gm
ñJU-xmgn-mwsñJU-mgmsñJUcl-mgms
ñPOc-miñPOc-xmtq-mi
ñmapsYMUñmoaYMUñmusYMU
Dolerite dyke, sill or plug
Quartz vein or pod
Metagranite interleaved with subordinate foliated, metamafic rockFoliated biotite metamonzogranite
Granitic rock, undivided
Metamonzogranite to granodiorite
Chlorite–tremolite(–talc) schist AmphiboliteUltramafic schist
ñGLw-fñGLw-bñGLw-bkñGLw-bsñGLw-mus
Felsic volcanic rock, including andesite, dacite and rhyoliteMafic volcanic rocks
Komatiitic basalt with local pyroxene spinifex texture Pyroxene spinifex-textured basalt and local basalt
Ultramafic schist
ñGLr-sñGLr-ssq
Clastic sedimentary rocksQuartz-rich sandstone
Metabasalt and felsic metavolcanic rock
ñPOw-mhs
ñPOw-fr
ñPOw-sfñPOw-cib
Schistose pelite and psammite
Quartz-porphyritic rhyolite
Mudstone, siltstone, and sandstoneBanded iron-formation and ferruginous banded chert
Deformation Event 2 (D2)
Deformation Event 1 (D1)
Wattagee Formation
Ryansville Formation
Wilgie Mia Formation
Greensleeves FormationñPOg-mfsñPOg-fñPOg-fa
Felsic schist derived from volcanic rockAndesitic to rhyolitic volcanic and volcaniclastic rocks
Andesite
Meekatharra FormationñPOm-mhsñPOm-mbñPOm-bñPOm-mukt
Schistose pelite and psammiteMetamafic rockMafic volcanic rock dominantTalc–carbonate(–chlorite–serpentine) schist
Coodardy Pool Formation
Walg
anna
Suit
eBa
ld Ro
ck S
uper
suite
Jung
ar S
uite
Tuck
anar
ra
Suite
Glen
Gro
upPo
lelle
Grou
p
Murc
hison
Sup
ergr
oup
ñSDB-mgñSDcr-mgg
ñSDY-xony-anyñSDY-od
Layered mafic–ultramafic intrusive rocksDolerite
Metagranite
ñANct-gtlñANC-mg
Gnanagooragoo Igneous Complex
Metagranite
Cue Tonalite
Anne
an S
uper
suite
Cullc
ulli S
uite
Austi
n Do
wns S
uper
suite
Yalgo
wra
Suite
Big B
ell S
uite
Murc
hison
Dom
ain
Crossroads Granodiorite
Garden Rock MonzograniteTelegootherra Monozogranite
Chunderloo Monzogranite
Metatonalite, metagranodiorite, and metatrondhjemite
Quartzite and metamorphosed iron formationMetamorphosed iron formation
Youa
nmi T
erra
ne
YILGA
RN CR
ATON
ñGLw-b
ñGLr-s
ñPOg-f
ñGLw-f
ñSDY-od
ñgYMU
ñTU-mg
ñPOw-fr
ñSDB-mg
ñAN-mg
ñANC-mg
ñPOm-b
ñPOw-sf
zq
ñANct-gtl
ñPOg-mfs
ñPOm-mb
ñANgn-od
ñBRtg-gm
ñGLw-mus
ñJU-mgms
ñmusYMU
ñPOw-mhs
ñmoaYMU
ñPOm-mhs
ñBRga-gm
ñSDcr-mgg
ñPOm-mukt
ñmapsYMU
ñPOg-fa
ñJUcl-mgms
ñPO-xmb-mf
ñGLw-bsñGLw-bk
ñGLr-ssq
ñSDY-xony-any
ñPOc-xmtq-mi
ìod
ñJU-xmgn-mws
ñPOw-cib
ñPOc-mi
Murch
ison D
omain
Youa
nmi T
erra
ne
YILG
ARN
CRAT
ON
Colluvial units
C§fC§gC§q
Sheetwash units
W§fW§l
W§c
Wf
Alluvial unitsA¢A¤A§A¹Ak
Lacustrine unitsL¤L¥e¨L§L¨k
L²Lk
L®k¤
L¥1
Eolian unitE¦q
Lacustrine unit, first generationL¥2
Residual or relict unitsR´fR´fp¨
R´zzRµgRµl
R´gp¨
RkRkp¨
ñBRG-gyhñBRga-gmñBRtg-gmñBRtg-gmdvñBRtg-gmv
Deformation Event 2 (D2: 2665–2640 Ma)
ñmzqYMUñgmapYMU
C
ñJU-xmgn-mwsñJU-mgmmñJU-mgmsñJUcl-mgms
Deformation Event 1 (D1: 2676–2665 Ma)
ñTU-mggñTU-mgmñTU-mgmlñTU-gmap
ñmapsYMUñmaxYMUñmoaYMUñmwasYMUñmusYMUñodYMU
WATTAGEE FORMATION
ñGLw-mfsñGLw-mlv
ñGLw-fañGLw-fdñGLw-bkñGLw-bkoñGLw-bs
RYANSVILLE FORMATIONñGLr-mhsñGLr-sfñGLr-ssq
WILGIE MIA FORMATIONñPOw-mhsñPOw-sl
ñPOw-stñPOw-ssqñPOw-cibñPOw-fr
GREENSLEEVES FORMATIONñPOg-mhsñPOg-mlvñPOg-mfsñPOg-mfdsñPOg-fnñPOg-fañPOg-fdtñPOg-frmb
MEEKATHARRA FORMATION
ñPOm-xmba-mgp
ñPOm-mhs
ñPOm-mbñPOm-mbañPOm-mbanñPOm-mbasñPOm-mbbñPOm-mbbsñPOm-mbbyñPOm-mbmñPOm-mbmhñPOm-mbms
ñPOm-fnl
ñPOm-bbñPOm-bbo
ñPOm-bkñPOm-bko
ñPOm-bs
COODARDY POOL FORMATIONñPOc-xmtq-miñPOc-xmtq-maps
ñPOc-miñPOc-mtq
Dolerite dyke, sill or plug; fine- to medium-grained dolerite and gabbro
Quartz vein or pod; massive, crystalline, or brecciated; age uncertain
Hornblende syenite; contains amphibolite inclusionsmonzogranite to syenogranite; undeformed
monzogranite to syenogranite; undeformed, but with common igneous flow fabricsMuscovite-bearing pegmatitic monzogranite to syenogranite; undeformedMuscovite-bearing monzogranite; medium to coarse grained; undeformed
Fine-grained porphyritic monzogranite, as dykes; weakly metamorphosed; locally foliated
Metagranite interleaved with subordinate, foliated, metamafic rock; gneissic banding developed locallyMuscovite metagranite; medium to coarse grained, equigranular; foliatedFoliated biotite metamonzogranite; minor metagranodiorite, metasyenogranite, and pegmatite; fine to coarse grained; locally gneissic
biotite metamonzogranite; commonly with abundant K-feldspar phenocrysts/porphyroclasts; well foliated to mylonitic; may include amphibolite lenses
Foliated metagranodiorite; medium grained to K-feldspar porphyriticMetamonzogranite; medium to coarse grained, K-feldspar porphyritic; foliatedMedium-grained, leucocratic metamonzogranite; foliatedQuartz and feldspar porphyritic, fine-grained monzogranite; locally foliated
Chlorite–tremolite(–talc) schist derived from peridotiteMetapyroxenite; medium grained; deeply weatheredAmphibolite; medium to coarse grained; derived from dolerite and gabbroStrongly foliated amphibolite and amphibolite schist; commonly also lineatedUltramafic schistDolerite; medium grained; massive, locally weakly deformed; metamorphosed
Quartz–sericite schist derived from felsic volcanic rock; metamorphosedLight- to dark- grey slate; yellow weathering; highly fissile; metamorphosed
Fine-grained, intermediate volcanic rock; weakly metamorphosedDacite; massive, fine to medium grained; locally plagioclase-phyric; weakly metamorphosedKomatiitic basalt with local pyroxene spinifex texture; weakly metamorphosed
Pillowed komatiitic basalt with common pyroxene spinifex texture; weakly metamorphosedPyroxene spinifex-textured basalt and local basalt; locally variolitic; weakly metamorphosed
Schistose pelite and psammite; local biotite porphyroblasts and minor bands of felsic volcaniclastic rockSiltstone and fine- to coarse-grained sandstone; common graded bedding; local fracture cleavage; weakly metamorphosedQuartz-rich sandstone; common fracture cleavage; weakly metamorphosed
Ultramafic schist; commonly deeply weathered
Chert-pebble to boulder conglomerate; generally well sorted; weakly metamorphosed
Schistose pelite and psammite with local biotite porphyroblastsSiltstone; massive to faintly bedded with fine-grained sandstone; local fracture cleavage; weakly metamorphosed
Sandstone; fine to coarse and locally graded; weakly metamorphosedQuartz-rich sandstone; common fracture cleavage; weakly metamorphosedBanded iron-formation and ferruginous banded chert; minor jaspilite and hematite-rich rock; minor volcaniclastic sandstone; metamorphosedQuartz-porphyritic rhyolite; weakly deformed and metamorphosed
Schistose pelite and psammite; locally contains biotite porphyroblastsWhite to grey slate; highly fissile; locally grades to fine-grained sandstoneFelsic schist derived from volcanic rock; commonly deeply weatheredDacitic schist; locally feldspar (and quartz) porphyritic; rare graded beddingFelsic volcanic and volcaniclastic rock, undivided; metamorphosed; commonly deeply weathered and kaolinizedAndesite; massive to fragmental, with siliceous clasts; pale grey weathering, silicifiedGrey, dacite and dacitic volcaniclastic rocks; commonly with plagioclase phenocrysts; locally vesicular; weakly metamorphosedCrystal-vitric rhyolite breccia and volcaniclastic sandstone; locally foliated; weakly metamorphosed
Amphibolite derived from basalt with sheared metapegmatite veins; strongly transposed, foliated, lineated, and folded; minor meta iron-formation
Schistose pelite and psammite with local biotite porphyroblasts
Metamafic rock; generally fine to medium grained; foliated to schistoseAmphibolite derived from basalt; massive to foliated and/or lineatedAmphibolite gneiss derived from basalt; commonly well foliated and lineatedAmphibolite schist derived from basalt; fine to medium grained; commonly also lineatedMetabasalt; generally fine grained and massive; locally pillowed and/or vesicularStrongly foliated metabasalt and local amphiboliteMylonitic metabasalt; fine grained to very fine grained; commonly lineatedMetakomatiitic basalt; massive to pillowed with local hyaloclastite; with fracture cleavage, or foliatedMetakomatiitic basalt breccia; includes rounded, vesicular pillow fragments to 30 cm and monomict volcaniclastic conglomerate; undeformed to foliatedFine-grained ultramafic schist derived from komatiitic basalt; local talc–carbonate rock; commonly deeply weathered
Felsic volcaniclastic siltstone; locally grades to fine-grained volcaniclastic sandstone; weakly metamorphosed
Basalt; massive to weakly foliated; locally pillowed and/or vesicular; metamorphosedPillowed basalt; locally fractured to foliated; weakly metamorphosed
Komatiitic basalt; locally pillowed and/or variolitic; fractured to locally foliated; weakly metamorphosedPillowed komatiitic basalt; local fine pyroxene spinifex texture; weakly metamorphosed
Pyroxene spinifex-textured basalt and minor basalt; locally variolitic; metamorphosed
Quartzite and metamorphosed iron formation; well foliatedQuartzite with interlayered metaperidotite schist
Metamorphosed iron formation; weakly layered; strongly foliatedQuartzite; medium grained; foliated
felsic volcaniclastic rocks and banded iron-formation; local quartzite; widely intruded by layered gabbroic to periodotite sills; metamorphosed (section only)YALOGINDA FORMATION:
ñANct-gtlñANC-mgtnñANC-mgtañANC-mggañANC-mg
ñAN-gmapñAN-mgtnñAN-mgnñAN-mgmuñAN-mgmsñAN-mggsñAN-xmgn-mgmñAN-xmgm-mfsñAN-xmggs-gmdñAN-xmg-mba
GNANAGOORAGOO IGNEOUS COMPLEX:
ñSDY-adñSDY-apñSDY-axñSDY-ogyñSDY-oglñSDY-ogñSDY-od
ñGLw-mus
ñGLr-scc
ñPOm-mukt Talc–carbonate(–chlorite–serpentine) schist derived from ultramafic volcanic rock; commonly deeply weathered and lateritized
MURROULI BASALT: strongly foliated metabasalt and local amphibolite
ñSDB-mgmñSDB-mgmsñSDB-mgmuñSDcr-mggñSDcr-mggnñSDcr-xmgm-gmp
leucocratic tonalite; medium to coarse grained; metamorphosedTonalitic gneiss; medium grained; strongly foliatedMetatonalite with hornblende phenocrysts and common, small, elliptical mafic xenolithsHornblende-bearing metagranodiorite with minor metatonalite; contains scattered, small, mafic xenoliths
Metatonalite, metagranodiorite, and metatrondhjemite; typically hornblende bearing, and with common mafic clots
Fine-grained granite, commonly as dykes in greenstones; quartz (and feldspar) porphyritic to locally even grained; locally schistoseFine-grained biotite tonalite gneiss; includes crosscutting younger phases and pegmatitesMedium-grained granitic gneiss; locally muscovite bearing; strongly foliatedK-feldspar and quartz porphyritic biotite metamonzogranite; strongly foliatedFoliated biotite metamonzogranite, with local K-feldspar phenocrysts; common pegmatite veinsBiotite metagranodiorite; strongly foliated; commonly with pegmatite and leucogranite veinsMedium-grained biotite granite gneiss cut by sheets of metamonzogranite; varies to migmatitic gneissFoliated metamonzogranite with slivers and rafts of fine-grained felsic schistMedium-grained, foliated to gneissic metagranodiorite with abundant pegmatite veinsFoliated, heterogeneous metagranite with dismembered trains of amphibolite xenoliths; commonly with abundant pegmatite
Biotite metamonzogranite; generally leucocratic; commonly foliated (section only)Metamonzogranite; locally quartz porphyritic; strongly foliatedK-feldspar megacrystic biotite metamonzogranite; strongly foliated
metagranodiorite; commonly foliatedBiotite metagranodiorite; strongly foliated; commonly with pegmatite veins and other intrusive granitic phasesPegmatite-layered metamonzogranite gneiss
Dolerite; weakly metamorphosed and locally weakly foliatedGabbro; massive to weakly foliated; local dolerite, quartz gabbro, and gabbronorite; weakly metamorphosed
Gabbro; fine to medium grained, with compositional layering; weakly metamorphosedPyroxenite; medium to coarse grained; weakly metamorphosedPeridotite; fine to medium grained; serpentinized and locally foliatedDunite, with local relict cumulate texture; serpentinized
2820 Mac.
c. 2800 Ma
2800–2760 Ma
c. 2761 Ma 3
2752–2735 Ma
2735–2725 Ma
2725 Ma
c. 2676 Ma
2665–2640 Ma
c. 2623 Mac. 2617 Ma 1 GARDEN ROCK MONZOGRANITE:
TELEGOOTHERRA MONZOGRANITE:
CHUNDERLOO MONZOGRANITE:
PHAN
EROZ
OIC
PROT
EROZ
OIC
ARCH
EAN
Murc
hiso
n Su
perg
roup
Norie
Gro
upPo
lelle
Gro
upGl
en G
roup
Tuck
anar
ra S
uite
Jung
ar S
uite
Bald
Roc
k Su
pers
uite
Walg
anna
Sui
te
Aust
in D
owns
Sup
e rsu
ite
Yalg
owra
Sui
teBi
g Be
ll Su
iteCu
llcul
li Su
ite
Colluvium derived from different rock types; includes gravel, sand, and siltColluvial footslope deposits containing ferruginous gravel and reworked ferruginous duricrust Colluvial footslope containing quartzofeldspathic gravel, sand, and silt commonly derived from granite and associated weathering productsQuartz-vein debris on colluvial footslope
Clay, silt, and sand with abundant ferruginous grit on sheetflood fanClay, silt, and sand on sheetflood fan; local ferruginous gravel
Very low gradient sheetflood deposits, with numerous claypans; includes sand and silt
Clay, silt, and sand sheetwash deposits, with abundant ferruginous grit
Clay, silt, sand, and gravel on alluvial plainsClay, silt, sand, and gravel in fluvial channels Clay, silt, and sand on floodplainsAlluvial fan deposits; includes gravel, sand, and siltCalcrete and carbonate-cemented alluvium in fluvial channels
Clay and silt in lakes and localized depressionsLithified and unconsolidated gypsum and clay, in mounds and dunes adjacent to playa lakesFreshwater lakes, commonly surrounded by swampsBedded carbonate, silt, and clay deposits in shallow lakes adjacent to streams and rivers
Saline and gypsiferous evaporite deposits, clay, silt, and sand in playa lakesCalcrete and carbonate deposits within lake systems
Calcareous lake deposit; predominantly cemented calcite
Dune and lake deposits; active systems within and adjacent to playa lakes; non-vegetated or poorly vegetated
Eolian sand, in sheet deposits and dunes; iron-stained
Stabilized dunes within and adjacent to playa lakes; typically vegetated
Ferruginous duricrust, massive to rubbly; includes iron-cemented reworked productsFerruginous duricrust, massive to rubbly; derived from granitic rocks; includes iron-cemented reworked products
Silcrete; cobbles of silicified rock in silica cementQuartzofeldspathic sand, commonly over graniteYellow sand with minor pisolitic laterite, ferruginized silcrete, silt, and clay; common on low plateaus associated with weathered granite
Undivided residual or relict material; mainly ferruginous and quartzofeldspathic duricrust over deeply weathered granite; minor kaolinized rock; includes mottled and leached zones of weathering profile
Residual calcrete and nodular carbonate deposits; includes reworked carbonate productsCalcrete and nodular carbonate, developed over deeply weathered granite; includes reworked carbonate products
dolerite; medium grained with local fine- and coarse-grained layers;
Metamorphosed hydrothermal vein quartz; sucrosic, recrystallized texture; locally foliated and/or lineated
2815–2800 Ma
CROSSROADS GRANODIORITE:
CUE TONALITE:
ñodYMU
zq
ñmzqYMU
ñmaxYMU ñmwasYMU
ñPOm-mbmh
massive, locally weakly deformed; metamorphosed
Anne
an S
uper
suite
ñPOw-sf Mudstone, siltstone, and sandstone, showing local bedding; weakly metamorphosed
Lacustrine unit, second generation
CENO
ZOIC
C
A§
L§
A¹A¤A¢
L²
Wf
Lc
Ak
Lk
C§f
RkRµl
W§f
L¥1
W§lC§q
L¥2
E¦q
C§g
L¨k
Rµg
W§c
L®k¤
R´zz
L¥e¨
Rkp¨R´gp¨R´fp¨R´f
ñANC-mg
ñPOm-mb
ñSDY-ax
ñGLr-sf
ñGLw-bk
ñSDY-ad
ñSDY-od
ñSDY-ap
ñPOm-bkñPOm-bb
ñSDY-ogl
ñPOw-fr
ñPOg-fn
ñGLr-scc
ñPOw-sl ñPOw-st
ñGLw-fa ñGLw-fd
ñPOw-sf
ñSDY-ogy
ñGLw-bs
ñPOg-fdt
ñGLr-ssq
ñTU-mgg
ñANct-gtl
ñPOm-bs
ñBRG-gyh
ñAN-mgn
ñGLr-mhs
ñTU-mgm
ñPOg-mlv
ñGLw-mlv
ñAN-mgtn
ñPOg-mfs
ñGLw-mfs
ñANgn-od
ñPOw-ssq
ñTU-mgml
ñAN-mggs
ñPOg-mhs
ñTU-gmap
ñGLw-mus
ñJU-mgms
ñmusYMU
ñPOg-frmb
ñPOw-mhs
ñmoaYMU
ñPOm-mhs
ñAN-mgms ñAN-mgmu
ñPOg-mfds
ñPOm-mbb
ñBRga-gm
ñJU-mgmm
zq
ñPOm-mukt
ñPOm-mbm
ñNOy-xf-cib
ñmapsYMU
ñgmapYMU
ñJUcl-mgms
ñPOm-mbbs ñPOm-mbby
ñNOm-mbbs
ñSDB-mgm
ñANC-mgtn
ñPOm-mbms
ñANC-mgta
ñGLw-bko
ñPOm-bko
ñANC-mgga
ñPOm-bbo
ñPOc-xmtq-mi
ñSDB-mgms
ñAN-xmg-mba
ñSDB-mgmu
ñAN-xmgm-mfs
ñJU-xmgn-mws
ñPOm-mbas
ñPOm-mban
ñSDcr-mggn
ñAN-xmgn-mgm
ñBRtg-gmdv
ñAN-xmggs-gmd
ñPOc-xmtq-maps
ñPOm-xmba-mgp
ñSDcr-xmgm-gmp
ìod
ñBRtg-gmv
ñSDY-og
ñPOg-fa
ñPOc-mi
ñBRt-gm
ñPOw-cib
ñPOm-fnl
ñAN-gmap
ñPOm-mba
ñPOc-mtq
ñSDcr-mgg
c. 2759 Ma 3c. 2748 Ma
c. 2747 Ma
c. 2702 Ma c. 2724 Ma
c. 2735 Ma
c. 2744 Ma
c. 2757 Ma
c. 2737 Ma 2
Leucogabbro, coarse grained; locally with alternating layers of melanocratic and leucocratic gabbro; generally massive; weakly metamorphosed
CUEGEOLOGICAL SURVEY OF WESTERN AUSTRALIAAUSTRALIA 1 : 100 000 GEOLOGICAL SERIES SHEET 2443
DIAGRAMMATIC SECTIONB
True north, grid north, and magnetic north areshown diagrammatically for the centre of themap. Magnetic north is correct for 2010 and
moves westerly by approx. 40" annually
TN
GNMN
GRID / MAGNETICANGLE 09°
GRIDCONVERGENCE
0.3°
SCALE 1:500 000
INTERPRETED BEDROCK GEOLOGY
ñSDcr-mggnñSDcr-mggn ñANct-gtlñSDY-ogñPOm-bb
ñBRtg-gm
ñPOg-fa
ñJU-mgmsñTU-mgml
ìodñPOm-bb
ñSDB-mgm
ñPOg-fdtñANC-mg
ñPOm-mbañPOm-bb
ñTU-mgm
ñGLw-bs
ñAN-mgms
ñPOg-fdt
ñPOm-bk
ñAN-mgn
ñPOm-bkñPOm-bk
ìodñNOy-xf-cib
ñPOm-mbms
ñPOm-bk
ñNOm-mbbsñPOg-mlv
ñPOm-mban
ñPOm-bb ñPOm-mba
ñPOm-mbms
ñPOm-mukt
ñSDY-og
ñPOm-mban
ñPOm-bb
ñAN-mgms
ñPOm-mbbsñTU-mgml
ñSDY-og
ñPOm-bbñGLw-bko
ñSDY-og
ñPOm-mbbsñPOg-mfsñAN-mggs
ñBRtg-gm
ñAN-xmggs-gmdñPOm-mbms ñPOg-frmb
ñJU-mgms
SEA LEVEL
2 km
4 km
A
0 5 10 15 20
Kilometres
For further details refer to main reference
SEA LEVEL
2 km
4 km
BERINGARRA CUE ROAD GREAT NORTHERN HIGHWAYNallan CreekC
Wond
inong
60 km
Meek
atharr
a 92
kmCo
gla Do
wns H
omes
ted 11
0 km
Grea
t Nort
hern
Highw
ay 8 k
m
Beebyn Homestead 10 kmBeebyn Homestead 23 kmMadoonga Homestead 10 km
Kalli H
omest
ead 4
2 km
Mount Magnet 80 kmLakeside Homestead 42 km
BELELESG 50-11
BYROSG 50-10
CUESG 50-15
MURGOOSG 50-14
CUE2443
KALLI2344
MEKA2243
BYRO2145
REEDY2543
TARDIE2142
AUSTIN2442
MILEURA2345
TIERACO2545
MURGOO2143
NOONDIE2343
BOOLARDY2244
MADOONGA2444
MILLY MILLY2245
MELANGATA2242
KOONMARRA2445
WYNYANGOO2542
DALGARANGA2342
BILLABALONG2043
BADGERADDA2044
MEEKATHARRA2544
BOOKA BOOKA2045
CHULYAWARRA2144
MUGGAMURRA2042
SHEET INDEX
1 : 100 000 maps shown in black1 : 250 000 maps shown in brown
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COODARDY NOONDIE ROAD COODARDY NOONDIE ROAD
Geological boundary
exposed...............................................................................................................Fault or shear
exposed..............................................................................................................
interpreted...........................................................................................................
CUE
UNIVERSAL TRANSVERSE MERCATOR PROJECTIONHORIZONTAL DATUM: GEOCENTRIC DATUM OF AUSTRALIA 1994
VERTICAL DATUM: AUSTRALIA HEIGHT DATUM
Grid lines indicate 1000 metre interval of the Map Grid Australia Zone 50
©
The Map Grid Australia (MGA) is based on the Geocentric Datum of Australia 1994 (GDA94)GDA94 positions are compatible within one metre of the datum WGS84 positions
Kilometres
1000 0 1 2 3 4 5 6 7 8 9 10
SCALE 1 : 100 000
Metres
80
70
85
75
70
70
70
Fold, showing axial trace and generalized plunge direction
Small-scale fold axial surface, showing strike and dipinclined................................................................................................................
Small-scale fold axis, showing trend and plungeunspecified..........................................................................................................
antiform...............................................................................................................S-vergence...........................................................................................................
M-vergence..........................................................................................................
Z-vergence...........................................................................................................Bedding, showing strike and dip
inclined................................................................................................................vertical.................................................................................................................
overturned...........................................................................................................
Igneous layering, showing strike and dip
inclined................................................................................................................vertical.................................................................................................................
Igneous flow banding, showing strike and dipinclined................................................................................................................vertical.................................................................................................................
Igneous contact showing strike and dip
inclined................................................................................................................Way-up indicator
Metamorphic foliation, showing strike and dipinclined................................................................................................................vertical.................................................................................................................
Gneissic banding, showing strike and dip
inclined................................................................................................................Cleavage, showing strike and dip
inclined................................................................................................................vertical.................................................................................................................
Crenulation cleavage, showing strike and dip
inclined................................................................................................................Shear-sense indicator
dextral..................................................................................................................showing dip of foliation
dextralinclined.......................................................................................................
sinistralinclined.......................................................................................................
vertical........................................................................................................reverse...........................................................................................................
Mineral lineation, showing trend and plunge
inclined.................................................................................................................
Mineral alignment, showing trend and plungeinclined................................................................................................................
Igneous lineation, showing trend and plunge
horizontal.............................................................................................................
60
58
65
35
35
42
Stretching lineation, showing trend and plunge
inclined................................................................................................................. 34
Cleavage–cleavage intersection lineation, showing trend and plungeinclined................................................................................................................ 70
anticline; exposed, interpreted.............................................................................syncline; exposed, interpreted.............................................................................antiform; exposed, interpreted.............................................................................
Highway with national route marker..........................................................................
Road, sealed.............................................................................................................Road, unsealed.........................................................................................................Major track................................................................................................................Track.........................................................................................................................
Fence, generally with track.......................................................................................Railway, abandoned..................................................................................................
Townsitepopulation less than 1000...................................................................................
Homestead................................................................................................................
Locality......................................................................................................................Yard..........................................................................................................................Horizontal control; major, minor................................................................................
Breakaway................................................................................................................Contour line, 20 metre interval..................................................................................
Soak, spring..............................................................................................................
Watercourse with ephemeral pool.............................................................................Pool...........................................................................................................................
Bore, well..................................................................................................................
Windpump.................................................................................................................Dam, tank..................................................................................................................
CUE
Yalenberine
Position doubtful........................................................................................................ (PD)
synformal anticline; interpreted............................................................................
trend of bedding..................................................................................................
Trend of bedding or foliation......................................................................................
Isotopic age determination site with identification number........................................ 178194
40
Waterhole..................................................................................................................
Pool
Waterhole
Well
Soak Spring
Pipeline......................................................................................................................
Nallan
40
10
65
82
60
40
Yard
300
Borepipeline
igneous differentiation.........................................................................................
pillow structure....................................................................................................graded bedding....................................................................................................fining upwards sequence.....................................................................................
spinifex texture....................................................................................................
trend of igneous layering.....................................................................................
Bore Well
Aeromagnetic lineament
unspecified..........................................................................................................
Published by the Geological Survey of Western Australia. A free PDF of this map can be downloaded from . Hard copies of this map are available from the Information Centre, Department of Mines and Petroleum, 100 Plain Street, East Perth, WA 6004.Phone (08) 9222 3459 Fax (08) 9222 3444Website Email [email protected]
The recommended reference for this map is:Van Kranendonk, MJ 2010, Cue, WA Sheet 2443,Geological Survey of Western Australia, 1:100 000 Geological Series.
SHEET 2443 FIRST EDITION 2011Version 1.0 – January 2011
Western Australia 2011
RyansvilleAu
Au
W
Fe
Be
CuAu
Cu
Mt MulcahyCu
CuAu
Cu Zn Fe
Tither NorthAu
Au
AuNinden
Zn
Zn, Ag
Cu
Cu
BehringTreasureAu
Au
BehringNorth
PGE
PGE
Zn
WW
WW,Mo
W
CallieSpring Be
SnBe
Coodardy
Big BellAu,Ag
U
ULakeside
ULst
LstLst
Au
AuAu
Au
Au
Au
LstAu
City of Chester
Au
CuCuddingwarra
TreasureTrove
Cu,Zn
Cu,Zn
U
Lst
Au
Au
HiddenTreasure
Kln
Au
Au
AuGolden Gate
Black SwanAu
AuBlackSwanSouth
Black Swann – Rapier
Au
Au
Au
YellowTaxi
Au
TrentonAu
Au
Au
GoldenCrownAu
Try Again
MountainView
Au
GreatFingall
CremeD'OrAu
KinsellaAu
Cu
Cu
DeceiverAu
PrincessRoyal
Au
Au Au
Au
Au
CueNo 1
Au Ag
Au
Cue VictoryAu
Gem of CueAu
Au
Au
Au
SalisburyAu
Light of AsiaDuke of YorkAu
AgamemnonAu
Brle
M U R C H I S O N M I N E R A L F I E L D
C U E D I S T R I C T
D A Y D A W N D I S T R I C T
M E E K A T H A R R A D I S T R I C T
Dam
Bore
TankBore
Bore
Bore
Bore
Bore
BoreBore
Bores
Bore
Bore
Tank
Vat Bore
Pat Well
Ram Well
No 3 BoreNo 2 Bore
Lane Well
No 1 Well Webb Bore
No 4 Well
Bolt Well
Deep Well
Bore with windpump Cocky Well
Well Stock Bore
Bore
Bore
Pinda Well
Milly WellRoddy Well
Milly Bore
Bore with windpump
Well
Well Well
Judas WellWell
Well with windpump Emily Well
No 15 Bore
Smith Well
Depot Bore
Well with windpump
Alice Well
Well with windpump
Dairy Well
Well with windpump
Well with windpump
Well
5 Mile Bore
Middle Bore
Sunday Well
Afghan BoreGidgie Bore
3 Mile Well
Gidgie Well
7 Mile Well
9 Mile Well
Wasley Bore
6 Mile Well
Clinch Well
Garden Well
Midway Bore
Bailey Bore
16 Mile Well
Bore
Clarrie Bore
Railway Bore
Wallace Well
Stewart Well
Wandagee Well
Wattagee Well
Big Tank Well
Boundary Bore
Borehole Bore
Bellevue Bore
Churriga Well
Lakeside Bore
15 Well
Windarra Well
Redgrove Bore
Limestone WellBocadeera Well
Longtime Bore
Tuckiarra Bore
Maffeking Bore
Governess Bore
Riverside Bore
Cavanagah Bore
South Pool Bore
No 1 Well
Deep Bore
Pope Well
Government Well
Cross Road Bore
Government Well
Afghan Rock Well
Milliwarry Well
O'Dea Well
Jeffries Well
Mulcahy Bore (PD)
9 Mile Well Little Milly Well
Larsen Bore
Tootoowannie Well
Water Supply Bore
Berring Bore
Dehring Bore
Martin Corner Bore
Old Homestead Well
Southern Cross Well
Deighton Well
Stockyard Well
Milliwarrie Middle Well
Tank
Nallan
Coodardy
Austin Downs
Old Yarraquin
Glen
Yard
Yard
YardYardYard
Yard
Yard
Yard
Yard
Yard
Yard
Yard
Yards YardYard
YardYard
Yard
Yard
YardsYard
Yard
Yards
YardYardYard
Yard
Yard
Yards Yard
Yard Yard Yard
Yards
Yard
Yard Yard
YardYard
Yards
YardYard
Yards
YardYardYards
YardYard
Yard YardYard
Yard
Yard
YardYards
Yard
Yard
YardYard
Nallan
Ryansville
Big Bell
Day Dawn
Cuddingwarra
Milly Soak
Karbar Pool
Fleece Pool
Berring Pool
Wallace Pool
Tragedy Pool
Muddigan Pool
Wattagee PoolCoodardy Pool
Bocadeera Pool
Extension Pool
Dardonabubba Pool
Cuddingwarra Pool
Telegootherra Spring (PD)
Callie Spring
Jungar Pool
Berring
Nallan Creek
95 Mile Creek
Casu
arina
Jungar Creek
Creek
Creek
Jungar
Creek
Lake Austin
BERINGARRA CUE ROAD
KALLI ROAD
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WATTAGEE HILL
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CARDAWEEDA HILL
8 MILE HILL
CUDDINGWARRA HILL
TELEGOOTHERRA HILL
BEEBYNBEENBYNGANNA HILL
Bald Rock
Afghan Rock
Granite Rock
Milliwarry Rock
Bubbowroo Rock
Mekatanna Rock
Coombeloona Rock
KARBAR RANGE
420
480
460
520
500
480
460
500
420
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520
480
400
500
520
440
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420
440
480
540
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landing ground
pipelin
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MC 16
CUE 7
G 20 13
K 28
G 20 9
G 20 10
G 20 1
G 20 5
G 21 3
Cue 163
178194178195
178197
178199
183975
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ñBRtg-gm
ñPOm-mbb
ñPOm-mbby
ñAN-gmap
ñSDY-ap
ñAN-xmgn-mgm
ñPOm-mbm
ñPOm-bk
ñPOm-mbms
ñPOw-ssq
ñPOm-mba
ñPOg-mfs
ñPOm-mbms
ñPOc-mi
ñSDY-og
ñPOm-mb
ñPOg-fdt
ñGLw-mfs
A§
A§
Lc
R´f
L²
A§
Rk
Wf
R´f
A§
R´f
Lc
R´f
C
R´f
Lc
A¤
A¤
A¤
A¤
A¤
C
A¤
A¤
R´gp¨
A¤
A¤
A¤
L¥1
A§
A¤
A¤
A§
C
A¤
A¤
C
R´f
A¤
C
R´gp¨
C
R´f
A¤
C
R´f
A¢
Rk
A§
R´f
A§
R´f
Rkp¨
C
R´f
A¤
A¤
C
Rkp¨
L¥1
A§
C
E¦q
Wf
A¤
Ak
Wf
A¤
A§
A¤
A¤
A§
Ak
A¤
R´f
R´fp¨
A§
Rk
C
R´f
R´f
A§
C
Lk
C
R´f
A§
R´f
A§
C
A¤
R´f
Wf
C
A¤
R´f
C
Wf
R´f
W§f
A§
R´gp¨
L²
R´f
L¥1
A¤
R´f
A§
Ak
W§f
Wf
A§
C
A¤
A¤
R´f
Lc
A¤
R´f
R´f
Rk
R´f
Lc
Ak
A¢
A¤
R´f
R´f
R´f
Wf
R´f
R´f
Rkp¨
C
R´f
L¥1
Rµg
A¹
R´gp¨
Wf
R´f
A¤
R´f
R´f
Wf
R´f
Lc
R´fR´f
A¹
L¥1
R´f
R´f
R´f
R´f
ñGLw-bk
ñBRga-gm
ñPOw-st
ñPOm-mbm
ñBRga-gm
ñSDY-og
ñPOm-mban
ñmusYMU
ñGLw-mfs
ñPOm-mbas
ñPOm-mbas
ñPOw-sf
ñPOm-mbas
ñPOm-mbb
ñPOm-mhs
ñSDY-axñPOm-mbby
ñPOm-mhs
ñmapsYMU
ñJU-mgms
ñPOg-fdt
ñPOw-mhs
ñPOm-mba
ñSDY-og
ñSDY-od
ñGLw-bs
ñANC-mgta
ñPOw-sf
ñSDY-og
ñSDY-ax
ñBRtg-gm
ñPOw-fr
ñPOw-sf
ñGLw-mus
ñSDY-og
ñmapsYMU
ñJU-mgms
ñGLr-sf
ñPOm-bko
ñAN-mgms
ñPOc-mtq
ñBRtg-gm
ñPOw-mhs
ñAN-mgmu
ñBRtg-gm
ñNOm-mbbs
ñPOm-bk
ñANct-gtl
ñPOm-bko
ñBRga-gm
ñPOc-mi
ñPOm-bbo
ñPOw-mhs
ñGLr-ssq ñJU-mgms
ñPOc-mi
ñGLr-ssq
ñPOg-frmb
ñPOw-mhs
ñJU-mgms
ñBRga-gm
ñJU-mgmm
ñTU-mgm
ñPOm-mbms
ñPOm-mbas
zq
ñPOm-mbb
ñPOc-xmtq-mi
ñPOm-bb
ñPOm-mbas
ñPOm-mbas
ñSDcr-xmgm-gmp
ñJU-mgms
ñGLw-mlv
ñPOm-mbas
ñPOm-bk
ñSDY-ax
ñPOm-bbñPOm-bb
ñPOw-sl
ñSDY-od
ñSDY-ad
ñPOg-mlv
ñPOg-mlv
ñPOw-sf
ñPOw-sf
ñSDB-mgms
ñBRtg-gm
ñPOw-mhs
ñPOc-mtq
ñGLr-mhs
ñPOm-mba
ñPOc-mtq
ñGLw-bko
ñAN-xmgm-mfs
ñmusYMU
ñJUcl-mgms
ñmusYMU
ñPOm-mbms
ñJU-xmgn-mws
ñAN-gmap
ñmapsYMUñBRtg-gmdv
ñPOc-xmtq-maps
ñPOm-mban
ñPOw-cib
ñANC-mgtn
ñJU-mgms
ñGLr-scc
zq
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
C§f
ñTU-mgg
ñTU-mgg
C§qC§q
C§g
C§g
ñAN-xmggs-gmd
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g
ñPOg-mfds
C§g
C§g
C§g
C§g
C§g
C§g
C§g
C§g C§g
C§g
C§g
ñANC-mg
C§g
C§g
C§qC§gñANC-mg
ñAN-mggs
ñANC-mg
C§g
C§g
ñAN-mggs
ñAN-xmggs-gmd
ñANC-mg
ñSDcr-mgg
ñSDcr-mgg
ñAN-mggs
ñANC-mg
ñSDcr-mggn
ñSDcr-mggn
ñANC-mgga
C§q
ñAN-mggs
R´zz
ñGLw-bs
ñPOm-mbmsñPOm-mba
Wf
ñBRG-gyh
ñPOm-xmba-mgp
ñPOw-sf
ñPOg-fa
ñPOg-mlv
ñPOm-bbo
ìod
ñSDY-ogl
ñPOg-frmb
ñSDY-og
ñPOm-mbbs
ñJU-mgms
C§q
C§q
C§q
C§q
C§q
C§q
ñAN-xmggs-gmd
ñAN-mggs
ñAN-mggs
ñANC-mg
ñAN-mggs
ñAN-xmg-mba
ñTU-mgml
ìod
zq ñGLr-ssq
ñPOw-cib
ñPOm-mba
zq
zq
ñWGtg-gm
zq
CUE
A
B
C
550
550000mE
52
52
54
54
56
56
58
58
560
560
62
62
64
64
66
66
68
68
570
570
72
72
74
74
76
76
78
78
580
580
82
82
84
84
86
86
88
88
590
590
92
92
94
94
96
96
98
98
58
69606960
6262
6464
6666
6868
69706970
7272
7474
7676
7878
69806980
8282
8484
8686
8888
69906990
9292
9494
9696
9898
70007000
0202
0404
0606
0808
70107010
1212
Orthomagmatic mafic and ultramafic
Porphyry, pegmatite, greisin, and skarn
MINERALIZATION STYLE
MINERAL SITES
Vein and hydrothermal
Stratabound volcanic and sedimentary
Regolith hosted
Undivided
Stratabound sedimentary and/or sedimentary banded iron-formation
COMMODITY GROUP
COMMODITY
All precious metal sites are gold unless otherwise indicated
SITE STATUS
Mineralization sites on this map have been extracted from MINEDEX database of GSWA. For clarity, names have been shown only for selected sites. Full details of sitenumbers, site locations, site status, mineralization, and commodities can be obtainedfrom the MINEDEX database, accessed at
Mine, deposit, prospect, or occurence............... Coodardy
CuCopper.......................................................AuGold...........................................................
BeBeryllium....................................................
FeIron............................................................KlnKaolinite; Kaolin.........................................LstLimestone..................................................MoMolybdenum..............................................PGEPlatinum Group Elements..........................AgSilver..........................................................SnTin..............................................................WTungsten....................................................UUranium.....................................................ZnZinc............................................................
Beryl, emerald........................................... Brle
Theme Data Source Data Currency Organization
Geology*
DATA DIRECTORY
GSWA 2010 Dept of Mines and Petroleum
Dept of Mines and Petroleum
Dept of Mines and Petroleum
JUNE 2010
MAY 2010
JUNE 2010
2010
2010
2000
Landgate
Landgate
Landgate
Consultative Group for International AgricultureResearch Consortium for Spatial Information
WAROX
MINEDEX
GESMAR
GEONOMA
Landgate and GSWA field survey
NASA SRTM 90m Digital Elevation Data
Structural data
Mineral sites*
Horizontal control
Topographic nomenclature
Topography
Contours
* DMP data can be viewed online at , and related datasets can be downloaded from the GSWA Data andSoftware Centre
Cartography by I Lesiak and P BackhouseEdited by S White
Geochronology by: (1) Pidgeon, RT and Hallberg, JA 2000, Australian Journal of Earth Sciences, v. 47, p. 153–165. (2) Mueller, AG et al. 1996, Economic Geology, v. 91, p. 896–915. (3) Wang, Q 1998, Australian National University, Canberra, PhD thesis (unpublished),186p.
Geology by MJ Van Kranendonk 2006–2009, TJ Ivanic 2006.Compiled by MJ Van Kranendonk, 2010
Geochronology from GSWA data (published and in preparation) and interpreted from external sources (listed below).Some GSWA geochronology may come from samples obtained on adjoining map sheets. GSWA geochronologydata are available online at and on DVD (Compilation of geochronology data– updated as required), or can be downloaded from
Speciality metal
Precious metal
Precious mineral
Base metal
Iron
Energy
Industrial mineral
Construction material
Tailings......................................................................................................................Mineral field district boundary...................................................................................