GLENBURGH GEOLOGICAL SURVEY OF WESTERN AUSTRALIA
Yard
Rg
280
A1
ìMW-od
80
ìDA-moa od ìMW-od
W
W
od
od
ìMW-od
300
Rf
A1
C2
zq
80
C1q
od 60
82
A UL LE W – AR VO N CA RN
04
410
08
06
ìDA-moa ìDA-mgtw 14
12
od
83
Byro Homestead 80 km
ìDA-mgtw 360
C1q
80
80
ìMO-gp
80
Yard Salt Well
ìMO-gp
ìMW-od
420
18
Yalbra Well
24
28
ìMW-od Yard
380
ìMO-gp ìDAna-mgtl
Rf
ìBB-gtl
zq
ìMW-od
Rg
Ak
Rg ìMO-gp
C1 34
36
440
38
42
SOUTHERN CARNARVON BASIN
Lyons Group
Plagioclase–actinolite–tremolite gneiss; after gabbro
ìMG-xmh-mk
Moogie Metamorphics
od od ìMW-od
od
ðha-mgn
Halfway Gneiss
For further details refer to main reference 20
EDMUND BASIN
Bangemall Supergroup
PALEOPROTEROZOIC – MESOPROTEROZOIC
Edmund Group Mount James Subgroup
Cobble and boulder metaconglomerate; strongly foliated; locally includes quartzite and muscovite–quartz(–biotite) schist
Moorarie Supersuite
PROTEROZOIC
ìMOdu-ggp
460
Lineation, unspecified, showing trend and plunge Mineral lineation, showing trend and plunge 80
ìMO-mgmz
thrust, interpreted, triangle on upthrown side...........................................
Cleavage–cleavage intersection lineation, showing trend and plunge
116°10'
ìMO-gmp
ìMO-gp
ìMO-gmvl
Fold, showing axial trace and generalized plunge direction anticline, exposed, interpreted.................................................................
Mineral alignment, showing trend and plunge
syncline, exposed, interpreted.................................................................
inclined.....................................................................................................
60
antiform, exposed, interpreted.................................................................
Isotopic age determination site with identification number............................
164309
synform, exposed, interpreted................................................................. Road, unsealed..............................................................................................
75
Track.............................................................................................................. Fence, generally with track............................................................................ Homestead.....................................................................................................
unspecified...............................................................................................
60
S-vergence...............................................................................................
71
B
Gascoyne River
Yard...............................................................................................................
Yard
Horizontal control; major. minor.....................................................................
inclined.....................................................................................................
60
way-up not known, inclined......................................................................
78
Breakaway.....................................................................................................
D
Watercourse with ephemeral pool................................................................. 60
SEA LEVEL
ðha-mgn
ìMGm-mls
zq
ìMG-mkk
ìmwaGAG ìMG-mkq ìMG-mkk
ìMO-gmeb
ðha-mgnw
4 km
ðha-mgnl
ìMG-mkk ìMW-od
zq
zq
ðha-mgn
ìMGm-mls ìmwaGAG
ðha-mgn ìMOsc-gm
od
zq
ðha-mgn
ìmwaGAG ìMG-mkq ðha-mgnl
ìMW-od ìMW-od
ìMG-mkk
od
zq zq
2 km
zq
ìMG-mkk
ìMGm-mls
ìMO-gmeb
zq
zq
ìMOdu-ggp
ðha-mgn
ìMG-mkq
zq ìMGm-mls
ìMG-mkq
ìMOdu-ggp
ìMGm-mtq ìMGm-mtsf ìMO-gmvl
zq
zq
ìMEy-st
ìMG-mkk
ìPOs-mtqs ìmwaGAG
zq
ìMO-mgmz ìMO-gmeb
ðha-mgn
ðha-mgnl ìmwaGAG
ìmwaGAG
Bore, Well...................................................................................................... 60
Windpump......................................................................................................
trend of foliation.......................................................................................
Mineral field boundary................................................................................... 60
inclined.................................................................................................... vertical..................................................................................................... Trend of foliation or gneissic banding............................................................
Unassigned Moogie Metamorphics
ìDA-mgml
ìDA-mgtw
ìDA-xmgt-mgm
ìDA-xmgg-mwo
ìDA-xmgt-mgg
ìDA-xmgml-mgg
ìDA-mgp
ìDA-moa
NARDOO GRANITE: foliated, medium-grained biotite metatonalite and meta quartz diorite; equigranular or porphyritic; abundant small mafic clots Foliated, medium-grained, weakly porphyritic, leucocratic biotite metatonalite and minor metagranodiorite Medium-grained, leucocratic biotite metamonzogranite; foliated; commonly with clots of biotite after garnet Fine-grained mesocratic metatonalite; minor fine-grained metamonzogranite and leucocratic metatonalite, medium-grained metatonalite and metagranodiorite, and leucocratic metamonzogranite and metagranodiorite Interlayered, fine-grained mesocratic metatonalite and fine-grained, pale grey, biotite metamonzogranite and leucocratic metatonalite; commonly with clots of biotite after garnet Foliated metagranodiorite and metamonzogranite sheets, with abundant layers of mafic granulite; minor pelite, including diatexite migmatite Interlayered medium-grained metatonalite and metagranodiorite together with leucocratic biotite metamonzogranite and metagranodiorite; subordinate fine-grained metatonalite and metamonzogranite; gneissic to weakly foliated Interlayered medium-grained, leucocratic biotite metamonzogranite and metagranodiorite; commonly with clots of biotite after garnet Coarse-grained leucocratic metapegmatite and metagranite; commonly with clots of biotite after garnet Amphibolite; locally mafic granulite
ìmliGAG
ìmwaGAG
ìmogGAG
MINERAL SITES
GASCOYNE PROVINCE
Bertibubba Supersuite Dalgaringa Supersuite
PALEOPROTEROZOIC
ìDAna-mgtl
COMMODITY GROUP
MINERALIZATION STYLE Porphyry, pegmatite, greisen, and skarn
Precious metal
Vein and hydrothermal
Steel alloy metal
Stratabound sedimentary and/or sedimentary banded iron-formation
Base metal Energy
Regolith hosted
ìmusGAG
Industrial mineral
All precious metal sites are gold unless otherwise indicated
ìmiGAG ìmliGAG ìmwaGAG ìmogGAG ìmusGAG
Metamorphosed banded iron-formation Migmatitic pelitic gneiss (diatexite migmatite) Amphibolite Plagioclase–actinolite–tremolite gneiss; after gabbro Fine- to medium-grained actinolite(–clinozoisite–albite–titanite) and tremolite(–serpentine–talc–calcite) schist
ìMGm-mtsf
COMMODITY
Pelitic schist commonly with chloritoid; locally with relict garnet porphyroblasts
Barite..........................................................Brt Beryl...........................................................Brl Cobalt........................................................ Co Copper....................................................... Cu Corundum.................................................. Cor Gold........................................................... Au
MUMBA PSAMMITE: quartzofeldspathic psammitic schist commonly with chloritoid; local minor pelitic schist and quartzite
Graphite..................................................... Gr
ìMGm-mtq
Lead........................................................... Pb
Metamorphosed quartz sandstone, granule metaconglomerate, and quartzite gneiss, locally micaceous; minor psammitic schist; locally with relict cross-bedding
Thorium...................................................... Th Tungsten.................................................... W
ìMG-mkq
Uranium......................................................U
ìMG-mkk
SITE NAME
Calc-silicate gneiss; pargasite- or diopside-bearing quartz–plagioclase–epidote(–titanite) rock; tremolite–diopside(–garnet) calc-silicate rock with minor marble Marble; dolomite(–quartz) and dolomite–calcite–forsterite–clinohumite–serpentine rock; locally contains garnet
ðha-mgn ðha-mgn ðha-mgnl ðha-mgnw
ðha-mgnl
Mine, deposit, prospect or occurrence....... Apollo 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 .
ðha-mgnw
HALFWAY GNEISS: interlayered leucocratic and mesocratic granitic gneiss, pale-grey granitic gneiss and foliated metagranite, and gneissic to foliated porphyritic metagranodiorite Leucocratic granitic gneiss and foliated leucocratic metagranite; derived from biotite monzogranite and granodiorite Mesocratic granitic gneiss; derived from variably porphyritic tonalite
MOUNT PHILLIPS 2149
od
GN MN
GRID CONVERGENCE 0.3°
Rf 82
2449
N.T.
MOUNT EGERTON SG 50-3
YINNETHARRA
PINK HILLS
CANDOLLE
2048
2148
2248
2348
MOUNT EGERTON 2448
GLENBURGH
LANDOR
ERRABIDDY
MARQUIS
MILGUN
2147
2247
2347
2447
2547
GLENBURGH SG 50-6
GRID / MAGNETIC ANGLE 0.2°
MOUNT VERNON 2549
TEANO
LOCKIER
DAURIE CREEK 2047
84
zq
MOUNT PEEDAWARRA AUGUSTUS 2349 2249
MOUNT PHILLIPS SG 50-2
ìDAna-mgt
ìMO-gp
od
Qld
MULGUL 2548
W.A.
S.A.
ROBINSON RANGE SG 50-7
N.S.W.
CARRANDIBBY
YALBRA
ERONG
GOULD
MOORARIE
PADBURY
2046
2146
2246
2346
2446
2546
A.C.T Vic.
1 : 100 000 maps shown in black 1 : 250 000 maps shown in brown Search for GSWA map products online
Tas.
ìDAna-mgtl ìMW-od
ìDAna-mgt
ìDA-xmgt-mgm
C1
46
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. 55"annually
7180
od
80
25°30'
48
E
ðha-mgn ìMW-od
zq ìMG-mkk
ìPOs-mtqs
ìMW-od
zq
zq
zq
zq
ìMOsc-gm
od
od
ìMOsc-gm
ìMO-gmeb
2 km
ìDA-xmgml-mgg
ìMO-gmeb
4 km
1000 Metres
DATA DIRECTORY Theme
(3) Sheppard, S et al. 2005, Australian Journal of Earth Sciences, v. 52, p. 443–460
Geology *
(4) Evans, DAD et al. 2003, Australian Journal of Earth Sciences, v. 50, p. 853–864 Edited by SR White Published by the Geological Survey of Western Australia.
od ðha-mgn
Geochronology by: (1) Wingate, MTD and Giddings, JW 2000, Precambrian Research, v. 100, p. 335–357
Cartography by S Coldicutt and AK Jones
ìDA-moa
SCALE 1 : 100 000
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 .
(2) Sheppard, S et al. 2007, Journal of Metamorphic Geology, v. 25, p. 477–494
ìPOb-mlpc ìDA-xmgt-mgg zq od
ìDA-moa ìMO-gmeb
SEA LEVEL
ìDA-moa
zq zq
Geology by SA Occhipinti and S Sheppard 1998–1999, and SP Johnson 2010
F
DALGETY DOWNS – LANDOR ROAD Fitzpatrick Anticline
ìMW-od ìmwaGAG
Bore
Fine-grained, massive, leucocratic tonalite and granodiorite
ìDAna-mgtl
zq
ìMW-od
ìMG-mkq
ìMG-mkk
ìMW-od od
ìMO-gmeb
Pool
Pool................................................................................................................
Gneissic banding, showing strike and dip
86
Rg
Deadman Fault
Dalgety Brook
320
Contour line, 20 metre interval......................................................................
116°30'
C
Glenburgh
Locality...........................................................................................................
Compiled by SP Johnson 2010
A
42
inclined.....................................................................................................
vertical.....................................................................................................
SCRUBBER GRANITE: porphyritic to equigranular, coarse-grained, biotite- and muscovite-bearing monzogranite, syenogranite, and pegmatite; locally tourmaline bearing DUMBIE GRANODIORITE: porphyritic, fine- to medium-grained granodiorite; minor monzogranite; medium to coarse tabular phenocrysts of K-feldspar; locally magnetite and allanite bearing Leucocratic, equigranular biotite–muscovite granodiorite; fine to medium grained; massive to weakly foliated Altered granite; consists of quartz–sericite–pyrite; locally foliated Massive, equigranular to sparsely porphyritic biotite monzogranite; medium and coarse grained; minor muscovite in places; includes some granodiorite and minor leucocratic tonalite Massive, medium-grained, porphyritic biotite monzogranite; round phenocrysts of K-feldspar up to 5 cm in diameter; minor fine- to medium-grained, sparsely porphyritic biotite monzogranite Medium- to coarse-grained, even-textured, leucocratic, biotite-poor muscovite monzogranite; locally foliated and metamorphosed Porphyritic to equigranular, coarse-grained, biotite- and muscovite-bearing monzogranite, syenogranite, and pegmatite; locally tourmaline bearing
Rf
116°20'
DIAGRAMMATIC SECTIONS
60
inclined.....................................................................................................
Metamorphic foliation, showing strike and dip
TN
C1
44
60
inclined..................................................................................................... Stretching lineation, showing trend and plunge
inclined.....................................................................................................
ìMO-ggev
70
inclined.....................................................................................................
Igneous contact, showing strike and dip
ìMO-gmeb
60
inclined.....................................................................................................
trend of bedding.......................................................................................
Rg
zq ìDA-mgtw
Cleavage, showing strike and dip
Yalbra Outcamp 14 km
116°0'
SOUTHERN CARNARVON BASIN
ìmogGAG
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: Occhipinti, SA, Sheppard, S and Johnson, SP 2011, Glenburgh, WA Sheet 2147 (2nd edition): Geological Survey of Western Australia, 1:100 000 Geological Series.
Data Currency
Organization †
2011
Geological Survey of Western Australia, Department of Mines and Petroleum
Mineral sites *
JUN 2011
Geological Survey of Western Australia, Department of Mines and Petroleum
Structural data
JUN 2011
Geological Survey of Western Australia, Department of Mines and Petroleum
Horizontal control
MAR 2011
Landgate
2011
Landgate
Topographic nomenclature Topography
2011
Landgate
Contours
2010
Geoscience Australia (Commonwealth)
* 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
0
1
2
3
4
5
6
7
8
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
GLENBURGH SHEET 2147
SECOND EDITION 2011 Version 1.0 — June 2011
© Western Australia 2011
9
10 Kilometres
EDMUND BASIN
Pooranoo Edmund Metamorphics Group
Bangemall Supergroup
Unassigned QUATERNARY
CENOZOIC PALEOZOIC
CARBONIFEROUS – PERMIAN
Pooranoo Metamorphics
ìPOb-mxq
Rg
Rf
GASCOYNE PROVINCE
Ga sco Mo un t
ìDAna-mgtl ìDA-xmgml-mgg
ìMG-mkq
Amphibolite
strike-slip, exposed, showing relative sinistral horizontal displacement... interpreted................................................................................................
EUDAMULLAH
Yard
Parrot Bore
ìDAna-mgtl
ìmwaGAG
Kilometres
2049
Rg Yard
Rf
Dalgaringa Supersuite
88
Pool
ìDAna-mgt
W
ìDA-mg
od
Bedding, showing strike and dip
Rf ìDA-moa
od ìDA-xmgt-mgm
A
ìMW-od zq
Moorarie Supersuite
ìMW-od
SCALE 1: 500 000 10 15
5
ìMO-g
SHEET INDEX
ìMW-od
77
71
Rf Well
ìMW-od
ìMW-od
0
Yard
ìDAna-mgtl
ìDAna-mgt
Mount James Subgroup
ìDA-moa
ìMW-od
C1
ìPOJ-md
S
ìDAna-mgtl
C1q
Pool
ìMG-mkq
40
od 142928 od Ak 142929 ìBB-gtl od od
zq
ìMW-od
ìMO-gp
32
ìMW-od od
od ìMW-od ìDA-xmgt-mgm ìBB-gtl
W
ìDAna-mgtl
ìMW-od
od
C1q
Ak
zq ìMW-od zq
zq
430
Rg
od
C1
69
ìDA-xmgt-mgm 26
od
70
C1q
Rg
22
yne
0 36
ìMO-gp
Yard
Rg
od
od
ìDA-mgml
C1q C1
od
ìDA-moa Ak od
380
od
Cree k
ìDA-mgml
380
340
od
od
ìDAna-mgt
86
7190
2663–2429 Ma
81
od
ìMW-od
58
ìDA-xmgt-mgm
ìMW-od
od
Small-scale fold axis, showing trend and plunge
Phyllite and slate; locally chlorite rich with magnetite porphyroblasts
ìMG-mkq ìMG-mkk
92
80
ìMW-od
Rf Minga BoreìMW-od
od
Glenburgh Terrane
360
360
0 36
od ìMW-od 86
ìDAna-mgtl
ìDA-xmgt-mgm
ìMO-gp zq ìDA-moa
zq
ìMG-mkq ìMW-od ìDA-mgtw
Yard
od
NEOPROTEROZOIC
380 0 40
Dardoo Well
Cree k
ìDA-xmgt-mgm
38 0
360
380
ek Cre
ìMO-gp
Yard
Depositional Package 1 (Yilgatherra, Irregully Formations)
Rg
zq
od 78
ìMG-mkq
ìDA-mgml
Geeranoo
ìDA-moa
16
ìDAna-mgt
C1
84
ìDA-moa
zq
ìDA-mgtw
od
od
od ìMW-od od
ìMW-od od
ìMW-od
ìDA-mg
Rf C2
ìMW-od ìDAna-mgt
ìDAna-mgtl
ìMW-od
od
od
83
ìMW-od ìDAna-mgtl
zq
Gr
36 0
ìDA-mgtw
od
od
zq
ìMW-od
McIntosh Well ìMG-mkq
Ak
Yard
C1q
zq
od
W
ìDAna-mgtl
ìMW-od
0
Rg
0
340
32
zq
2240–2125 Ma
C1
zq
83
ìDA-xmgt-mgm
85
ìDA-mgtw
Rg
od
ìDA-mgtw
Conroy Well
94
C1
40
Cree k 02
C1
ìDA-mgml ìDA-mgp
80
ìDAna-mgt
ìPOb-mlpc
ìMGm-mls
Rf
zq 80
2083–1997 Ma
96
C1
ìMW-od 84 od
Yard
Rg
ìMG-mkq
Yard
od
od ìMW-od
ìDA-mgtw
ìDAna-mgtl
od zq
od
McIntosh Well
ìMG-mkq
ìMW-od
ìMW-od
C1q
33
M
zq
C1
ìDA-moa
od
C1
Bore
od od
ìMEP1-kt
400
83
72
C1
ìDA-xmgt-mgm
Ak
od
ìDA-mgp
od od
78
oo
32 0
32
zq
zq
od
61 60
od
Yard
zq
od ìDA-mgtw
142932
D
ìMW-od
Dard
ìDA-moa
A RO
ìDA-xmgt-mgm ìDA-mgml
zq
od
83
Creek
ìDAna-mgtl ìMO-gp
C2
zq ìMW-od
0
Well
ìMW-od
75
ìDA-mgml ìDA-moa
75
ulla
ìDA-mgml
16
280
280 7180000m N
YA LB RA
C1
zq
69
ìDA-mgtw
C2
A1 400000mE
Rf zq
320
m rn a Bo o
ìDA-xmgt-mgm
Rg
ìDA-mgml ìDA-xmgt-mgm
Rz
C1
od
340
ng o Co
zq
142923
RO AD
Rf
ìDA-mgml
ìMW-od
80
84
Yard Deep Well
od
od
od
380
ìDA-xmgt-mgm
od
ìDA-xmgt-mgm ìDAna-mgt ìMO-gp Ak 34
ìMW-od ìDAna-mgtl ìMW-od
142930
ìMW-od
ìDA-moa
zq
ìDAna-mgtl
ìDA-xmgt-mgm Yard
ìDA-mgml ìMW-od
ìMW-od
340
ìMW-od
Rg
300
æåLY-sepg
Rg
25°30'
Glenburgh
0
ìDA-mgtw 142933 ìDA-mgml ìMW-od ìDA-xmgml-mgg ìDA-moa
od ìMW-od ìDA-moa
Rg
W
C1
landing ground
Yards
C1
S
ìDA-moa
Yard
320
88
Yard
Meerawana Well
38
ìDA-moa
od ìDA-xmgt-mgg od ìDA-xmgml-mgg od ìMW-od ìDA-moa ìDA-moa zq
ìDA-mgml ìMW-od ìMW-od
ìDA-mgml
ìDA-xmgt-mgm
Rf
od
zq
od
Well Yard
Rz
zq 340
ìDA-moa
zq
od
ìMW-od
75
Pools
ìMW-od
ìDA-xmgt-mgm
zq
81
360
zq
ROA D
ìDA-mgml ìMW-od ìDA-moa
Ak
ìDA-mgml Ak ìDA-moa
ìDA-moa od
od
ìDA-moa
od
od
ìDA-mgml
ìPOb-mtef
ìDAna-mgt ìDAna-mgtl ìDA-mgml ìDA-mgtw ìDA-xmgt-mgm ìDA-xmgg-mwo ìDA-xmgt-mgg ìDA-xmgml-mgg ìDA-mgp ìDA-moa
25°20'
ARCHEAN – PROTEROZOIC
ìDA-xmgg-mwo
Tuxedo
MULL E WA
ìDA-moa
85 Rf Paradise Well Yard
zq
ìDA-mgml
ìDAna-mgt
od
vertical......................................................................................................
BIDDENEW FORMATION: feldspathic metasandstone and minor feldspathic pebbly metasandstone; medium to coarse grained; locally ripple marked and cross-bedded
ìDAna-mgt
W
380
Well
zq
68
A
zq
Ak
380
NS DA LG ET YD
OW
Yard
Icon
85
C1
Well
Yards
A
A
380
A1
ìDA-xmgt-mgg
ìDA-moa
ìDA-moa od
ìMW-od
Yard
98
Mulunka Well
Yard
A1
ìDA-xmgt-mgm
380
–
Apollo Mustang
C2
50
ìmliGAG
185942
od
ìDA-moa od
380
Cree k
Shelby
Hurricane ìDA-mgml od
ìDA-moa zq ìDA-xmgg-mwo ìDA-mgml
0
EN –
GL Kileytharra Well
ìDA-moa
70
zq od ìDA-moa
ìMW-od
zq
84
od
inclined.....................................................................................................
SPRING CAMP FORMATION: quartzite and quartz–muscovite schist; foliated; quartz metasandstone, feldspathic metasandstone, and quartz-lithic metasandstone; locally ripple marked and cross-bedded
ìBB-gtl
S
A
C1q
Yard
od
Small-scale fold axial surface, showing strike and dip
ìmiGAG
ok
ìDA-moa ìDA-xmgml-mgg
zq Zone 126 ìDA-moa Zone 102
zq
zq
zq
zq
C1q
YILGATHERRA FORMATION: sandstone; subordinate siltstone, conglomerate, and dolostone
ìPOs-mtqs
ìMOsc-gm ìMOdu-ggp ìMO-ggev ìMO-mgmz ìMO-gmeb ìMO-gmp ìMO-gmvl ìMO-gp
Ak
o Br
zq
30 0
ìmiGAG
C1
NE 3
Yard
od
Ak
34
RG H BU
320
ìmusGAG
69
83
zq
Well
Yard
02
142927
73
Mundine Well Dolerite Suite
ìMW-od od
inclined.....................................................................................................
7200
380
280 320
zq
C1
ìDA-moa od
340
oo
ìDA-moa
7190
86
Um ba
k ee 300
ìmiGAG
od
ìDA-moa od
340
300
Carlo
280
ìDA-xmgt-mgg
80
CA Yard RN AR VO S N
Mumba
Creek
r Sch ro e de
260
ìDA-xmgml-mgg
0 34
n er a Ge
ìDA-moa
Rg
A2
0 32
Gascoyne River od
zq Yard
Boonka Well
ìMEy-st
2002–1974 Ma
od
142926
ìMW-od
c.1945 Ma
ty
94
C1q
75
Ak
ìDA-moa
ìmiGAG
A
Cu,Pb,Au ìDA-xmgml-mgg
92
340
28 0
k ee Cr
300
Dairy Creek Homestead 17 km
Cr
0 32
ìDA-moa
ìDA-xmgt-mgg
A
85
ìDA-xmgt-mgg ìDA-xmgt-mgm Ak ìMW-od od
C1
A1§
ìMO-gmeb
lg e Da
Dairy Creek Homestead 20 km
Dalgety Downs 3 Yard
C1
A ìDA-xmgt-mgg
0
Yard
AD
od
ìDA-moa
34
32 0
96
RO
od
C1
75
380
zq
landing ground
Ak
ìDA-xmgt-mgg
zq
od
od
C1q
400
300 75
50
75
od
W
ìDA-moa zq
61
ìDA-moa
ìDA-xmgml-mgg
zq
od
78
zq
Rg
ìDA-moa
Yard
Sandstone, conglomerate, siltstone, and dolostone
ìMOsc-gm
360
C1
340
ìDA-xmgml-mgg
od
71
C1
ìDA-xmgt-mgm
ìMW-od zq
od
ìMW-od
Glenburgh Orogeny (2005– 1950 Ma)
04
zq
360
80
380
300
ìDA-xmgt-mgg
ìPOb-mlpc Sonny Well
ìDA-moa
od
Well
0 32
75
ìDA-moa zq ìDA-xmgml-mgg
78
ìDA-moa
C2
3 40
Rg
Rf
80
ìPOs-mtqs
ìPOs-mtqs
ìMO-ggev ìMO-ggev ìMW-od
3 40
ìPOb-mlpc
zq
Yard
320
50
zq
360
zq
C1
142925
36 0
zq
59
78
Yard Challenger Well
06
A1
142924
ìDA-moa
zq
od
0
320
ìMW-od
78
79
Hadlam Well
Yard
72
80
ìMW-od
ìDA-moa
A1 Yard
ìDA-xmgt-mgg
ìDA-xmgt-mgg zq
ìDA-mgtw zq
C1q
75
zq
ìDA-moa
C1q
zq
C2
A1
Ak
ìPOs-mtqs ìPOb-mlpc
zq
80
ìDA-xmgml-mgg
zq
75
320
30 0
ìMEi-kd ìMEi-st
landing ground
ìDA-xmgml-mgg od
zq
C1 Cu Ak Dalgety Downs / Richards Cu Dalgety Downs Cu,Au
Nings Bore
zq ìMW-od
zq
Br ook
40
landing ground
ìmusGAG zq
zq
C1q
Dalgety Downs 2
ìDA-moa
73
ìDA-xmgt-mgg
08
A1
ìMO-ggev
ìMO-ggev
80
A1§
C1
W
od
IRREGULLY FORMATION: stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate
ìMEi-st
1811–1799 Ma
ìMO-gmeb
od
C1q
C1
ìDA-xmgml-mgg
ìDA-mgtw
zq
zq
Ak
0
40
ìMW-od
zq
zq
ìDA-xmgml-mgg
Dalgety
Dilly Dally Well
ìMW-od
ìMW-od
Yard Well
Rg
C1
40
zq
ìDA-mgml
ìPOs-mtqs
86
od
C1 Area 20
ìMW-od 60
ìmusGAG od
od
Yard
A1
Woodcock Well Yards
od
od
od
75
od
F
A1
Mollies Well
70
300
ìDA-moa
Cu ìMW-od
98
od
ìDA-moa od
ìMW-od
168937
ROAD
R
70
0
300
od
Rg
ìMG-mkk Ning Bore U,Th,Pb
ìMW-od
landing ground
Dalgety Downs
ìDA-moa
od
W
zq
landing ground
A1
ìPOs-mtqs
Ak Rz
ìDA-xmgt-mgg
36
ìDA-xmgml-mgg
70
lin e
thrust, exposed, triangle on upthrown side, showing dip..........................
Ma 2)
Capricorn Orogeny (1820– 1770 Ma 4) Gregory Bore
ìDA-xmgt-mgg ìMO-ggev
zq ìDA-mgtw
od
34
od ìMG-mkq
od
280
320
65
28 0
ìDA-xmgt-mgg
C1q
zq ìMG-mkk zq
60
od
ìMW-od
ìmiGAG
od
80
Y GET DAL
60
65
Yard
DO L AN S – N W DO
85
ìMEi-kd
ìMO-ggev
ìDA-xmgml-mgg
360
C2
ìMW-od
zq
od
od
360
50
ìPOs-mtqs
W
A1§
ìPOs-mtqs ìPOb-mlpc
Fitzpatrick Well
Cu
360
320
zq
ìMG-mkk
49
80
od
ìDA-moa
Dalgety Downs 4
ìDA-moa
0 38
ìMG-mkk
zq
04 ìMGm-mls
7200
ìMW-od
65 70
ìDA-xmgml-mgg ìDA-moa
25°20'
ìMG-mkq
od
0
zq
ìMG-mkk
zq ìDA-moa
74
