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Port Hedland 195 kmPort Hedland 195 km

Newman 55 km Newman 55 km

Warrie Outcamp

Bonney Downs

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1249 m

507 m

832 m

423 m

457 m

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C H I C H E S T E R

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Byer W

Banjo W

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Cockeye B

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Koolandie W (abd)

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Trig W (abd)

Woggie W

Bonney W

Ballas W (abd)

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Dandy W

Bustler W

Jack W (abd)

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Bookagee W

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Murrays Hill

Chichester West

Chichester East

Dales Gorge

Yampire North-Dales Gorge

Koodaideri West

Koodaideri Central

Mount LockyerSouthwest

Juna Lockyer

Koodaideri K75

K58

K38

K21

Marillana Creek

Marillana CreekCentral 5

Camp Hill

Wildflower Mountain

Juna Downs

Hill 65

Fork N

Meander

The Noose

Floodplain

Deposit EDeposit F

Deposit D

Deposit C

Junction

Ore body 10

Ore body 7Ore body 6

Deposit A

C Range

Deposit R

Hope Downs

Ore body 13

Ore body 4

Ore body 11

Ore body 14 Mindy Mindy

Mount Lockyer

West

Marrillana 2

Deposit B

Marillana Creek

Fe

P I L B A R A M I N E R A L F I E L D

W E S T P I L B A R A M I N E R A L F I E L D

M A R B L E B A R D I S T R I C T

N U L L A G I N E D I S T R I C T

Munjina

Marillana Station

Devans

Pool

Weeli Wolli

Chichester RangeGroup

Ore body 12

Koodaideri 186

Goodiadarrie Hills

DevansMn

Fe

Fe

Fe

Fe

Fe

Mn

Ad

Gs

Gr

? ?

Shaw Granitoid Complex Yule Granitoid Complex

M 1078

M 10

M 6578

OPHTHALMIA FOLD BELTYandicoogina SynclineWeeli Wolli Anticline

2

2

1

Calcrete_sheet carbonate; found along major drainage lines

Hematite-goethite deposits on banded iron-formation and adjacent scree deposits

MOUNT McRAE SHALE and

Pelite and thin-bedded metadolomite

Quartz vein

Metadolerite dyke

Metabasalt and metamorphosed pyroxene spinifex-textured basalt, chlorite schist, and tremolite schistMetamorphosed pyroxene spinifex-textured basalt and tremolite schist

Metagabbro and hornblende schist

QUAT

ERNA

RY

CAIN

OZOI

C

PHAN

EROZ

OIC

PROT

EROZ

OIC

ARCH

AEAN

2490 Ma

Geological boundary

exposed..........................................................................................................

Fault

exposed..........................................................................................................

concealed.......................................................................................................

Minor fold, showing strike and dip of axial surface, trend and

Capricorn Orogeny

inclined..............................................................................................

vertical...............................................................................................

Pre-Fortescue Group

strike and dip estimated from aerial photographs

horizontal.................................................................................................

16_45¾.....................................................................................................

46_90¾.....................................................................................................

0_15¾.......................................................................................................

Pre-Fortescue Group

vertical......................................................................................................

Cleavage, showing strike and dip

Capricorn Orogeny

inclined..............................................................................................

Pre-Fortescue Group

Formed road........................................................................................................

Track.....................................................................................................................

Homestead...........................................................................................................

Building.................................................................................................................

Yard.......................................................................................................................

Horizontal control, major.....................................................................................

Watercourse, ephemeral......................................................................................

Bore, well..............................................................................................................

Windpump.............................................................................................................

Mineral field boundary.........................................................................................

Major opencut.......................................................................................................

Prospect................................................................................................................

Iron..................................................................................................................

Manganese.....................................................................................................

Gravel..............................................................................................................

Hamersley Group

Fortescue Group

Greenstone

Ham

ersle

y Ba

sin

PILB

ARA

CRAT

ON

Quaternary alluvium, colluvium, lacustrine deposits, Cainozoic calcrete and siliceous caprock

Cainozoic hematite-goethite deposits and laterite

ROBE PISOLITE

Precambrian rock outcrop

SEA LEVEL

5 km

SEA LEVEL

5 km

DIAGRAMMATIC SECTION

A BNATURAL SCALE

22

65

682

72

6253

sc

65

Mineral field district boundary.............................................................................

SECOND EDITION 1996

10

Kilometres

SCALE 1:1Ý000ÝÝ000

0 20 30 40 50

10

Kilometres

SCALE 1:1Ý000ÝÝ000

0 20 30 40 50

Airfield, landing ground.......................................................................................

Abandoned, position doubtful.............................................................................

Dam, tank.............................................................................................................

Pool, spring, waterhole, soak.............................................................................

Locality..................................................................................................................

National park boundary.......................................................................................

Microwave repeater station.................................................................................

Sand dune............................................................................................................

Highway with national route marker..................................................................

Railway with siding..............................................................................................

Quarry....................................................................................................................

Mineral occurrence...............................................................................................

c.2690 Ma

Mou

nt B

ruce

Supe

rgro

up

Major fold, showing trend and plunge direction

plunge direction, and nature of vergence (Z, M, or S profile)

Metamorphic foliation, showing strike and dip

Intersection lineation, showing trend and plunge direction

Mine, abandoned..................................................................................................

Alluvial workings...................................................................................................

Cainozoic colluvium, alluvium, and sand over granitoid rock

Shaw Granitoid ComplexYule Granitoid ComplexKurrana Granitoid Complex

Alluvium_unconsolidated silt, sand, and gravel; in drainage channels and on adjacent floodplains

Eolian deposit_sand; in sheets and longitudinal dunesAlluvium and colluvium_red-brown sandy and clayey soil; on low slopes and sheetwash areas

Alluvium_partly consolidated silt, sand, and gravel; old alluvium dissected by present-day drainage

Brecciated siliceous caprock over dolomitic rock; angular chert fragments in a chert matrix; overlies WITTENOOM FORMATION

Colluvium_partly consolidated quartz and rock fragments in silt and sand matrix; old valley-fill deposits

Lateritic deposits_massive and pisolitic ferruginous duricrust

Dolerite dykes, sills, and small intrusions; numbers identify different suites, lowest number earliest

c.2500 Ma

Metabasaltic flows and breccia

intruded by a network of metamorphosed muscovite pegmatite veins

locally intruded by a network of metamorphosed muscovite pegmatite veinsMetamorphosed biotite monzogranite and minor granodiorite

Strongly foliated monzogranite

Banded iron-formation; locally jaspilitic

Massive serpentinite, and tremolite-chlorite schist

Prot

eroz

oic

Arch

aean

syncline, exposed..........................................................................................

Ophthalmia Fold Belt

inclined.....................................................................................................

Bedding, showing strike and dip

inclined...........................................................................................................

trend..........................................................................................................

interpreted from aerial photographs

inclined....................................................................................................

C-S fabric................................................................................................

Ophthalmia Fold Belt

C-S intersection; inclined..............................................................................

Stromatolite locality..............................................................................................

vertical................................................................................................

trend...................................................................................................

Sand over granitoid rock_quartzofeldspathic sand; includes areas of low, weathered outcrop

Medium- to coarse-grained metadolerite sills intruded into Hamersley Group

Medium- to coarse-grained metadolerite sills intruded into Fortescue Group

intruded by a network of metamorphosed muscovite pegmatite veins

Metamorphosed biotite monzogranite and minor granodiorite; weakly to strongly foliated; local metabasalt and metadolerite xenoliths

Quartzofeldspathic schist and quartz-chlorite schist

inclined.....................................................................................................

inclined...............................................................................................

Asbestos; crocidolite......................................................................................

anticline; exposed, concealed......................................................................

Lacustrine deposits_clay and silt; claypan (predominantly freshwater) deposits

Gemstones......................................................................................................

Dolerite dyke (various ages)

Pillowed and massive metabasaltic flows and metabasaltic breccia

Colluvium_unconsolidated quartz and rock fragments in soil; locally derived soil, and scree, and talus deposits

Pelite, metamorphosed mafic to intermediate volcanic sandstone, and chert; local accretionary lapilli and stromatolites

metadolerite; local accretionary lapilli and stromatolites

ROBE PISOLITE: pisolitic limonite deposits developed along river channels

BOOLGEEDA IRON FORMATION: fine-grained, finely laminated iron-formation; pelite and chert

WOONGARRA RHYOLITE: metamorphosed rhyolite, rhyodacite, rhyolitic breccia, and banded iron-formation

WEELI WOLLI FORMATION: banded iron-formation (commonly jaspilitic), pelite, and numerous metadolerite sills

BROCKMAN IRON FORMATION: banded iron-formation, chert, and pelite

MOUNT SYLVIA FORMATION: pelite, chert, and banded iron-formation

WITTENOOM FORMATION: thin- to medium-bedded metadolomite, dolomitic pelite, chert, and metamorphosed volcanic sandstone

MARRA MAMBA IRON FORMATION: chert, banded iron-formation, and pelite

JEERINAH FORMATION: pelite, chert, and thin-bedded metasandstone; intruded by metadolerite sills in the Hamersley Range

Woodiana Member: metamorphosed quartzitic sandstone, pelite, and chert (locally stromatolitic)

MADDINA BASALT: amygdaloidal metabasaltic flows and breccia

Kuruna Member: metamorphosed volcanic sandstone, pelite, chert, and metadolomite; local accretionary lapilli and stromatolites

Meentheena Member: metamorphosed stromatolitic limestone and dolomite, pelite, and volcanic sandstone

TUMBIANA FORMATION: metamorphosed mafic to intermediate volcanic sandstone, pelite, metabasaltic flows and breccia, chert, and

KYLENA BASALT: thin to very thick, massive or amygdaloidal metabasaltic flows; minor metabasaltic breccia and metasandstone

BAMBOO SPRINGS MONZOGRANITE: metamorphosed porphyritic biotite monzogranite; weakly to strongly foliated;

TAMBOURAH GRANODIORITE: metamorphosed medium- to coarse-grained biotite granodiorite and monzogranite; weakly to strongly foliated;

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118¾30À22¾00À

15À

30À

45À

23¾00À118¾30À 45À 119¾00À 15À 30À 45À

23¾00À120¾00À

45À

30À

15À

120¾00À22¾00À

45À30À15À119¾00À45À

Ham

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y Gro

upFo

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ue G

roup

AUSTRALIA 1:Ý250Ý000 GEOLOGICAL SERIES GEOLOGICAL SURVEY OF WESTERN AUSTRALIA SHEET SF 50-12REFERENCE

SYMBOLS

CAINOZOIC GEOLOGY

SHEET SF 50-12

c.

eolian sand, and mixed alluvium and colluvium

Mou

nt B

ruce

Sup

ergr

oup

This map is also available in digital form

East Perth, WA, 6004. Phone (09) 222 3459, Fax (09) 222 3444Mining Information Centre, Department of Minerals and Energy, 100 Plain Street,

Edited by D. Ferdinando and G. Loan

Cartography by P. Taylor

Published by the Geological Survey of Western Australia. Copies available from the

SIMPLIFIED GEOLOGY

Undivided Archaean granitoid rock

with modifications from geological field survey

1:250Ý000 Geological Series

Printed by Allwest Print, Western Australia

The recommended reference for this map is: THORNE, A. M., and TYLER, I. M., 1996,

Topography from the Department of Land Administration Sheet SF 50Ý-12

Roy Hill, W.A., Sheet SF 50Ý-12 (2nd edition): Western Australia Geological Survey,

Geological boundary, position uncertain

d dd

d

Ham

ersle

y Ba

sin

A

B

PILB

ARA

CRAT

ON

Com

plex

Kurra

naGr

anito

idYu

leGr

anito

id C

ompl

exSh

awGr

anito

id C

ompl

ex

Gran

ite_

gree

nsto

ne te

rrain

Geology by A.M. Thorne 1990-93, and I.M. Tyler 1985-86

ðHë

¦ Western Australia 1996

1

1

1

1

1

1

??

?

?

ñHs

GEOLO

G IC A L SURVEY

WE

ST

E R N A U S T RA

LIA

PIETRO GUJ

DIRECTOR, GEOLOGICAL SURVEY

OF WESTERN AUSTRALIAW.A.

N.T.

S.A.

N.S.W.

Vic.

Qld.

Tas.

A.C.T.

ROY HILL BALFOUR DOWNS RUDALLMOUNT BRUCEWYLOO

YARRALOOLA

DAMPIER

EDMUND

MOUNT PHILLIPS

ROEBOURNE PORT HEDLAND YARRIE ANKETELL

PYRAMID MARBLE BAR NULLAGINE PATTERSON RANGE

TUREE CREEK NEWMAN ROBERTSON GUNANYA

MOUNT EGERTON COLLIER BULLEN TRAINOR

SF 50-2 SF 50-3 SF 50-4 SF 51-1 SF 51-2

SF 50-6 SF 50-7 SF 50-8 SF 51-5 SF 51-6

SF 50-10 SF 50-11 SF 50-12 SF 51-9 SF 51-10

SF 50-14 SF 50-15 SF 50-16 SF 51-13 SF 51-14

SG 50-2 SG 50-3 SG 50-4 SG 51-1 SG 51-2

SHEET INDEX

+ means declination is east and correction must be

subtracted from compass bearing to give true bearing

Annual change is 1À easterly

- means declination is west and correction must be

The lines indicate magnetic declination, 1990

added to compass bearing to give true bearing

DEPARTMENT OF MINERALS AND ENERGY

HON. GEORGE CASH, J.P., M.L.C.

MINISTER FOR MINES

K.R. PERRY, DIRECTOR GENERAL

0 5 10 15 20 25 305000

Metres KilometresTRANSVERSE MERCATOR PROJECTION

SCALE 1:Ý250ÝÝ000

Grid lines indicate 20ÝÝ000 metre interval of the Australian Map Grid Zone 50