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04 May 2006 07:28:19 U:\CAMP\Projects\Archived\100_000\Elliott_Creek\2250-GDA.dgn
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Cobbina Yard(abd)
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landingground
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landing ground(Hoppys Strip)
ALICIA TABLETOPlanding ground
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Yard
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Cobra Homestead 25 km
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WHITE CLIFFS
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(abd) (PD)
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C3C2
C2
C2
C2
C2
C2
C2
C2
C2
C2
ìMEi-st
C3
A
A1
A1
A1
A1
A1
A1A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
A1
38
20
29
30
84
40
19
20
36
19
9
23
2210
71
19
34
16
9
4
31
16
14
13
28
20
14
13
3
7
5
17
8
4
18 7
12
6
14
24
30
14
19316
21
282014
28
24
17
24
20
34
20 7077
24
22
18
25
11
21
21
3318
45
90
9
9
16
19
38
19
29
9
17
10
13
16
15
868
14
1450
65
35
4
9
11
8
20
13
5
7
6
11 12
10
10 10
16
16
19
119
751
22
84
1
41
20
3057
74
66
69
1
34
73 64 57
67
50
38
2051
55
5219
1 79
44
69
5 10
381
5 166 35
10
6
2
12
25
12
1
13
1 88
30
5861
4
12
11
87
3
8
20
15
12
19
5
20
3
4
25
18
45
77
57
42
42
68
75 1
80
18
4880
42
65
68
68
57
6162
54
68
166042
19
1 80
75
68
8548
1
60
1
78
6570
55
25
55
4678
1
7070
55
48
22
68
30 82
1
42
46
4882
17062
20
801
70
2
44
60
8
48
16
25
4
4
3
1
8
1
1
12
10
22
1
1
38
C3
C3C3
C3
C3
C3C3
C3 C3
C3
C3
C3C3
C3
C3
C3
C3
od
212
Dmd
2148
Mn
2149Mn
2150Mn
2151
G A S C O Y N E M I N E R A L F I E L D
A S H B U R T O N M I N E R A L F I E L D
Asbs
Asbs
Dmd
Mn
2149
? ?
? ?
58
SM 30
15
10
Wanna Syncline
2
Edmundian Orogeny (1070Ê755 MaÝä)
Capricorn Orogeny (1805Ê1780 MaÝì)
40À116°30À
24°00À
50À 117°00À
24°00À
50À
40À
23°30À
117°00À50À40À116°30À
50À
40À
23°30À
SHEET 2250AUSTRALIA 1Ý:Ý100Ý000 GEOLOGICAL SERIES GEOLOGICAL SURVEY OF WESTERN AUSTRALIA
Geological boundary
exposed...........................................................................................................
deformation events, where known
e 2
e 1
a
a
Edmund Fold Belt (DÛÝ )..........................................................................
Edmund Fold Belt (DÕÝ )..........................................................................
Ashburton Fold Belt (DÛÝ ).......................................................................
Ashburton Fold Belt (DÕÝ ).......................................................................
4
3
Fault
exposed...........................................................................................................
concealed........................................................................................................
anticline; exposed, concealed.......................................................................
syncline; exposed, concealed.......................................................................
Small-scale fold axial surface, showing strike and dip
inclined............................................................................................................
vertical.............................................................................................................
syncline...........................................................................................................
S-vergence......................................................................................................
M-vergence.....................................................................................................
Bedding, showing strike and dip
inclined............................................................................................................36
Cleavage, showing strike and dip
inclined............................................................................................................80
22
Airphoto lineament
Track.......................................................................................................................
Homestead.............................................................................................................
Yard........................................................................................................................
Contour line, 20 metre interval............................................................................
Spring.....................................................................................................................
Windpump..............................................................................................................
Abandoned, position doubtful..............................................................................
Bore........................................................................................................................
Well.........................................................................................................................
¦
TRANSVERSE MERCATOR PROJECTION
Grid lines indicate 1000 metre interval of the Map Grid Australia Zone 50
HORIZONTAL DATUM: GEOCENTRIC DATUM OF AUSTRALIA 1994VERTICAL DATUM: AUSTRALIAN HEIGHT DATUM
0 1 2 3 4 5 6 7 8 9 10
KilometresMetres
1000
SCALE 1:100Ý000
2048
2049
2050
2051
2148
2149
2150
2151
2248
2249
2250
2251
2348
2349
2350
2351
2448
2449
2450
2451
2548
2549
2550
2551
LOCKIER
EUDAMULLAH
MANGAROON
MAROONAH
YINNETHARRA
EDMUND
ULLAWARRA CAPRICORN
CANDOLLE
PEEDAWARRA
ASHBURTON
TEANO
BOGGOLA
PARABURDOO
MULGUL
KALLENIA
EDMUND TUREE CREEK
MOUNT EGERTONMOUNT PHILLIPS
SG 50-2 SG 50-3
SF 50-14 SF 50-15
PINK HILLS
MOUNT VERNON
SNOWY MOUNT
KENNETH RANGEELLIOTT CREEK
MOUNT PHILLIPSMOUNT
AUGUSTUS
MOUNT EGERTON
1:100Ý000 maps shown in black
1:250Ý000 maps shown in brown
SHEET INDEX
GNMN
GRID / MAGNETIC
GRIDCONVERGENCE
True north, grid north and magnetic north
are shown diagrammatically for the centre
of the map. Magnetic north is correct for
TN
0.1¾
Building..................................................................................................................
Mineral field boundary...........................................................................................
4 km
2 km
SEA LEVEL SEA LEVEL
2 km
4 km
DIAGRAMMATIC SECTIONA B
Collier Group
Edmund Group
Wyloo Group
concealed........................................................................................................
Fence, generally with track...................................................................................
Dolerite dykes and small intrusions
COLLIER BASIN
EDMUND BASIN
Structural symbols are labelled according to the sequence of deformation
Capricorn Orogeny (1830Ê1780 Ma)
normal, tick on downthrown side.................................................................
reverse, triangle on upthrown side...............................................................
concealed, position uncertain.......................................................................
anticline...........................................................................................................
Small-scale fold axis, showing trend and plunge
inclined............................................................................................................
ASHBURTON BASIN
Watercourse with ephemeral pool or waterhole................................................
Quartz vein
Fold, showing axial trace and generalized plunge direction
BeddingÊcleavage intersection lineation, showing trend and plunge
SHEET 2250
B
A
The Map Grid Australia (MGA) is based on the Geocentric Datum of Australia 1994 (GDA94)
GEOCENTRIC DATUM OF AUSTRALIA
GDA94 positions are compatible within one metre of the datum WGS84 positions
GEOLO
G IC A L SURV EY
WE
ST
E R N A U S T RA
LIA
TIM GRIFFIN
DIRECTOR
Geological Survey ofWestern Australia
0 5 10 15 20
Kilometres
SCALE 1:Ý500Ý000
W Wf A L
WWf
A
L
Sandy and clayey distal sheetwash and slope deposits, no clearly defined drainageFerruginous sand and silt
Silt, sand, and gravel in active drainage channels and adjacent to floodplains; includes ferruginous deposits
C1C1c£C1fC1qC1tsµ
C1 C1c£ C1f C1q C1tsµ A1 A1c£
A1A1c£
Quartz and rock fragments in an unconsolidated silt and sand matrix; includes ferruginous deposits
Unconsolidated ferruginous rubble and screeQuartz fragments in an unconsolidated silt and sand matrix, derived from quartz veins and quartzose rockSandstone fragments in a silt and sand matrix, derived from sandstone
Unconsolidated silt, sand, and gravel in active drainage channels; includes ferruginous depositsSwelling clay (gilgai) developed on alluvial flats
C2
C2 A2
A2
Quartz and rock fragments in a partly consolidated silt and sand matrix
Partly consolidated silt, sand, and gravel; partly dissected by present-day drainage
C3 A3
C3
A3
Sheetwash units
Alluvial unit
Lacustrine unit
Colluvial units, third generation
Alluvial units, third generation
Colluvial units second generation
Alluvial unit, second generation
Colluvial unit first generation
Alluvial unit, first generation
Residual or relict units
Rf Rk Rz
RfRkRz
Ferruginous deposits, including lateritic, ferruginous, and manganiferous duricrust
Silcrete and brecciated siliceous caprock
od
zq
ìodÀ
Quartz veins, of various ages
c.
Dolerite and gabbro sills intruded into
ìMCi-s
ìMCc-s
ìMCb-s
ìMCb-st
ìMCb-kd
ILGARARI FORMATION:
BACKDOOR FORMATION:
CALYIE FORMATION:
siltstone, mudstone, and thin- to thick-bedded sandstone; minor chert and dolostone
siltstone, mudstone, and fine-grained sandstone
quartz sandstone, siltstone, mudstone, conglomerate, and dolostone
Thin- to thick-bedded sandstone and siltstone
ìod¿,À Edmund Group c.c.
COODARDOO FORMATION:
ULLAWARRA FORMATION
ULLAWARRA FORMATION:
DEVIL CREEK FORMATION:
DISCOVERY FORMATION:
Curran Member:
thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone
siltstone and fine- to coarse-grained sandstone; locally intruded by dolerite sills; has gradational contacts with underlying
laminated dolostone and dolomitic siltstone; local thick-bedded dolorudite
ìod¿,À
MUNTHARRA FORMATION:
ìMEc-s
ìMElc-sf
ìMEl-s
ìMEv-k
ìMEd-c
ìMEm-k
ìMEk-s
ìMEk-st
thin- to thick-bedded dolostone and stromatoloitic dolostone, and sandstone and siltstone
KIANGI CREEK FORMATION:
ìMEk-kd Dolostone, siltstone, and sandstone
ìMEk-sl
CHEYNE SPRINGS FORMATION: dololutite, dolarenite, dolorudite, mudstone, siltstone, and minor sandstoneìMEp-k
ìMEb-sl BLUE BILLY FORMATION: siltstone and mudstone; minor thin- to thick-bedded sandstone; locally sulfidic
ìMEg-s GOORAGOORA FORMATION: fine- to coarse-grained sandstone and siltstone; minor conglomerate, dolostone, and dolomitic siltstone
ìMEi-k IRREGULLY FORMATION: stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate
ìMEi-st
ìMEy-s YILGATHERRA FORMATION:
ìWa-s
Rzi
Rzi Ferruginous silcrete and brecciated siliceous caprock
ASHBURTON FORMATION
Unas
signe
dQU
ATER
NARY
CAIN
OZOI
C
PHAN
EROZ
OIC
Collie
r Gro
up
MES
OPRO
TERO
ZOIC
c. 1070 MaÝåÝè
Bang
emal
l Sup
ergr
oup
PALA
EOPR
OTER
OZOI
C _
MES
OPRO
TERO
ZOIC
Edm
und
Grou
p
PROT
EROZ
OIC
c. 1620 MaÝê
Wylo
o Gr
oup
COLL
IER
BASI
NED
MUN
D BA
SIN
ASHB
URTO
N BA
SIN
PALA
EOPR
OTER
OZOI
C
ìodÀ
ìodÀ
ìodÀ
ìMEb-sl
ìMEb-sl
ìMEb-sl
ìMEb-sl
ìMEv-k
ìMEv-k
ìMEg-s
ìMEg-s
ìMEp-k
ìMEp-kìMEk-sìMEk-s ìMEk-s
ìMEk-s
ìMEk-sìMEk-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEl-s
ìMEd-c
ìMEd-c
ìMEd-c
ìMEc-s
ìMEc-s
ìMEl-s
ìMElc-sf
ìMElc-sf
ìMCb-s
ìMCb-sìMCb-s
ìMCb-s
ìMCb-st
ìMCb-st
ìMCb-st
ìMCc-s
ìMCc-s ìMCi-s
ìMEk-st
ìMEk-st
od
od
odìMEi-k
ìWa-s
ìWa-mh
W.A.
N.T.
S.A.
N.S.W.
Vic.
Qld
Tas.
A.C.T.
ìMCb-kd
Department of
CLIVE BROWN, M.L.A.
MINISTER FOR STATE DEVELOPMENT
JIM LIMERICK
DIRECTOR GENERAL
Industry and Resources
FIRST EDITION 2004
Precious mineral
Steel industry metal
Industrial mineral
MINERAL AND ROCK COMMODITY GROUPS
MINERAL OCCURRENCES
MINERAL AND ROCK COMMODITIES
Asbestos, serpentine (chrysotile)...............................
OPERATING STATUS AND SITE IDENTIFICATION NUMBER
Regolith hosted
Mineral occurrence or prospect e.g.
MINERALIZATION STYLESÝ
Diamond.......................................................................
Manganese...................................................................
ìMEb-sl ìMEg-sìMEi-st
ìMEb-sl
ìMEp-k
ìMEk-st
ìMEp-k
ìMEi-st
ìMEg-sìMEi-k
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,À
ìod¿,Àìod¿,À
Unconsolidated, fine-grained deposits in claypans, perennial lakes, and swamps; low-lying areas with internal drainage; usually thickly vegetated
Swelling clay (gilgai) and rock fragments, mostly developed over dolerite
Weakly cemented and compacted silt, sand, and gravel; deeply dissected valley-fill deposits
Calcrete, developed in and adjacent to alluvial channels; locally silicified; dissected by major present-day drainage lines
Dolerite dykes, sills, and small intrusions, of various ages; one suite dated at 755 MaÝâ; dashed where interpreted from aeromagnetic data
Thin- to thick-bedded dololutite, dolomitic siltstone, dolarenite, and siltstone
ìod¿ ìodÀ
and overlying COODARDOO FORMATION
siltstone, fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills ( )
massive or laminated chert, and silicified mudstone, and siltstone; local silicified sandstone and conglomerate
siltstone, mudstone, and thin to very thick bedded quartz sandstone; minor dolostone and conglomerate
Medium to very thick bedded quartz sandstone and siltstone
Siltstone; minor fine-grained sandstone
sandstone, siltstone, conglomerate, and dolostone
ìWa-mh
ìWa-sìWa-mh
zq
ìod¿,À
Dolerite and gabbro sills
Dolerite and gabbro sills
ìMC-s
ìME-s
ìW-s
Version 1.0 _ June 2004
Western Australia 2004
Western Australia Geological Survey, 1:100Ý000 Geological Series
The recommended reference for this map is:
100 Plain Street, East Perth, WA, 6004. Phone (08) 9222 3459, Fax (08) 9222 3444
Published by the Geological Survey of Western Australia. Digital and hard copies of thismap are available from the Information Centre, Department of Industry and Resources,
(1) M. T. D. Wingate and J. W. Giddings, 2000, Precambrian Research, v. 100, p. 335Ê357.Geochronology by:
Interpreted geochronology by:
(3) M. T. D. Wingate, 2002, GSWA Record 2002/4.
(5) D. R. Nelson, 1998, GSWA Record 1998/2, p. 194Ê197.(4) D. R. Nelson, 2001, GSWA Record 2001/2, p. 10Ê20.
WebÝ www.doir.wa.gov.au/gswa EmailÝ [email protected]
(2) D. McB. Martin and A. M. Thorne, 2004, Precambrian Research, v. 128, p. 385Ê409.
(6) S. Sheppard, et al., 2001, GSWA Record 2001/5, p. 3Ê4.(7) C. E. Hall, et al., 2001, Australian Journal of Earth Sciences, v.48, p. 731Ê744.
(9) K. N. Sircombe, 2003, Australian Journal of Earth Sciences, v. 50, p. 967Ê974.
ìMCb-st
od
ìMCb-st ìMElc-sf
od
unspecified......................................................................................................
1829Ê1806 MaÝîÝðÝò
(8) GSWA, in prep., GSWA Record.
2004 and moves easterly by about 0.1^ in
For further details, refer to main reference
Quartz and rock fragments in a weakly cemented and compacted silt and sand matrix; deeply dissected valley-fill deposits
andEdmund Collier Groups
Dolerite and gabbro sills intruded into Ý; oldest suite ( ) dated at 1465 MaÝåÝè and youngest suite ( ) dated at 1070 MaÝåÝè
Bang
emal
lSu
perg
roup
Bang
emal
lSu
perg
roup
Fault
DATA DIRECTORY
Theme AgencyData Source Data Currency
Geology 1998ÝÊÝ2001GSWA
Topography DLI and GSWA field survey 2001
Structural data WAROX
GEONOMA
Cadastre TENGRAPH APR 2004
MAY 2004GESMARHorizontal control
Topographic nomenclature
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Industry and Resources
Dept of Land Information
Dept of Land Information
Dept of Land Information
MAY 2004
MAY 2004
APR 2004
WAMIN MAY 2004 Dept of Industry and Resources
Mineral occurrences(non-confidential)
Geology by D. McB. Martin, A. M. Thorne, and I. A. Copp 1997-98, and D. McB. Martin 2003 Edited by F. Eddison and G. Loan
Cartography by P. Taylor and B.Williams
MARTIN, D. McB., THORNE, A. M., and COPP, I. A., 2004, Elliott Creek, W.A. Sheet 2250
Edmundian Orogeny (1070Ê755 Ma)
Fold axes
INTERPRETED BEDROCK GEOLOGY
concealed, interpreted from aeromagnetic data........................................
Stratabound sedimentary
ANGLE 1.1¾
1 years.
Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist faciesInterbedded psammite and pelite; includes quartzÊmuscoviteÊbiotiteÊcordieriteÊandalusiteÊgarnet schist and quartzÊmuscoviteÊbiotiteÊstaurolite schist;
upper greenschist to amphibolite facies (Section only)
MINEDEX
ìMEy-s
ìMEy-s
ìMEy-s
Road, unsealed......................................................................................................
Sandstone, conglomerate, siltstone, and dolostone
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