AUSTIN
GEOLOGICAL SURVEY OF WESTERN AUSTRALIA
Gidgee Tank
DAWN
A¥
MURCHISON
Aª
ñapuYMU ñNOy-muy
Wq
$e ñgvlqYMU
C§f
6
C 46 0
R´f
ñPOm-bk
Wq
ñPOm-mhs
48 0
0
A¥
Rμg
R´f
44
ñTU-gmfe
C§f
$e
Kiah Well Yard
$e Rμg
ñPOm-bk
27°50'
$e ñTU-xgmfp-gmal
C§f
R´f
500
18
$e
Yard Smith Well
Wg
ñSDB-gme
R´f
Mundra Well
$e
C§l
Rμg
A LG DA
C§f
C§f
C§f
46 0
R´f
ñTU-gmfp
ìod
ìod
Rμg R´f
C§l
Mungilgy Bore
ñTU-gmfp
$e
ñTU-gmal
ñTU-gmal
C§f
A¥
50
0
06
ñTU-gmfp
46 0
MINERAL FIELD
Bore
ñTU-gmfp
6904000m N
440
ñTU-gmfp
ER
WE LL
A¥
ñTU-gmfe RO AD
Rμg
54
80
C§f 56
58
560
ñgvlqYMU
62
64
66
570
68
ñTU-gmfe
Peedmont Bore
74
76
Eastern Jaspilite Yuletide 70
$e
C§m
ñNOy-mib
68
ñNOy-xcxj-mus Rμf ñNOy-muq C§l
Wq
Mount Magnet 25 km
117°30'
ñPOm-bb
$e
72
R´f
78
ñSDB-mgms Au,Ag
Wheel of Fortune Au,Ag
A¥
Wf
AT
ñNOm-mb
Yard
A¥
82
84
34
86
R´f Murdye Spring
D
L¯
ñPOm-mbas
ñPOm-mbm 14
A¥
L¥
Yard
$e
ñPOm-mbm ñgmapYMU ñPOm-mbas
$e
30
26
2800 – 2760 Ma
L¯
ñTUcu-mgmy
zq
ñPOm-mhs
12
Rμk
zq ñTUcu-mgmu
Zadow Bore 6910
ñPOm-mbas 2815 – 2805 Ma
ñNOy-xf-cib
08 Wandagabbie Bore
Wq Nellie Bore 06
ñPOm-mhs ñPOm-mibs ñPOm-mbas ñPOm-mbba ñPOm-mbm ñPOm-mbms ñPOm-bb ñPOm-bk ñPOm-mukt
ñNOy-xf-cib
A¥
ñNOy-mhs ñNOy-mcbs ñNOy-mib ñNOy-xcxj-mus ñNOy-mbbs ñNOy-muq ñNOy-muy ñNOm-mb
A¥ 04
ñNOy-muy ñNOm-mibs zq ñodYMU
Teranty Bore
R´f 88
ñBRga-gm ñBRtg-gm ñBRtg-gma ñBRtg-gmp
AgmapYMU
590
92
94
ñBRtg-gm
Igneous differentation................................................................................... Metamorphic foliation, showing strike and dip
20
vertical..........................................................................................................
Cleavage, showing strike and dip
ñTU-mg ñTU-mg ñTU-gn ñTUcu-mg ñTUcu-gm
ñTU-gn
ñTUgmfe
ñTU-gmfp
vertical.......................................................................................................... Shear-sense indicator dextral........................................................................................................... sinistral......................................................................................................... showing dip of foliation sinistral inclined...............................................................................................
ñTUcu-mgmy
ñTUcu-gmal
ñTUcu-gmfe
ñTUcu-mg
Mineral lineation, showing trend and plunge
96
75
inclined......................................................................................................... Stretching lineation, showing trend and plunge
8
inclined......................................................................................................... horizontal......................................................................................................
ñmfasYMU
Axis of crenulation, showing trend and plunge inclined.........................................................................................................
12
Cleavage–cleavage intersection lineation, showing trend and plunge
ñoYMU
inclined.........................................................................................................
ñuYMU
55
Mineral alignment, showing trend and plunge
Amphibolite Mafic intrusive rock, undivided Ultramafic volcanic rock, undivided
inclined.........................................................................................................
28
Igneous lineation, showing trend and plunge horizontal.....................................................................................................
ñSDB-mg ñSDB-mg ñSDB-gn ñSDcr-mgg
ñSDB-gn
ñSDcr-mgg
Metagranite; locally foliated Granitic rock, undivided Crossroads Granodiorite
ñSDY-xony-any
Layered mafic–ultramafic intrusive rocks
Aeromagnetic lineament unspecified.................................................................................................. Highway with national route marker................................................................... Road, unsealed................................................................................................. Track................................................................................................................ Fence...............................................................................................................
ñPOg-f
ñTUcu-gmfp
ñmfasYMU Quartz–mica schist; commonly as discontinuous septa within granites Meta-andesite; massive to fragmental; commonly strongly deformed
ñogYMU
5
inclined.........................................................................................................
ñTUcu-gm
Quartz–mica schist Meta-andesite
ñPO-xmb-mf
CUNDIMURRA MONZOGRANITE: K-feldspar megacrystic biotite metamonzogranite; strongly foliated Meta biotite monzogranite; mylonitic; commonly with pegmatite veins and other intrusive granitic phases Fine-grained leucocratic monzogranite; undeformed; common magmatic foliation Equigranular monzogranite to syenogranite; undeformed; common magmatic foliation K-feldspar porphyritic monzogranite to syenogranite; undeformed; common magmatic foliation
ñodYMU
80
Lineation, unspecified, showing trend and plunge
ñTU-gmfs
K-feldspar megacrystic, flow-banded monzogranite intruded by undeformed fine-grained granite with common magmatic foliation K-feldspar megacrystic biotite metamonzogranite; strongly foliated Fine-grained granite; undeformed; common magmatic foliation Monzogranite to syenogranite; undeformed; common magmatic foliation K-feldspar porphyritic monzogranite to syenogranite; undeformed; common magmatic foliation Monzogranite to syenogranite; undeformed; common magmatic foliation
80
inclined.........................................................................................................
ñBRtg-gmp
Metamonzogranite to metagranodiorite; commonly foliated Granite, undivided; metamorphosed; includes deeply weathered rock Cundimurra Monzogranite: metamonzogranite to metasyenogranite; locally undeformed Monzogranitic rock, undivided
ñmwasYMU ñoYMU ñuYMU
ñgvlqYMU
ñBRtg-gma
Granitic rock, undivided Quartz–plagioclase granophyre
ñmwasYMU
ñTU-gmal
80
vertical..........................................................................................................
ñgvlqYMU
ñmsqmYMU ñmfasYMU
Granitic rock, undivided; metamorphosed (section only) Fine-grained porphyritic monzogranite, as dykes; weakly metamorphosed; locally foliated Quartz–plagioclase granophyre; locally strongly foliated
ñTU-mgmu
80
inclined.........................................................................................................
Garden Rock Monzogranite Telegootherra Monzogranite Fine-grained monzogranite to syenogranite K-feldspar porphyritic monzogranite to syenogranite
ñmsqmYMU
ñogdYMU
Strongly foliated amphibolite and amphibolite schist; commonly also lineated Dolerite; medium grained; massive, locally weakly deformed; metamorphosed Gabbro; coarse grained; massive, locally weakly deformed; locally contains dolerite, quartz gabbro, and gabbronorite; metamorphosed Pegmatoidal gabbro; coarse grained, massive; commonly strongly deformed; locally contains dolerite and quartz gabbro; metamorphosed
Metabasalt and felsic metavolcanic rocks
Greensleeves Formation: andesitic to rhyolitic volcanic and volcaniclastic rocks
ñPOm-mhs
ñPOm-mib
ñapuYMU Ultramafic schist Peridotite; coarse grained; massive, locally weakly deformed; metamorphosed
ñPOm-mb
ñPOm-b
ñPOm-mu
ñAN-mg
Metagranite
Abandoned railway........................................................................................... Townsite
ñNOy-xf-cib
ñNOy-mhs
ñNOy-mib
ñANC-mg
Metatonalite, metagranodiorite, and metatrondhjemite
Locality..............................................................................................................
Merroe
Yard..................................................................................................................
Yard
Horizontal control; major, minor......................................................................... Breakaway........................................................................................................ 420
Contour line, 20 metre interval........................................................................... Watercourse......................................................................................................
ñNOy-xcxj-mus
ñNOy-mb
ñNOy-mu
Yaloginda Formation ñNOy-xf-cib Psammitic and pelitic schist ñNOy-mhs ñNOy-mib Meta banded iron-formation ñNOy-xcxj-mus Mixed jaspilitic chert and iron formation, interlayered with ultramafic schist ñNOy-mb Metabasalt and metakomatiitic basalt ñNOy-mu Meta-ultramafic rock, undivided
ñNOm-mib
Austin Wattle Creek
less than 1000............................................................................................... Homestead........................................................................................................
Meekatharra Formation Schistose pelite and psammite Meta banded iron-formation Metamafic rock Mafic volcanic rock, undivided Meta-ultramafic rock, undivided
ñPOm-mhs ñPOm-mib ñPOm-mb ñPOm-b ñPOm-mu
ñNOm-mb ñNOm-mib ñNOm-mu
16
80 60
GARDEN ROCK MONZOGRANITE: monzogranite to syenogranite; undeformed K-feldspar porphyritic monzogranite; undeformed; common magmatic foliation TELEGOOTHERRA MONZOGRANITE: monzogranite to syenogranite; undeformed; common magmatic foliation Fine-grained monzogranite to syenogranite; undeformed; common magmatic foliation K-feldspar porphyritic monzogranite to syenogranite; undeformed; common magmatic foliation
18
Pool...................................................................................................................
Pool
Rockhole............................................................................................................
Rockhole Soak
Spring................................................................................................................ Bore, well..........................................................................................................
Spring
Bore
Well
Windpump......................................................................................................... Dam, tank..........................................................................................................
ñNOm-mu
Mineral field boundary....................................................................................... Mineral field district boundary............................................................................
Murrouli Basalt Meta banded iron-formation Meta-ultramafic rock, undivided
Tailings or stockpile...........................................................................................
For further details refer to main reference
c. 2820 Ma
ñNOm-mb ñNOm-mibs ñNOm-mbbs ñNOm-must
ñPOm-mibs ñPOm-mbms
ñPOm-mbas
ñPOm-mbba
ñPOm-bb
ñPOm-bk
ñSDB-mgms ñSDB-gme ñSDB-gmel
ñSDB-gme
ñSDB-gmel
ñSDcr-mggn
SHEET INDEX
Metamonzogranite; locally quartz porphyritic; strongly foliated Monzogranite to syenogranite; undeformed, locally with magmatic foliation Monzogranite to syenogranite; leucocratic; undeformed; locally with magmatic foliation CROSSROADS GRANODIORITE Biotite metagranodiorite; strongly foliated; commonly with pegmatite veins and other intrusive granitic phases
ñSDcr-mggn
BILLABALONG
ñANC-mgtn
Gabbro; massive to weakly foliated; local dolerite, quartz gabbro, and gabbronorite; weakly metamorphosed
Tonalitic gneiss; medium grained; strongly foliated
Vein and hydrothermal
Precious metal
Stratabound volcanic and sedimentary
Base metal
Regolith hosted
Industrial mineral
Undivided
Construction material
ñNOy-mib
ñNOy-mbbs
ñNOy-muq
ñNOy-muy
Copper.......................................................Cu Gold...........................................................Au
ñNOm-mbbs
2343
TARDIE
CUE
REEDY
2443
2543
CUE SG 50-15 MELANGATA DALGARANGA
AUSTIN
WYNYANGOO
2242
2342
2442
2542
TALLERING
WURARGA
YALGOO
EDAH
MOUNT MAGNET
CHALLA
2041
2141
2241
2341
2441
2541
YALGOO SH 50-2
KIRKALOCKA SH 50-3
MULLEWA
MELLENBYE
BADJA
2040
2140
2240
THUNDELARRA KIRKALOCKA COOLAMANINU 2340
2440
2540
1 : 100 000 maps shown in black 1 : 250 000 maps shown in brown Search for GSWA map products online at
GRID CONVERGENCE 0.3°
Gypsum......................................................Gp Limestone...................................................Lst Silver..........................................................Ag
SITE NAME
ñNOy-xcxj-mus
Austin
True north, grid north, and magnetic north are shown diagrammatically for the centre of the map. Magnetic north is correct for 2011 and moves westerly by approx. 40" annually
Mineralization sites on this map have been extracted from GSWA's MINEDEX database. For clarity, names have been shown only for selected sites. Full details of site numbers, site locations, site status, mineralization, and commodities can be obtained from the MINEDEX database, accessed at .
YALOGINDA FORMATION: felsic volcaniclastic rocks and banded iron-formation; local quartzite; widely intruded by layered gabbroic to peridotitic sills; metamorphosed Psammitic and pelitic schist interlayered on a metre to decametre scale; locally strongly sheared Strongly foliated metachert, locally ferruginous Meta banded iron-formation; typically with coarse, granular, and recrystallized magnetite crystals; foliated Mixed jaspilitic chert and iron formation, interlayered with ultramafic schist Strongly foliated metabasalt and local amphibolite Silicified meta-ultramafic rock Mylonitized meta-ultramafic rock
ñNOm-mibs
NOONDIE
2243
2142
MN
COMMODITY
Mine, deposit, prospect, or occurrence....... Lake
ñNOy-mcbs
TN GN
GRID / MAGNETIC ANGLE 0.8°
MEEKATHARRA FORMATION Schistose pelite and psammite with local biotite porphyroblasts Strongly foliated meta banded iron-formation Amphibolite schist derived from basalt; fine to medium grained; commonly also lineated Amphibolite derived from basalt; massive to foliated and/or lineated Metakomatiitic basalt; massive to pillowed with local hyaloclastite; with fracture cleavage, or foliated Fine-grained ultramafic schist derived from komatiitic basalt; local talc–carbonate rock; commonly deeply weathered Basalt; massive to weakly foliated; locally pillowed and/or vesicular; metamorphosed Komatiitic basalt; locally pillowed and/or variolitic; fractured to locally foliated; weakly metamorphosed Talc–carbonate (–chlorite–serpentine) schist derived from komatiitic rocks; commonly deeply weathered and lateritized
ñNOy-mhs
MUGGAMURRA 2042
COMMODITY GROUP
All precious metal sites are gold unless otherwise indicated
ñPOm-mukt
MEKA
2143
MURGOO SG 50-14
MINERAL SITES MINERALIZATION STYLE
ñSDY-og
MURGOO
2043
N.T. Qld W.A.
S.A. N.S.W. A.C.T Vic.
ñNOm-must
Tas.
MURROULI BASALT: metabasalt and metakomatiitic basalt Strongly foliated meta banded iron-formation Strongly foliated metabasalt and local amphibolite Tremolite–chlorite–talc schist
28°0'
98
117°50'
C
118°0'
DIAGRAMMATIC SECTIONS
D
ñTU-gmfp
ñNOm-mib ñNOm-mibs ñTUcu-mgmy
ñTU-gmfe
ñTUcu-mgmu
ñogdYMU ñTU-gmfe ìod
ñSDB-gme
ñTU-mgmu
ñTU-gmfp
ñPOm-bb
GREAT NORTHERN HIGHWAY
ñNOm-mbbs ñapuYMU
ñPOm-bk
ñTU-gmfe
ñANC-mgtn
ñmusYMU ñapuYMU
ñPOm-mbas
zq
C§l
Wq
ñTUcu-gmfe ñapuYMU
$e
ñBRtg-gmp
ñgvlqYMU
Gilbert Well
Rμg
Atkinson Well
$e
ñNOy-mcbs C§f Ard ñSDB-gme Brooklyn ñSDB-gme ñSDB-gmel ñNOy-muq 66 Patrick 70 C§l Wq $e C§f Wq R´f C§f zq 80 R´f Rμg
ñNOy-muy
ñTU-gmfs
ñogYMU
ñBRtg-gma
$e
WINJANGOO HILL ñapuYMU ñapuYMU
$e
ñmsqmYMU
$e
ñSDB-gme
40
580
CUE 8
ñgvlqYMU
Rμf
ñTUcu-mgmy
ñmwasYMU
$e
Wq
Lennonville
zq
ñTUcu-gmfp
Rμf
ñBRga-gm
ñgYMU ñgvlqYMU
ñSDB-mgms
ñapuYMU ñPOm-mbas
ñogYMU
ñogYMU ñPOm-mbm
70
MERROE–WANDARRIE ROAD
2 km
50
ìod
Yard
ñmusYMU
Carey Well
Yard Lennonville Bore
Way-up indicator
Quartz vein or pod
ñgYMU
Lake Bore
C§l
50
ñNOy-mib
Well
80
vertical.......................................................................................................... trend of igneous layering..............................................................................
Crenulation cleavage, showing strike and dip
Quartz vein or pod; massive, crystalline, or brecciated; age uncertain
ñBRtg-gm
80
inclined.........................................................................................................
Mount Magnet 11 km
B
SEA LEVEL
Buccaneer
$e
65
117°40'
A
68
Rμg
Deep Well
zq
ñPOm-mbm
zq 467m ñPOm-mibs
R´f
80
60
80
ñmusYMU ñPOm-bb
80
A¥ Wattle Creek Yard
Wg
R´f
ñTU-gmfe
Jobetah Well
55
Igneous layering, showing strike and dip
6920
L²
ñogYMU
$e
ñTUcu-gmfe
45
Creek
52
50
$e
Allen Bore
Bore
ñTU-gmfp
C§l
ñTUcu-gmfp
C§g
C§l
C§m
zq 85 ñapuYMU
R´f
Wq
80
R´f
R´f
46 0
Golden Treasure
66
C§l
New Jobetah Bore
$e
RN HE
C§f
46 0
550 000mE
C§l R´f
$e
$e Wq
Rμg
Wg
R´f
A¥
R´f
ñPOm-mbm
$e
ia ima Bar
C§l
28°0'
PA LM
zq
ñNOy-xcxj-mus 6 ñNOy-muy zq 72 ñNOm-must 75 Fairplay Well ñTUcu-mgmy ñNOy-muq Wq zq 78 80 ñapuYMU Welcome zq 58-1 ñNOy-mib ñNOy-mib 65 G ñPOm-bb Contura Wq 491m C§l zq R´f North 70 ñTU-gmfe ñPOm-bb Rμf ñgmapYMU C§m 50 0 APOm-mukt $e ñgvlqYMU ñPOm-mhs ñapuYMU zq ñapuYMU ñNOm-mibs Government Well
ñTU-gmfe
48 0
R´f
48 0
C§f
Wg
65
ñNOm-must
C§l
27°50'
zq 66 ñgvlqYMU ñgvlqYMU ñTUcu-mgmy ñogYMU 58
80
70 22
ñmwasYMU ñodYMU ñogYMU ñogdYMU
L¯
62
ñTUcu-gmfe
Dorothy Well
32
65
ñmwasYMU
ñogYMU
C§f
R´f
Coutts Well
ñTU-gmfs
Wg
0
A¥
$e
ñPOm-mbas
ñgvlqYMU
$e
Yard
Rμg 46
ñTU-gmfs
ñTU-gmfs
zq
60
ñmwasYMU
C§f
R´f Wg
Rμf
ìod
Palmer Well
YALGOO
A¥
ñANC-mgtn
A¥
ñTUcu-mgmu
Wq
Haeremai
ñuYMU
Dolerite dyke, sill, or plug
ñNOm-mb
Dixie Well
ñTUcu-gmfe
ñNOm-mbbs ñNOy-xf-cib ìod
ñapuYMU
zq
ñogYMU
$e
75
West Lennonville
R´f
500
08
C§f
80
C§f
C§l
Bore
60
WeedahYalan
Little Wynyangoo Well
Yard
RT NO
vertical..........................................................................................................
inclined.........................................................................................................
Rμk
Dolerite dyke, sill, or plug; fine- to medium-grained dolerite and gabbro
ñBRga-gmp
65
inclined.........................................................................................................
ñoYMU ìod
trend of gneissic layering.............................................................................
ìod
L¯
ROAD
Yard
18
ñmsqmYMU ñmfasYMU
22
ñNOm-mb ñogYMU 80 ñgmapYMU 80 60 ñmwasYMU 20 ñapuYMU
Wq
ñgvlqYMU
R´f ìod
ñTUcu-mgmy ñTUcu-gmfe
C§l zq
Success Well
ñmsqmYMU
L²
ñNOy-mib
Old Wynyangoo Homestead Well
ñNOy-muy ñNOy-mib
26
ñgmapYMU
Una Rockhole
ñPOm-bb
ñPOm-bb
85
ñPOm-mbm
zq
ñTUcu-mgmu
ñTUcu-mgmu ñTUcu-mgmy ñTUcu-gmal ñTUcu-gmfe ñTUcu-gmfp
c. 2680 Ma 2 3
L¯
Wq
T EA GR
Rμf
Rμg
zq ñNOy-mhs
AUSTIN
L¯
R´f
ñgmapYMU
R´f
Wq
ñTU-xgmfp-gmal ñTU-mgmu ñTU-gmal ñTU-gmfe ñTU-gmfp ñTU-gmfs
L¥ 28
ñgmapYMU
C§m 52
C§g
ñTUcu-mgmy
D
52 0
Yard
R´f
C§f
ñSDB-gme
80
ñTU-gmfs
C§f
R´f A RO
$e
ñTU-gmfp Bore
ET GN
6910
Rμg
ñPOm-bb
R´f
R´f C§f
MA
C§f $e
ñPOm-mhs
ñogYMU
50 0
A¥
T UN
ñTU-gmfp
R´f
ñSDB-gme
ìod
MO
R´f
–
Rμg
GA
C§f
C§f
ñNOm-mb ñNOm-mbbs ñogYMU ñNOy-mib ñPOm-mbas
ñTU-gmfs C§f
N RA
12
R´f
C§f
54
55
LAKE
ñapuYMU
House Well Merroe Well Yard Yard
70
6930
ñNOy-mib ñapuYMU
Au,Ag zq
ñTUcu-mgmu
ñapuYMU ñNOm-mibs ñNOm-mbbs
70
75
ñTU-gmal
ñTU-gmfs
Wq
zq ñNOy-muy ñapuYMU
c. 2676 Ma
24
Wanarie
Cu ñogdYMU
68
80
1/2 Mile Well
14
$e
ñapuYMU
Wandarrie
Caves Well
Rμg
48 0
R´f C§f
R´f
12
ñTU-xgmfp-gmal
32
L¯
Rμg
65 66
Bedding, showing strike and dip
ñNOm-mb ñNOm-mu ñSDB-gn ñNOm-mib ñoYMU ñuYMU
SCALE 1:500 000 10 15
Deformation Event 1 (D 1: 2676 – 2665 Ma)
$e
Old Granites
ñgvlqYMU
ñSDB-gme
500
16
Mount Farmer
ñTUcu-mgmu
80
ñapuYMU
C§f
45
70
ñogYMU
65
Glennie Well
80
ñBRga-gm ñBRga-gmp ñBRtg-gm ñBRtg-gma ñBRtg-gmp
ñgYMU ñgmapYMU ñgvlqYMU
ñPOm-mbm
L²
ñNOy-mib ñNOy-mbbs ñPOm-mbm
70
80
4
8
Sinbad Well
zq
32
C§f
Stephens Well
80
0
ñTUcu-mgmy 80
C§l
ñNOy-mib
zq
ñSDB-gme
A¥
Rμg
A¥
$e
R´f
$e
$e
White Well
C§m ñapuYMU
ñTU-gmfs
ñTU-gmfp
44
Stone Tank Well
ñogYMU
C§l R´f
zq
ñSDB-gme
Rμg
Wg
48 0
C§l
Spring
R´f
Wq
48
ñNOy-muy ñgmapYMU
zq
ñmwasYMU
Robertson Well
$e
C§f
C§l
ñTU-gmfs
6920
ñPOm-bb
ñgvlqYMU
34
0 42
ñgmapYMU
0
0 44
Dalgaranga Homestead 59 km
ñTU-gmfp
ñTU-gmfe
Rμg
Rμg
48 0
22
461m
5
ñNOm-must ñTUcu-gmfe
45
32
70
44
zq
ñBRga-gm
ñgYMU
Yard
75
ñNOy-muy ñNOy-mib
R´f
$e
ñTU-gmfp
Well
Moonlight
$e
Cundimurra Well
Bundoo Bore
48 0
R´f
80
4
ñTUcu-gmal
85 4
Au,Ag ñgmapYMU
46
24
MOYAGEE HILL
MC 17
80
ñNOy-mbbs
Try Again
ñNOy-muy
ñapuYMU ñgvlqYMU
Rμf
unspecified................................................................................................... Z-vergence...................................................................................................
Gneissic layering
Deformation Event 2 (D 2: 2665 – 2640 Ma)
ñgvlqYMU
ñTUcu-mgmu
Munbee Rockhole
ñNOy-mbbs
C§l Blackmans Lucky Spot Find
R´f ñPOm-bb
ñSDB-gme
ñTUcu-mgmy
ñTUcu-mgmu
85
ñapuYMU
ANOy-mhs
ñogYMU
Rμg
Pollick Well
Wq
ñPOm-bb
$e
Rμg
ñNOy-mib Moyagee Soak ñogYMU Gnamma Bore zq ñgvlqYMU ñNOy-mbbs White Well ñNOy-mib ñogYMU ìod ñNOm-mbbs R´f ñNOm-must 6 ñNOy-mbbs ñNOy-muy Eily Eily Rockhole 4 80 zq
ñogYMU
70
36
L¯ ñogYMU ñgvlqYMU ñgvlqYMU ñapuYMU ñPOm-mbm ñNOy-mbbs
ñTUcu-mgmu
ìod
AY
R´f
C§g
2
Wq
DISTRICT
80
40
HW
48 0
C§m
A¥
60
Rμg
85
60
RI E
ñTU-gmfs B
$e
$e
– W AND AR
Melarburgah Well
$e
R´f
zq ñogYMU
ñgvlqYMU ñogYMU ìod ñapuYMU ñPOm-mbm ñgvlqYMU 86 ñNOy-mbbs 45 zq 57
Black Tank Well
E MERRO
$e
Wg $e
C§l
ñodYMU
ñgvlqYMU
MAGNET
18
C§f
Sparrow Well 44 0
M OUNT
C§f
ñTU-gmfp
Yard
ìod
$e
ñTU-mgmu
C§f
R´f
R´f
Boodajerrie Bore
ñNOy-xf-cib
C§l
80
46 0
500
R´f
80
ñTUcu-mgmu
Yard 440
c. 2623 Ma
80
42 0
Yard Well
Williamson Well
28
Curries Well
Wg
Wg
Rμg
ìod
$e
Wq
FIELD C§m
$e
R´f
MINERAL
ìod
Jean Well
Moyagee Well Neds Well Yard
Wq
A¥
420
C§f ìod
A¥
ñTU-mgmu
A¥
$e
Wq
52 0
Well
C§l
ñTUcu-mgmy
4 4 ñapuYMU ñNOy-xf-cib Moyagee 87 ñogYMU
ñapuYMU
80
c. 2617 Ma 1
C§m
70
ñogYMU ñNOy-muy
46 0
440
10 Mile Well
Numbers
Rμg
$e
85
$e
38
L¯
70
Lady Zena
C§l
ñapuYMU
0
480
46 0
Edarno Well
32
6930
ñgvlqYMU
8
ñNOy-mbbs
ñNOy-muy
C§m
ñNOy-mib
ñTU-gmfs
ñNOy-mib
Wq
ñNOy-mib
85
Lady of the Lake
ñgvlqYMU ñPOm-bk
DISTRICT
Rμg
ñogYMU
44 0
DAY
Boonamia Well
26
C§l
462m
Au,Ag
zq
L²
ñNOy-muy
$e
G 58-4
Moyagee
Louise Well
zq
62
ìod
27°40'
50
ñNOy-mbbs
Well
Murralee Bore 70
Yard
ñPOm-bb
$e
R´f
85
80
$e
C§f
ñogYMU
Gidgie Well
ñmsqmYMU
Well
34
$e
Yard
Well
ñNOy-muy
Lena
50
6940
L¥e¨
ñNOy-mib
440
ñSDcr-mggn ñgmapYMU
Wg
28
C§m
zq
ñPOm-mib
YILGARN CRATON
Two Wells Bore
ñNOy-mib
zq
ñNOy-muy ñNOy-mcbs ñapuYMU zq ñNOy-mib25 12
ñNOy-mib
80
$e
North Outcamp Well
36
ñogYMU
440
Yard
ñANC-mgtn
Yard
L¯
ñgvlqYMU ñoYMU
Small-scale fold axis, showing trend and plunge
Youanmi Terrane
Rμk
L¥
Golconda Well
42 0
ñmwasYMU
ñmwasYMU
$e
ñNOy-mib
65
L¯
vertical..........................................................................................................
ìod ñoYMU ñPOm-mb
zq
70
inclined.........................................................................................................
Murchison Domain
Two Wells Well
A¥
L²
Brunswick Hill
80
Rμk
ñPOm-bb
0 48
zq
ñNOy-muy
ñodYMU
Moyagee North
ñPOm-mu ñuYMU ñNOy-xcxj-mus
Small-scale fold axial surface, showing strike and dip
Kilometres
Residual or relict units R´f Ferruginous duricrust, massive to rubbly; includes iron-cemented reworked products Residual sand and minor gravel derived from ferruginous duricrust Rμf Rμg Quartzofeldspathic sand, commonly over granite Residual sand and calcrete; nodular and pisolitic Rμk
42
ñodYMU
R´f
Lst
$e 38
L¥
L¯
Rμg
A
R´f
L¯
ñogYMU
L¥ 420
27°40'
ñTU-gmfe
ñTU-gmfp
R´f
ñNOy-mib
Green Well
ìod
ñNOy-mib ñNOy-xcxj-mus ñNOy-mu
5
Fold, exposed................................................................................................... Fold, concealed.................................................................................................
ñoYMU ñNOm-mb ñuYMU ñTUcu-gm ñNOm-mb ñNOy-xf-cib
Big Bell Suite
80
ìod
antiform; exposed, interpreted...................................................................... synform; exposed, interpreted......................................................................
44
ñodYMU
Eureka South
A¥
R´f
48 0
C§f
6940
Corktree Bore
ñTU-gmfs
ñNOy-mib ñANC-mg
strike-slip, interpreted, showing relative sinistral horizontal displacement ...... Fold, showing axial trace and generalized plunge direction
ñoYMU ñuYMU ñgYMU
ñSDB-gn
ñTU-gn
Lacustrine unit, first generation L¥2 Stabilized dunes within and adjacent to playa lakes; typically vegetated
Golconda Eureka
ìod
strike-slip, interpreted, showing relative dextral horizontal displacement ........
ñoYMU ñoYMU
ñuYMU
0
The Island
78
Austin
strike-slip, exposed, showing relative sinistral horizontal displacement ..........
ñoYMU ìod ñTUcu-mg ñoYMU ñPOm-mb ñNOy-mb ìod ñuYMU
ñgvlqYMU
L²
L¯
strike-slip, exposed, showing relative dextral horizontal displacement ............
ìod
ñNOy-mhs ñoYMU zq ñoYMU ñNOy-mb
ìod
ñTU-mg
L¥2
0
ñmsqmYMU
zq ìod ñmsqmYMU
42
ñPOm-bb
ìod
ìod
exposed........................................................................................................ interpreted....................................................................................................
ñoYMU
ñPOm-mhs
Austin Downs Supersuite
70
C§m
Yard
Tharandah Well
Yard
zq
ñPOm-b ñoYMU ñgvlqYMU
ñTU-mg
46
HI G
Deep Well
L²
0
ñANC-mgtn
Yard
ñmwasYMU
Rμg
72
C§f
L¥
LA K
50 0
80
L²
ñmsqmYMU
Lacustrine unit, second generation L¥1 Dune and lake deposits; active systems within and adjacent to playa lakes; non-vegetated or poorly vegetated
ñNOy-mib
44 0
zq
AUSTIN
420
42
zq
Birthday Bore
ñTU-gmfe
ñmwasYMU
ñmsqmYMU
R´f
ìod
ñNOy-mib
ñNOy-muy
Woolshed Wells
ìod
ñTU-gn
L¥1
L¥e¨
ìod ìod
L¯
42 0
ìod
OAD
ñNOy-mib
ìod
exposed........................................................................................................ Fault or shear
ñNOy-mb
ñPOm-mb
ñSDcr-mgg
Yalgowra Suite
zq
44
R
$e
Gp
ñmwasYMU ñANC-mg
Annean Supersuite
R´f
C§f
Austin Hill
44
48 0
ìod
LAKE
$e
Kowergabbie Well
Wq
Lake Austin
48
ñNOy-mbbs
ñNOy-mib
L²
ES I DE
46
458m
L¥e¨
ñAN-mg ìod
Lacustrine Units L¥ Sand, silt, and gypsum in dunes adjacent to and within playa lakes L¥e¨ Lithified to unconsolidated gypsum and clay, in mounds and dunes adjacent to playa lakes Mixed dunes, evaporite, and alluvial deposits; typically adjacent to playa lakes L¯ Saline and gypsiferous evaporite deposits, clay, silt, and sand in playa lakes L²
ñodYMU
GR E
0 48
ñANC-mgtn
ñNOy-mib
L¥
zq
Geological boundary
ñPOm-b ìod ñSDB-mg ñBRga-gm ñBRga-gm ñmfasYMU ñSDY-xony-any ñoYMU
ñPOm-mb ñgvlqYMU ñPOg-f
Cullculli Suite
zq
6950
50
G 21-2
Mainland
L¥e¨ ñANC-mgtn
4 km
ñogYMU
Mainland
Aª
Walganna Suite
48
480
Rμg
ñSDcr-mggn
42 0
C§m
A¥
Tuckanarra Suite
Wg
L²
Yard
ñNOy-muy zq
Day Dawn View
ñBRga-gm
North Well Yard
Boundary Bore
R´f
L¥
Wq
Polelle Group
L¯ C§f
Wg
Norie Group
Yard
ñNOy-mbbs ñodYMU ñogYMU ñgvlqYMU
$e
Wf
Bald Rock Supersuite
C§g
L²
L¥
52
ñBRga-gmp
Wq
Wc
Murchison Supergroup
A¥
ñBRga-gm zq
C§m
Austin Downs Supersuite
Well
L¯
L¥e¨
Jones Bore
Wg
ñmwasYMU 6950
Tank
Yard
ñmsqmYMU
ROAD
CLES PINNA Mainland Well
Wg L²
54
ñmfasYMU
C§l Yard
Jones Well
C§l
Colluvial units Colluvium derived from different rock types; includes gravel, sand, and silt C Colluvial footslope containing ferruginous gravel and reworked ferruginous duricrust C§f Colluvial footslope containing quartzofeldspathic gravel, sand, and silt commonly derived from granite and associated weathering products C§g Colluvial footslope deposits derived from different rock types; includes gravel, sand, and silt C§l C§m Colluvial footslope containing ferromagnesian gravel, sand, and silt commonly derived from mafic/ultramafic rocks and associated weathering products Sheetwash units Wc Very low gradient sheet flood deposits, with numerous claypans; includes sand and silt Wf Clay, silt, and sand sheetwash deposits, with abundant ferruginous grit Clay, silt, and sand sheetwash deposits, commonly derived from granitic rock Wg Clay, silt, and sand sheetwash deposits with abundant quartz-vein debris Wq Alluvial units Clay, silt, sand, and gravel in fluvial channels Ae A¥ Clay, silt, and sand in braided swales on floodplains Sand, silt, and clay in alluvial drainage depressions, claypans, and ephemeral floodplain lakes; low-lying areas with internal drainage Aª
Walganna Suite
$e
$e
Wf
ñgmapYMU
zq
ñgmapYMU
HIGH W AY
ñANC-mgtn
80
NOR TH ERN
zq
Bore
zq ìod
L¥e¨
420
C§g
56
Tuckanarra Suite
zq
L¯
L²
44 0
Casua rina
46 0
52
$e
ìod ñmwasYMU
L²
Ae
Polelle Group
46 0
Arthurs Well
0
ìod
C§l
Transformer ñgmapYMU
Wf
$e
C§g
ìod 44
ñgvlqYMU ìod
C§f
ñPO-xmb-mf ìod ñBRtg-gma ñBRtg-gmp ñBRtg-gm
YILGARN CRATON
L¥
$e
Wf ñBRga-gm
L²
L¥e¨
L¥
ñBRtg-gma
C
Youanmi Terrane
C§l
27°30'
Norie Group
ìod
C§f
INTERPRETED BEDROCK GEOLOGY
98
C§g CUE DISTRICT
ñBRga-gm
Butchers Well
0
ñBRtg-gmp
$e
96
ñPOm-bb
C§m
Brewers Bore
94
Wf R´f
$e
L²
$e
ñBRtg-gma
R´f
C§f
92
Wf
$e
Murchison Domain
C
590
88
Bald Rock Supersuite
zq
L¯
86
Wf
Big Bell Suite
A¥
C ñSDY-og
ñgvlqYMU
Wq
L¥2
R´f
42 0
ñPOm-mbba
84
Yalgowra Suite
L²
82 42 0 ñPOm-mbms
Cullculli Suite
L¥e¨
580
78
Annean Supersuite
L¥1
No 11 Well
54
Lakeside Homestead 2 km
76
Murchison Supergroup
L¥1
74
42
Wq
L¥1
72
420
Creek
0
R´f
ñBRtg-gm
Casuarina Well
Yard
Rμg
Yard
zq
C
Wc
Wf
570
68
CENOZOIC
46
56
Bore
66
64
PROTEROZOIC
ñmwasYMU Spring
ñBRtg-gm
62
ARCHEAN
A¥
Rμg
$e
Wondinong Homestead 47 km
Balyer Bluff
560
58
R´f
420
56
C
118°0'
Cue 10 km
42 0
54
52
48 0
550
27°30' 58
117°50' Cue 10 km
PHANEROZOIC
117°40'
42
117°30'
SHEET 2442
42 0
AUSTRALIA 1 : 100 000 GEOLOGICAL SERIES
ñNOm-mbbs ñogYMU ñNOm-mbbs ñTUcu-mgmy
ñTUcu-gmfe
ñTUcu-gmfp
ñPOm-mibs ñogYMU ñapuYMU
ñTUcu-mgmy
ñapuYMU
ñgvlqYMU
Geology by I Zibra, 2009
SEA LEVEL
ñogYMU ñogYMU ñapuYMU
2 km
ñogYMU
ñgYMU
ñPOm-mbm ñapuYMU
DATA DIRECTORY Organization †
Geochronology by: (1) Wang, Q 1998, Australian National University, PhD thesis (unpublished),186p.
2009
Geological Survey of Western Australia, Department of Mines and Petroleum
(2) Schiøtte, L and Campbell, IH 1996, Precambrian Research, v. 78, p. 237–260.
Mineral sites *
MAR 2011
Geological Survey of Western Australia, Department of Mines and Petroleum
(3) Wiedenbeck, M and Watkins, KP 1993, Precambrian Research, v. 61, p. 1–26.
Structural data
MAR 2011
Geological Survey of Western Australia, Department of Mines and Petroleum
Horizontal control
MAR 2011
Landgate
Theme Geology *
ñgvlqYMU ñapuYMU
Topographic nomenclature
ñPOm-mbas
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 geochronology data are available online at .
Data Currency
2011
Landgate
Topography
2011
Landgate
Contours
2010
Geoscience Australia (Commonwealth)
4 km * DMP data can be viewed interactively via GeoVIEW.WA , and related datasets can be downloaded from the GSWA Data and Software Centre †
WA State Government unless otherwise indicated
Cartography by S Mulligan
SCALE 1 : 100 000 1000 Metres
0
1
2
3
4
5
6
7
UNIVERSAL TRANSVERSE MERCATOR PROJECTION HORIZONTAL DATUM: GEOCENTRIC DATUM OF AUSTRALIA 1994 VERTICAL DATUM: AUSTRALIAN 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
Edited by SR White and K Greenberg Published by the Geological Survey of Western Australia This map is published in digital format (PDF) and is available online at . 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 3444 Website Email
[email protected] The recommended reference for this map is: Zibra, I 2011, Austin, WA Sheet 2442: Geological Survey of Western Australia, 1:100 000 Geological Series.
8
AUSTIN SHEET 2442
FIRST EDITION 2011 Version 1.0 — October 2011
© Western Australia 2011
9
10 Kilometres
