A Geological Survey of Western Newsletter January 2016 NUMBER 77

Geological Survey of

ISSN 1325-9377 ISBN (PRINT) 978-1-74168-660-9 Visit our Home Page at ISSN 1834-2272 ISBN (PDF) 978-1-74168-659-3

Round 12 Co-funded Exploration Drilling results

The government continues to support the quest for new resource discoveries across Western Australia through the latest round of the Exploration Incentive Scheme (EIS) Co-funded Exploration Drilling program.

The Minister for Mines and Petroleum, Bill Marmion, announced that 48 applicants were offered $5.17 million in Round 12 of the Co-funded Exploration Drilling program for projects to be drilled KUNUNURRA in 2016. Mr Marmion said the scheme was helping to underwrite Western Australia’s continued 30 17 prosperity. KIMBERLEY 27 29 ‘This is an important investment in the State’s future, particularly in the challenging financial environment faced by exploration companies. Heading into its eighth year, this highly competitive drilling program has resulted in major discoveries, with more being made every year,’ Mr Marmion said. PORT HEDLAND 4 KARRATHA 40 5 The successful projects are chosen via a transparent process 12 TELFER 11 which is subject to ongoing probity audits and ratified by a 33 committee representing all the peak resource industry bodies in Western Australia. continued on pages 2 and 3 22 21 41 20 36

GASCOYNE 48 13 18 24 MID-WEST 9 General 2 MEEKATHARRA 32 1 Agnew Gold Mining Company 27 Panoramic Resources 38 2 Anglo American - Traka Resources JV 28 Polar Metals Pty Ltd 15 3 3 Anglo American Exploration (Australia) 29 Prenti Exploration Pty Ltd 1 4 Antipa Minerals 30 Ram Resources Ltd 42 31 5 Antipa Minerals 31 Redcliffe Resources Ltd 39 LAVERTON 6 AusQuest Limited 32 Rox Resources Limited 37 7 Black Raven Mining 33 Rumble Resources Limited 35 8 Caravel Minerals Limited 34 Segue Resources Ltd 26 9 Cassini Resources Limited 35 St George Mining Limited 23 34 46 14 GOLDFIELDS-ESPERANCE 10 David Reed 36 Stirling Minerals Pty Ltd 10 47 11 Encounter Resources 37 Talisman Mining Ltd 8 16 25 19 43 38 Traka Resources Limited 7 12 Encounter Resources 45 13 Enterprise Metals Limited 39 Venus Metals Corporation WHEATBELT 28 Limited 14 Evolution Mining 44 15 Goldphyre Resources Limited 40 Warriedar Pty Ltd 6 16 Hanking Gold Mining Pty Ltd General 17 IronRinger (Killarney) Pty Ltd BUNBURY 18 Kalamazoo Resources Pty Ltd ESPERANCE Prospector Prospectors SOUTH GREAT 19 Kalgoorlie Consolidate d Gold Mines WEST SOUTHERN 20 Kalium Lakes Potash Pty Ltd 41 Anthony Stehn 0200km 21 Marindi Metals Pty Ltd 42 Brutus Constructions Pty Ltd 22 MRG Metals Ltd 43 Christopher Potts 23 Nexus Minerals 44 David Pascoe Figure 1. Location of projects 24 NiCul Minerals Limited 45 Ladislav Stanko 25 Northern Star Resources 46 Peter Kerley – Kalgoorlie Operations 47 Steven Kean 26 Orion Gold NL 48 Vanguard Exploration Ltd What’s inside? CO-FUNDED EXPLORATION DRILLING ...... 1,2,3 TECHNOLOGY UPDATE ...... 2 EVENTS ...... 4

PAGE AMADEUS BASIN ...... 5 PAGE PAGE 4 9 11 GEOLOGICAL MAP OF WESTERN AUSTRALIA ...... 6,7 3D GEOMODEL SERIES...... 8,9 FAREWELL ROGER HOCKING ...... 10 GEOPHYSICAL SURVEYS ...... 11 PERTH AND PEEL GREEN GROWTH PLAN ...... 11 PRODUCT RELEASES ...... 12 Technology update

ENS digital repository hosts all stratigraphic units

The Explanatory Notes System (ENS) is a digital repository that Reports are available in two formats (green boxes in figure): integrates stratigraphic relationships with links to all tectonic • Unit — for a single unit; colour-coding indicates whether the units and events recognized in Western Australia. It replaces description of the unit is complete (green tick) or only basic the previously published Explanatory Notes manuscripts that information is available (red tick) accompanied individual 1:100 000 and 1:250 000 series geological maps. The system allows incremental updates for new data • Overview — provides a stratigraphically sorted list of and refined interpretations, providing a seamless, up-to-date the selected unit/event and all its associated child units. summary of the geology of Western Australia. It is a virtual Overview reports are available as a table of contents or as Explanatory Notes for Western Australian geology. The best way fully expanded reports. to learn its capabilities is to have a play with ENS in GeoVIEW.WA Related units and events are hyperlinked, and further reports are – point-and-shoot or via icons and text searches. generated on the fly. Hyperlinks to Geological Survey of Western Australia publications are also provided. Explanatory Notes reports can be exported as PDF, or Microsoft Word and Excel documents.

ENS incorporates business rules that facilitate the sorting of rock units in a chronostratigraphic sequence. Spatial interrogation returns a list of rock units stratigraphically sorted (i.e. youngest at the top and oldest at the bottom) within individual tectonic units. Tectonic units themselves are ordered relative to each FigureFigure 1. GGeoVIEW.WAeoVIEW.WA interface for ENENSS other in a single framework for the State — thereby Explanatory Notes are written for providing the digital Lithostratigraphic units (both named and equivalent of the ‘geological’ column of a map legend. un-named), Tectonic units and Events, and are delivered via GeoVIEW.WA by a set of ENS search tools (yellow highlighted The Explanatory Notes information provided in GeoVIEW.WA box in figure). Spatial and textual query interfaces allow is updated weekly. Access GeoVIEW.WA on the Department of customers to produce geoscience reports by selecting a unit, a Mines and Petroleum website at generalized parameter (e.g. age, rank), or an area of interest (by . map name or rectangle; red boxes in figure). If a selected unit is represented in GeoVIEW.WA, the layer/s in which it is visible is/ For more information, contact are highlighted in a dedicated window (blue boxes in figure). Angela Riganti ([email protected]).

continued from page 1 and onto page 3

Significant success stories have included the Nova and applicants after completion of drilling and submission of Camelwood nickel deposits, the Yeneena copper deposits, reports which are released publically via the department’s Millenium zinc and the Dusk Til Dawn gold discovery. The WAMEX database after a six-month confidentiality period. Nova discovery, which was supported by co-funding in 2011–12, is currently in mine development stage with Round 12 of the EIS attracted 77 applications requesting production due to commence in 2016. $8.60 million in co-funding. The Economic Impact Study released earlier this year shows The minister said the Liberal National Government had that the EIS generates $10.3 million of exploration activity for committed a further $10 million a year to the EIS until the end every $1 million spent by the EIS, with the long-run expected of June 2017. total benefit to the State in terms of higher Gross State Product being $23.7 million. See for any updates on the The Co-funded Drilling Program refunds up to 50% of project. direct drilling costs with caps of $150 000 for a multi-hole project, $200 000 for a single deep hole, and $30 000 for For more information, contact a prospector’s project. Payments are made to successful Margaret Ellis ([email protected]).

2 Fieldnotes January 2016 Co-funded Exploration Drilling

Co-funded Exploration Drilling R12, 2016 Applicant name Drilling project title Target commodities 1 Agnew Gold Mining Company Agnew Stratigraphic Au 2 Anglo American – Traka Resources JV Musgraves Havarti Manyas La Serena project Ni, Cu, Pt, Au 3 Anglo American Exploration (Aus) West Musgraves Pepperjack and Rokpol project Ni, Cu, Pt, Au, 4 Antipa Minerals Rimfire Au,Cu, Ag, W 5 Antipa Minerals North Telfer – Minyari Prospect Au-Cu-W 6 AusQuest Ltd Balladonia Nickel–Copper Ni- Cu 7 Black Raven Mining BRM – SW Target Cu, Zn 8 Caravel Minerals Ltd Wongan Hills Cu, Au 9 Cassini Resources Ltd Babylon Prospect – West Musgrave Project Ni-Cu-PGE 10 David Reed Kalgoorlie Project Au 11 Encounter Resources BM7 and BM7 East Prospects Cu, Co 12 Encounter Resources Aria Prospect Cu, Au 13 Enterprise Metals Ltd Bono GEM Anomaly Au, Cu, Zn, Pb, Ag 14 Evolution Mining Broads Dam Stratigraphic Investigation Drill Hole Au 15 Goldphyre Resources Ltd Lake Wells Potash Deep Drilling Potash, gold, base metals 16 Hanking Gold Mining Pty Ltd Copperhead Magnetic Targets Au 17 IronRinger (Killarney) Pty Ltd Killarney 3 Cu, Au, Graphite 18 Kalamazoo Resources Pty Ltd Cork Tree Copper Project Cu 19 Kalgoorlie Consolidated Gold Mines Central Corridor Au 20 Kalium Lakes Potash Pty Ltd Lake Sunshine Test Bores K, Mg 21 Marindi Metals Pty Ltd Cu, Pb, Zn, Ag, Au 22 MRG Metals Ltd Xanadu – Pertinax Deep Hole Au 23 Nexus Minerals Pinnacles Project Au Jameson PGE Drilling, Spinifex Range Project, 24 NiCul Minerals Ltd Pt, Pd, Au, Cu West Musgrave Province 25 Northern Star Resources – Kal Ops Star Trek Seismic Reflector Au 26 Orion Gold NL Plumridge East Gravity Targets Ni, Cu, PGE Deep Diamond Drilling and Dhem, Dave Hill Eastern 27 Panoramic Resources Ni, Cu, Co, PGEs Kimberley 28 Polar Metals Pty Ltd Polar Bear Project, Nanook Gold Prospect Au 29 Prenti Exploration Pty Ltd Mad Gap Yards Diamond 30 Ram Resources Ltd West Kimberley Nickel Ni, Cu, Co, PGE 31 Redcliffe Resources Ltd Deep Drilling Programme Au 32 Rox Resources Ltd Fisher East, Musket Ni 33 Rumble Resources Ltd Beadell Project Kaos and 99 IP and EM Prospects Cu, Zn, Pb, Ag 34 Segue Resources Ltd Salt Creek Complex Characterization and Prospectivity Ni, Cu, PGE, Cr 35 St George Mining Ltd Ascalon gold target Au 36 Stirling Minerals Pty Ltd Oldham Range Project Ni, Cu, Zn 37 Talisman Mining Ltd Sinclair Nickel Project – Schmitz Well South Ni, 38 Traka Resources Ltd South Hill Area (Block 12 Spectrem survey area) Cu, Ni, PGE 39 Venus Metals Corp Ltd Inky South EM Copper Targets Cu, Zn & Precious Metals 40 Warriedar Pty Ltd Duke Halloysite Project Halloysite 41 Anthony Stehn Two Peaks Drilling Proposal Au Ag Pb Cu 42 Brutus Constructions Pty Ltd Bottle Well Nickel Prospect Ni 43 Christopher Potts Lurgan Project Au 44 David Pascoe Waverley Au 45 Ladislav Stanko Stanko’s Reward Au, Ni 46 Peter Kerley Never Can Tell Au 47 Steven Kean Turnpike Au 48 Vanguard Exploration Ltd Fairbairn Copper Project Cu, Au Figure 2. List of successful applicants Fieldnotes January 2016 3 Browse Basin

GSWA in the Browse Basin GSWA database training — dates for 2016

The gas discovery well for the Torosa field in the Browse Basin, Find out how to access data online and understand our systems including: Scott Reef 1, intersected a thick sequence of gas-bearing reservoirs within the Lower–Middle Jurassic sandstones of the • WAMEX Plover Formation. Eight appraisal wells were drilled to further • GeoVIEW.WA delineate the extent of the field, leading to an estimation of P50 • GeoMap.WA reserves at 11.5 TCF gas and 121 MMbbls condensate. • Data and Software Centre A satellite sweep of Australia’s territorial seas in May 2014 • Mineral drillholes and geochemistry databases detected a number of small rocks exposed on the Scott Reef • Department of Mines and Petroleum new and due to Cyclone Fay’s strike in 2004. The rocks prompted the improved website redrawing of maritime boundaries between Western Australia and Commonwealth Waters and a re-assessment of reservoirs PERTH in this area. Mineral House, 100 Plain Street, East Perth Thursday 3 March An independent seismic interpretation of four reservoir Thursday 9 June horizons and the fault network by the Geological Survey Thursday 27 October of Western Australia’s (GSWA) Basins and Energy section KALGOORLIE allowed the reservoir distribution to be evaluated by the Central campus of the Goldfields Institute of Technology, Petroleum Division. The Department of Mines and Petroleum’s 34 Cheetham Street, Kalgoorlie independent evaluation proved to be similar to that of the Thursday 10 March company responsible for the tenements, therefore assuring a Thursday 16 June high level of agreement in the allocation of petroleum between Thursday 3 November the Commonwealth (34.6%) and the State of Western Australia (65.4%). Sign up now for FREE training!

For more information, contact See the Department of Mines and Petroleum website for more Alex Zhan ([email protected]) or details and to register at . Charmaine Thomas ([email protected]).

Figure 1. Seismic section across Torosa 1 in the Browse Basin, showing GSWA’s interpretation of reservoir horizons and fault network

4 Fieldnotes January 2016 Amadeus Basin

Gravity and magnetic study of the western Amadeus Basin Recently released Geological Survey of Western Australia (GSWA) Report 154 by C Foss and others, provides a geophysical study of the western Amadeus Basin using all available gravity and magnetic a) datasets. It was carried out by CSIRO as part of the broader scale COBRA (Central Oz Basins Resources Kiwirrkurra Assessment) project; a collaboration between CSIRO, Government Geological Surveys, and industry partners. This component of the project was funded by the Kintore Exploration Incentive Scheme (EIS).

The western Amadeus Basin, situated between the 24°

inferred edge of Arunta (north) and Musgrave (south) basement Amadeus Basin regions, and onlapped by the Canning Basin from the Kaltukatjara west (Fig. 1a), is a barely explored frontier area for (Docker River) petroleum and mineral resources. The basin as a whole b and c Warakurna is of early Neoproterozoic to late Paleozoic age, and contains oil and gas fields with Ordovician and late Neoproterozoic reservoirs in the Northern Territory. The NT Western Australian end of the basin, predominantly of 26° Neoproterozoic age, is poorly exposed and currently Warburton SA

126° 128° WA 130° lacks seismic data or deep drilling, so an understanding of basin thickness and large-scale structure must be Gunbarrel Basin Murraba Basin Arunta region derived mainly from modelling of potential field data. Canning Basin Ngalia Basin Roads Community The magnetic field data clearly delineates the structural Amadeus Basin Officer Basin 100 km basin margin, even when concealed beneath onlapping Clutterbuck Inlier Musgrave region Canning Basin strata. Sparse magnetic field anomalies allow estimates of depth-to-magnetic basement, which b) Kiwirrkurra –1000 -5000 -3000 are often in excess of 10 km. Because such depths are -3000 23° -3500 considered improbable from known Amadeus Basin -3500 Kintore –3000 stratigraphy alone, they are inferred to locally include a magnetically transparent pre-Amadeus sedimentary or metasedimentary package. The basin model is derived –4000 primarily from gravity data. The thickest Amadeus -3500 -4000 -6000 section is modelled to exceed 8 km in the far east -5000 24° -4500 of the study area (Fig. 1b). Sedimentary strata thin -4000 -3500 –5000 -3000 towards the west with less than 3 km (mainly Canning -6500 Basin) overlying a broad north–south basement ridge -4000 –6000 -3500 considered to define the western edge of the Amadeus -8000 -3500 Basin. The integration of gravity and magnetic -7500 Kaltukatjara –9500 modelling allows the mapping of the pre-Amadeus (Docker River)

25° Amadeus and Canning basins (m) base Depth to package beneath the southern part of the Amadeus 127° 128° Warakurna 129° 50 km Basin (combined with the Amadeus section in Fig. 1c). Kiwirrkurra c) -5000 –2000 GSWA Report 154 COBRA — Amadeus Basin project: -3000 23° –3000

gravity and magnetic study of the western Amadeus -3000 Kintore -3500 Basin, Western Australia is available as a free –4000 downloadable PDF from -5000 . -6000 –5000

-4000 -10500

For more information, contact -9000 24° –6000 Peter Haines ([email protected]). -7000 –7000

Figure 1 a) Simplified bedrock geology of the study area; -10000 –8000 b) modelled thickness of Amadeus and onlapping Canning Basin -9500 -4000 -8000 strata, with magnetically defined Amadeus Basin western structural -7500 –9000

-7000 -7500 edge indicated by the red dashed line; and c) modelled depth to –10000 crystalline basement, which includes a pre-Amadeus sedimentary or Kaltukatjara –12000 metasedimentary package beneath the southern Amadeus Basin -5500 (Docker River) 25° (m) pre-Amadeus basement including Depth to 127° 128° Warakurna 129° 50 km

Fieldnotes January 2016 5 Geological map of Western Australia

The State Map, 2015 – it’s how we roll

1 The 14th edition of the Geological Map of Western Australia across tectonic unit boundaries (as in the Neoproterozoic

(Fig. 1) was released on 17 December 2015. It is the first Centralian Superbasin) are taken into account. For the first timeme 15° release since 1998 of a flagship Geological Survey of Western since 1988, dykes across the State have been re-compiled, andand Australia (GSWA) map that has been produced on average in the associated digital layer have attributes that reveal the 16° about every eight years since 1894. This map is the culmination various dyke suites, swarms, and ages where known. of 15 years of work that has profoundly reshaped how GSWA delivers geoscience data and products. The map is the first to The printed map may appear little different in most places 17° be compiled entirely by digital means, with spatial accuracy from its 1998 predecessor, other than a far denser depiction inherited from and reflecting larger scale spatially accurate of dykes across the State, and substantial changes where 18° geological mapping, rather than compiled by hand from pre- mapping has taken place since 1998. However, there is now an existing maps and then digitized and manipulated to produce accompanying set of spatially accurate digital layers that are 19° the final product. The map and associated 1:2 500 000 digital slightly more detailed than the printed map. These layers consistnsist layers were produced by rolling up 1:500 000 digital layers, of the primary 1:2 500 000 State interpreted bedrock geology,y, 20° which in turn were produced by rolling up 1:100 000 digital data the 1:2 500 000 State Cenozoic geology, the 1:2 500 000 Stateate now available over much of the State. The map thus inherits interpreted dyke suites, and the 1:2 500 000 State interpretedd 21° 1:500 000 scale spatial accuracy across Western Australia. bedrock linear structures layer. These can be interrogated onlinenline via GSWA’s free GeoVIEW.WA interface, or via a users’ ArcMap-ap- The first step towards smart, spatially accurate Statewide or MapInfo-compatible GIS system. A wealth of underlying 22° geology was made in 2001, when a digital 1:500 000 seamless attributes is then revealed — the geology is smart, rather thanan a interpreted bedrock geology (IBG) layer was compiled, primarily simple two-dimensional map. 23° from extant 1:250 000 maps. The two compilers, Vanderhor and 23°26'30" Tropic of C

Flint, had to work at an average rate of one 1:250 000 sheet per Some of the more noticeable changes to the printed map aree in 24°

Cape

Qu Point Q day to complete the job. This was then used to generate a new, the marginalia. The accompanying tectonic units map is noww GEOGRAPHEQUOB

reproduced at 1:10 000 000, and is considerably more detaileded BERNIER ISLAND detailed 1:500 000 map of tectonic units of Western Australia, 25° Ôk DORRE ISLAND

than the 1998 version, having been rolled up and simplified NATURALISTE CHANNEL by Tyler and Hocking. The IBG and Tectonic Units layers were Cape Inscription Cape Levillain

DIRK HARTOG ISLAND DENHA

Quoin Head SOUN revised incrementally but slowly, and a new Tectonic Units from the 1:500 000 geology. The legend is constructed usingg Ôk 26° SH South Passage Dirk

Steep Point version was released in 2007. Small amendments have continued similar principles to 1998 but has also been totally redesigneded Thunder Bay Zuytdorp Point Car to be made since then on the tectonic units and the 1:500 000 (see excerpt below) with a modified grouping of the 100 million-ion-

27°

2000 m geology, but the big advances since 2001 were in developing year time slices used in the coding of the Precambrian, 3000 m the back end to the digital process. This came to fruition in 2014 presentation of Phanerozoic and Precambrian units in a singlele with the release of fully re-interpreted and re-compiled 1:500 000 stratigraphic column, the depiction of known age ranges for 28° geology and tectonic unit layers. all units, and the inclusion for the first time of major orogenicc

and tectonic events. 29° The roll up process for the 1:2 500 000 layers consists of selectively merging 1:500 000 spatial units according to In future, annual or semi-annual updates to the 1:500 000 30° definitions held in the recently released Explanatory Notes and 1:2 500 000 digital datasets will mean that the State

System (ENS), while preserving polygon boundaries and geology remains current, and will prevent the long delays in 5000 m relationships wherever possible. Lithostratigraphic units are the release of this data that have been experienced 31° depicted at subgroup or suite level, or higher, and correlations in the past.

32° I N D I A

7b O C E A N

33° 1500

Edmund Group Scorpion Group sandstone, siltstone, B1 Sc sandstone, siltstone, mudstone, g7 7a mudstone, dolomite, chert dolomite, chert Yapungku PROTEROZOIC 34° 1600 1600

Bresnahan Group Liebig conglomerate, sandstone, Bh f6 Mount Barren Group 6e siltstone, mudstone phyllite, pelite, psammite, metasandstone

Mangaroon 35° Crowhurst, Bastion and Argilke Mount Minnie Group Mm Mb Zanthus 1700 sandstone, conglomerate, siltstone Cb Birrindudu Group

siltstone, shale, dolomite, Biranup sandstone, conglomerate Capricorn Group Miningarra Group n6 Strangways 6d Kimberley Group sandstone, shale, conglomerate, dolomite sandstone, siltstone, Ngadju sandstone, siltstone, Yambah K2 limestone 36° dolomite C Wyloo Group s6 b6 d6 g6 1800 sandstone, shale, shale, sandstone, K1 Wy Mn Capricorn Stafford basalt, dolomite conglomerate 112° Speewah Group 113° Sp Hc Tanami Group 6c sandstone, siltstone, shale Ta metasandstone, 6 Tanami Halls Creek Halls Halls Creek metasiltstone, Hooper Salmon Gums Padbury Group Group metabasalt f6 1900 sandstone, siltstone,BIF, GIF, Pa pelite, psammite, conglomerate, dolomite Tooloo Group Bryah Group metabasalt Br2 To siltstone, sandstone, 6b sandstone, siltstone, BIF GIF, dolomite Mooloogool Group basalt, sandstone, siltstone Br1 Mo sandstone, basalt, shale 2000 Glenburgh

d6 6a

2100 PALEOPROTEROZOIC Legend detail showing enhanced age ranges, ranges revisedreevised stratigraphic subdivision and coding, and new depiction of orogenies and tectonic events

6 Fieldnotes January 2016 Geological map of Western Australia

114° 115° 116° 12° 117° 118° 119° 120° 121° 122° I N D I A N 123° O C E A N 124° 125° Ashmor 126° West I e Reef East I Middle I 127° 128° 13° 129° GEOLOGICAL MAP MAIN TECTONIC UNITS OF 12° WESTERN AUSTRALIA Age (Ma) 0 CENOZOIC T I M O R S E A MESOZOIC PALEOZOIC PHANEROZOIC OF 1000 NEOPROTEROZOIC SOUTHERN BONAPARTE NORTHERN MESOPROTEROZOIC BASIN BONAPARTE 2000 BASIN

Sedimentary and volcanic rocks

14° PALEOPROTEROZOIC BASTION KIMBERLEY metamorphic rocks BASIN

Igneous, sedimentary and BASIN WESTERN AUSTRALIA CAR SP R 3000 EEWAH BOYD BASIN BASIN BASTION Igneous and metamorphic rocks BASIN KING LOUISA VICTORIA 13° ARCHEAN BASIN BASIN

Granite–greenstones LAMBO AND Holothuria Reef 4000 LE WOLFE OROGEN O SPEEWAH OSMOND BASIN OPOLD OROGENPRO BASIN BASIN RED ROCK VI NCE AND Otway Bank TEXAS DOWNS Compiled by Martin, DMcB and Hocking, RM 2015. ORD BASINS

Derived from Martin, DMcB, Hocking, RM, Riganti, A and Tyler, IM 2015, BASIN Y Tait Bank Scott Reef 1:500 000 Tectonic units of onshore Western Australia, 2015: R

5000 m 5000 Browse I 4000 m 4000 Cape Londonderry Parry Harbour SIR GRAHAM Cape Geological Survey of Western Australia Long Reef LAMBOO PROVINCE ITO Troughton Passage MOORE Is Talbot Patterns represent the extent of major orogens. LOUISA BASIN WOLFE 2015 K1 Eclips BASI R Jamieson Reef e Is N ROEBUCK HALLS CREEK Oyster Rock Mary I K1 View detailed data at . BASIN WOLFE Ingram Reef Pa K1 BASIN d6d ssage Vansittart Cape Rulhieres TER NAPIER d6d Montesquieu Is Yankawinga I Bay BIRRINDUDU BROOME

Albert Reef K1 BAS 3000 m 3000 Kingsmill Is BAY IN

West Montalivet I K1 East Montalivet I d6d PILBARA GRANITES– Maret MURRABA Is Cone Mountain Prudhoe Is K CRATON BASIN TANAMI 1 Robroy Reef S

K 1 RIVER NORTHERN

MONTAGUE N CANNING BASIN 2000 m 2000 I Turbin I ADMIRALTY Kalumbur CARNARVON OROGEN SOUND u A FORTESCUE BASIN d6 L 14° MONTAGUE SOUND GULF d DRYSDALE–LONDONDERRYP BASIN

JOSEPH BONAPARTE N K1 MARBLE BAR BIGGE I Warr C PATERSON K ender Hill arson N SUB–BASIN 1 O SE R ER RIVER iver T P Mt Connor PEL GULF YENEENA T Reveley I LAWLEY RIVER Mt Connelly BAR R BASIN TH GEORGE A A R C H I P E L A G O N Lamarck I G R K1 d E Buckle Head HAMERS 6d MITCHELL LEY MURRABA MITCHELL O S H E L F RIVER BASIN PLATEAU K1 MEDUSA BANKS BASIN K1 Kartja I KING Kin EDM N

C g Shoals UND 1000 m 1000 RUDALL YORK SOUND d6d O BASIN FORTESCUE CORONATION d6 LL PROVINCE IS d ISO ASHBURTON BASIN AILERON Mt Anderson EDWARD N Medusa Banks BASIN OROGEN Theda R Mt Nicholls PROVINCE A B O N A P A R T E N BRESNAHAN G Cape Dussejour SYLVANIA d6d E CAPRICORNBASIN INLIER OFFICER BASIN AMADEUS BRUNSWICK K2 Lacrosse I Beagle Reef Champagny Is K2 RIVER BASIN Darcy I BAY M WARUMPI Dingo Reef RIVER t Burns K DRYSDALE E 1 RIVER CAMBRIDGE PROVINCE K2 d6 G SOUTHERN AUGUSTUS I d N BERKELEY GULF Ôk COLLI

Churchill Reef HEYWOOD IS A CARNARVON COLLIER ER

Ad Mavis Reef PR R Mt M PROVINCE EDMUND BASIN 200 m 200 ele I K1 d ongona SCORP AMADEUS MacD 6d E ION ONALD ANG CARSON BASIN BASIN BASIN K2 I K1 AN R OROGEN BASIN BASIN K2 N MO OUCHM N Utting Gap St George CE C E O RANGE G T FORREST RAN RIVER KING AN N R H d6d ER I SALVATION Albert Reef CAMDEN SOUND Basin S S R NG S FOST RIVER êés Adele Island Shoal PRINCE REGENT – CAMDEN SOUND A A 15° BASIN GUNBARREL BASIN 0 M Doon N BI CARRANDIBBY gan G Deceptio d6d AY N n Bay Mt E INLIER SCALE 1 M Batten K2 G Ó MARYMIA INLIER 100 : 2 500 000 Hall P t King d6d Cb Mt Co s Frost Shoal oint R nnection çs NARRYER PRINCE REGENT RIVERA 200 Nicolle Reef N MILLIGAN TERRANE GOODIN G ASHTON Ningbing INLIER Tasmanian Shoal K2 ES RANGES çk PADBURY EARAHEEDY 300 AND YERRIDA BASIN Kilometres ND Ôk êés æz BADGERADDA MONTGOMERY IS H A GE Null êb BRYAH BASINS BASIN PATERSON ALB 400 K2 ET N a Nulla Wyndham ERS EQUAL AR K A R C H I P E L A G O MacLeay I B RA Drysdale Durack BASIN EA PROJEC Caffarelli I 1 LIZA INE River River êé OROGEN TION WI Bathurst I Ô E R MAI K2 s êb TH CENTRAL M k E CAMBRIDGE GULF MUSGRAVE PROVIN HOR ERIDIAN 121°0 K2 d6d TH Carlto PINJARRA OROGEN CE IZONTAL DA 0' AND STAN Cockatoo I CA T ORD n Hill OFFICER TUM: GE DARD PA Pantij d6d L OCENTR RALLE an A E RIVER IC DAT LS 17°3 Yampi Sound R Cg BASIN UM OF AU 0' AND 31°3 KOOLAN I Doubtful d6 ND STRALIA 199 0' B U C C A N E E R K1 d Hom S êb 4 (GDA 94) KINGFISHER IS K1 G e Valley C Cb KING K K A R O I K1 K 1 K2 Bay R D N N Kim Sunday Strait 2 K2 E R A C Cb berley Eagle Point P R K E K1 L A T N A Re Strickland Bay E A RIVER PENTECOST B R search U G COLLIER BAY N U AN K2 Ivanh C E RIVER E G R oe Station g A R Cape Leveque 6d GE G E N G Sp çk G RIVER N R êb Mt Septimus eology Sunday Traverse I O N ROAD E by Geologic I K1 g6d K1 GE RA L GIBB – WYNDHAM A d6d Nullywah Mt Cecil al Surve RAN INE R NORTHAMPTON y of Western K2 Secure K2 ING CHARNLEY d6d çs Miri Compil Australia PENDER K2 ARD S Ellenbr ST êés ma çs INLIER ed by DM Bardi Cone Bay K2 H d ae O K æåe cB Martin Lomba One Ar Bay 6d CALDER IN R C UNUNURR , RM Hoc Lombadina Pointdina Djarindjin m Point K HANN A E êés A In kin N G s formation de g, A Rigan Skeleton Point g6c s6 ED G T êb K1 6c rived f ti, and c Walcott Inlet Edward Peak RIVER I ROYST N rom I ES GIBB B O El published M Tyler K1 M N E Questro Sheba OFFICER a B

nd unpublish Cygnet cLARTY Ôk RANG P Hill CANNING BASIN

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H I P E L Pardoo Óv MOUNT BANNERMANMt Bannerman BAINES H G e intrusions ...... drainage, ina ...... ILLS ARDNER RANGE (lamproite, lam ctive or rarely a A R C Geographe Shoals De Grey Ós prophyre, ctive...... Ôk P Sturt kimberlite ...... Ôk ORT HEDLAN Mt Morris , carbonatite)..... Bathymetric c ...... MONTEBELLO IS Legendre I Cape Thouin D ã Lake McLernon ...... ontour...... Beagle Ree S ORD s I ...... DA f g3b OUTH D C ål çs Cn mpact structu ...... MPIER AND Rosemary I g3 RANGES ASE Billiluna re...... BARROW ISLAND Ôk Delambre I HE b G Mt Erskine ...... 100 g4a Booda DLAND oldsworthy âs Clapp Ridge Y Mindibungu BILLILUNA ...... 0 m d4a Cape Co rie RA BRAM Dia ...... ssigny SHAW ALL pir...... ás æå NG TANAMI ...... Wolfe 1 : 25 E R g4a F ROEBOURNE g3b g3b Strelley e Lake Doman E HILLS Tent Hill ...... Creek 0 000 geologic 3 R g ..... al m M P I g P DE GREY 3b Cb ...... ap sheet...... Cape Dupuy g3b g4a 3b Cape Lambe Ronsard Pippin G s6d ...... Lowendal Is D A Eagle Nickol F1 rt I garra Mulyie R E A g6c g6d Larranganni Bluff ...... Ilma ...... hawk I DAMP Poi Ô g3c g2a Sh Óv T KURA Diapir ...... 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h West Cape Ói G E P g3a g2b g3c na Downs F3 æåe ås r Bluff B PHI Lake Jeavons k üs RIVER L 56 Ma Vlamingh Head Y Mumbillina Bluf D E ås rine and coa Point Mm alleen g2c f Wood d2c g1d g3c NULLAGINE F5 L Paleoce stal sandston Murat Urala Ói stock g3c d2 G Ós AN ne úk e Jurabi Point MUNGAR F2 c P g2a REG L F5 OONA RIVER BL DS imesto P g3b ACK g2a F1 g2a Kaliranu Hill Cn1 66 ne, marl, basal g Peedamulla F4 RANGE RANGE d2c F F1 P T reensand O ATER E R R I T O EX Ói H1 F3 g1d g3b 2 SON RANGE A N A M I MOUTH Mt F g3c RY Yam Hill lorance Hillside Cn1 g8 þz Ôk Ói Ói COCKERAGA R g2b S c g8 Min Coola g3c êd c der Mt wa Ò oo Minnie nyah g3c STOCK ä z g ål s Ò 3b g6c Cn z WESTB1 Hoole d2c 1 Ós T ák Con Ói Óv y å ål tinen F2 R s æåe D E S tal siliciclastic ro g3 g N A P Lake Guli E c EXMOUT ASHBURTON Red Hill Mt Margaret b 3c F u F5 g4 Mt Crofton SAHARA Farewell Lakes R T ks of unce H s3b 2 N a A rtain age; pre T s Mm P S D G Telfer Ó ák umed Cen 50 H g1d g E s ozoic Cane Riv 2b E Marin or Mes er M A Silver Grass Peak R WI æåe e limesto ozoic m Nul F5 F2 R S ne, m RANGE M lagine S LK PERCIVA 21° Cre arl and GULF s6c g RIVER A L LAKES Point T tace green 3c O N æåe ous sand; Rundle Hill E Ói I A ERIC calcareo L N G A us earmonth RIVER H2 F4 F3 PERCIVAL Moody NS Lake White pelag R F3 Mt Ma E Ós ic dep cPher osits Ningaloo Reef Ói SHAW g son P Mt Delp S F4 2c g2 RANG Ói hine Ó c MO ES L i C R ARRY RANG Ói g3b g F1 ál Point Lefroy H 3b B C Koordarr E I 2 A ie RE Úk g6d Sh Y Mulg C Lookout Rocks NG Óv a Down H WESTERN Ó g3c Wy s i Ói F3 å Ó E ål l OI Mt Farquhar i B Ex S 2 E mout Mt B roc Mt Jack HELENA Lake Wills h Gul kma T Tobin Lake f s6c n êd ál H E R g Mt Maggie R þz Marine to c d4 ame Bon 2c DAVIS AN oa PE YANREY– a F5 F5 rsley ney Dow H1 å stal siltston NING NORTH R Mt Sylvia ns êd s s6e þz e, shale E þ C Si , an ALOO Óv ás F4 F3 F5 Óv G z liciclas d radi H æ I ti o CA Mt Mu A 1 R H åe Mt Isdell c rock larian

1 OAKOVER áb s si rray A æåe E Warri Cree , easte ltstone ESOZ r N First Hill N CANNING k n Canning Ba Yanrey g6d Mt Stuart WYLOO G Red Hill G B2 Lake Ós ål ål 145 sin; presumed RI E E Cape Warton Coolbro Creek STANSMORE Ó M áb Mesozo VER d v M ZO C ic Ós Nanutarra Road Tc 4a Mt MacLeod Ói Noree THROSS URRABA ontinental ba Na house F2 Duck Cr Mt Brockman d4a na Downs ELL Dora ás salt, southern nuta eek FORTESCUE RANGES äs O Perth YANNARIE rra F3 F5 Basin Ningaloo b3a T MOUNT BRUCE Mt Stevenson F5 æåe RANGE Lake Auld Ó Jura âs South c v R s e Ói F F4 sic ás rn margin Point Giralia g6d Boolaloo F4 g3c Auski Roa d2b 4 êd þz Conti breakup Cloates Ós F1 F5 F5 Mt De La Hunty dhouse E nental to Bullara ROY HILL Rat Hill B Yap coastal sa Mt McGrath Mt s6d R ås paru âs ndstone Ói Divid Mt Russell N Con and c 100 H2 BALFOUR DOWNS e O Claypan âz tinental sandsto onglomerate HENRY F3 Ói RIVER Cn1 R A ne, le W Mt Bruce A sse Uaroo yloo TOM Dinne D r siltsto Mt Clement H2 PRICE r Hill H1 s2b s2b A G R Carneg ne and c H ie Bluf 2 oa N E A f 01 l mea Ôk F3 B T H sur s2 Mt Hyogo 2 UR es a G Tc d4a Mt Wi Marillana RIVER S A Cn âz s6c H ndell Boorabee Hill E Cn1 N Co Chabjuwardoo ük F5 1 F b2a Ói Roy s6d D Y P ntinen 2 Ói Hill F3 n6d S D tal and marin ál B1 s2a Mt Lewin F5 T E S Tri e sandst Bay H2 g2b H2 Kunawarritji Cam E R T s6 assic ãs one, siltstone, s T Ói êd RUDALLn6d p N hale, and So Marrilla Kooline HARDEY c H1 F5 s6d Lake Blanche limestone We uthern Nort g6d Wy g6 Sh F1 Ói F3 WILSON CLIFFS äs stern margin h Wy d Rocklea Juna Dow H1 Óv West úk Glen Flor Mt Barricade ns g B2 Redknap ãs C Shelf break C ál s6c rie Mt Jope 3c Mound ãl ontinental a breakup up ardabia Nyang RIVER RIVER TABLETOP 252 nd coasta s6d d4a F5 F2 g2b Óv Cn4 åz l sandstone, m Coral Bay ák g6e g6d êd SAL ãl inor siltstone F2 Mt Meharry Balfour Marine to Damp g6d d4a Mt Trevar F5 F4 TB Lake George 22° Permian coastal sha ier–Barro Winning B1 F3 ton Ethel Downs RAN US g7a ás le, minor lim w rift ons FITZGERALD F2 G H s6d URAL äs åc estone et GIRALIA RANGE g6d Tow RANGE W Creek E s6 s6c åc San era IL êd e dstone, ca ü g6e L F3 Ói H H2 ås g6d ål rbonaceous 200 k IA F1 A d4a F æåe Ós åz shale, coal, p RIVER s6c W M M F5 3 g3c ås E R Contin ebble con s6c y g6 R E WE Suffic 299 ental and glomerate F e A R b6d n6 ål iency Knob marine sa itzroy Mo N S êd R d s6e ål ndstone an vement LYNDON B1 G Wy PA Sh Padtherung Hill Hickman Cn3 A LL ås Marine a d siltston d7b E H2 RABURDOO L N S n6d g6 nd lesser c e, minor lim Capricorn Mia Mia Mt Palgrave C E G b6d æåe WILSON g6d d ontinental s estone çs g6e Wy Y F H E Cn3 Mc s6c æåe ås iltstone, sha g6 Winning Hill d7b 5 2 K æåe Carbonife Contin le and sands Warroora e Ash OPH AY s6c rous ental and coa tone WINNING POOL – MINILYA s6d burton Tc THALMI W R s6d Ós g stal sandst d7b D R A RAN H1 alagunya AN 6d one, siltston s6c owns Mt Channar A GE GE ål æåe Con e, and coal me Maroonah Ulla H2 N G Mt Newman Mt Newm Cn4 LAKE MacKAY æz tinental and m asures úk RIVER warra CAP E an WEBB arine glacially in Perth Cape Farquhar g6e s6d Carinna Hill EDMUND F5 H1 E s6c fluenced silic Basin Permi H H1 C icla a Moogooloo Hill H B RICO C 1 G g7 359 çæl æz stic depo n rifting GOOCH RANGE a s I A d7b b2a NEWMAN Cn3 Óv Marine a its, minor ås æåe GH R B TUREE CREEK H2 N g6d nd continenta limestone ål d7a 2 OI l sa ák g6d Ly LE R A ndstone, s ndon N Mt Elephant F5 R g6 iltstone, Úk E H2 Capri Veevers æåe Cn4 d shale; 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b4a ne, 190900 en a ERE Warradarge Hill Wonjan Óv Riverina b4a dleyarri LAKE MINIGWAL æåe Mooloooogoolool G GIIFF, dolomite d7 T r G R Menz RAESIDE d Carlisle Lakes oupup reen He GAIRDNE g4a g4b ies LAKE ad SC E n3c LAKE MINIGWAL Shell Lakes sandston Marchage D 29° OTO e, basa Mo R e l s4b MARMION t,t, sha h Green Lake J Lake Ilma lele A Pinjarrega Lake H GREAT Lake Goorly g4b UD g6e Gwynne Creek æåe R g NGE DI r ãs EL COONDEROO b3b E HARD g4a Mc Y I PLUMRIDGE P W b4a N u 6 Mt Lesueur ubin RANGE b4 A b a b Ó O R R g4a v g4 Plumridge Lakes Ilma Diapir b4a Menan Ya s4b g4 n g4 gi b EOPRE A Remla b na boo R p e Jurien Bay s A Yabboo Hill âs N 4a l Mt BeniaRIVER g4b Hill L N b4a Cn JU GE G JUBILEE 1 RIE D GGl N BAY HILL Lake De Courcy g4 avyhurst n3c A Dalwallinu Lake E Lake Colville Forrest Lakes Wathe PAP roo g Mt J f4a g4 Lake 2000 Bad 4 ackson g4b Owen Goongarrie gingarra Lake Harvey RA HUN Wangine d4b Ó Ronsard Bay s4a s4b Ós ROAD v d6 MOORA Pitha Kalannie Kawana NG Lake s4b b4a d7d 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n WONGAN C p RIVER g redo 210100 2000 m RANGE 4a d sandstotone DLE HILLS g4b 4b Yin , s 200 m OO Bro di iltststotone Wi 1000 m DIW Blac ad Arrow SUE , shal KOO Lake Hinds k Úk e RANGE KALGOORLIE Flag Sh Shhingleing K le n Piawanning anowna KURNALPI Creek Groupoup Bidgerabbie Hill Ca a doux b4a E d4 basalt,t, s i b Be nnuin g4 Mt Finnerty s4a b f4 sandstonone, silts 3b ncubbin b4a s4b b tone, c mmi Koorda n4a s4 onglo l 5d Seven Sisters g4b f4b b Ku meratr te s3 g4b rnalpi a RIVER b Wongan Hill b4 d7d s s4b a g6 h Cowcowing e t Koolyanobbing KALGOOR s4b Mt Hunt CUNDEELEE Lancelin Lakes Mukinbudin Lake Baladjie Timberf LIE–BOU f4b Turee Cree h MOORE b3b ield LDER Lake Roe Tc k Group Lake g4 Hampton H 30° mudston Ledge g4a g4b ill LAKE Lake Yindana e, silts s Op Point d3b Óv Wallambin Lake Walton f4b n6e tone, sandsto 5 2200 B Calingiri n3 Lake Mt Burges YINDARLGOODA SEEMORE conglo ne, INDOON c Bullfin g merate, do n4a Tray ch 4a Seabrook CONNIE lomite, diamicti ning K Lake Julia Mungari P te ás ununoppin Coo f4b d4 HAMPTON remier Downs Dowerin Eva Lake s4b lgardie s4b b g4 Sea Óv Óv PLAINS Decoration Cave bird Bullabu b4a S f4b LOONGANA lling A SP 5c Bol Nu HI INIFEX Ponton g6 gart Wy ngarin D K e G alkatch uilderton Goomalling em g4b g KANGAR d L D O gy4b d3b n4 4 OO 4b L L f4 O RA Seemor RANGE a SO S b NGE e Dow G UTHERN C HILL E BR S ns ingin ROSS S A LL Ô b3b Boorabbin E I Cowarna k g4a b4a S H f4b BINDOON b3b n3c Burracopp n3c Westonia HIGHWAY f4b Downs N U L L A R FORREST Ó in EASTERN g4 K B O R 2300 s PERTH s3b Moo b4a Nalarine Rock Mt Belches b4a anandah P L 5 TO rine KAMBAL A I N ODYAY M Walgo Boodalin Rock d4b DA Óv Muc n3c KELLERBERRIN ERREDIN GREAT olan YILGARN g4b f4b ük hea R g4 b4a f4b s6e s3b AVON G RANGE LAKE LEFROY TRANS-AUSTRALIAN rass Valley H b SOUTHERN CROSS Marvel Lo g4 Lake Rivers Uraryie Rock Creek Rawlinna 5b b3b Tammin ines Hill 3b ch Mandilla b4a Doodlakine s3b f4b Harris Lake RAILWAY Bakers Hill NORTHAM Meckering Cunder Tandegin Rock s4a b4 BOORABBIN Lake Ha din Kellerberrin a b4a s4b Haig 2 mersley Group f4b Spy Hill Kybo 500 H2 BIF, Wundowie Sandalwood Rock PARKER Madoonia chert, shale, rh 2 s3b RAN Widgiemooltha WIDGIEMOOLTHA Downs yolite, doler 400 YORK b3b GE f4b ite A N b3b H1 Bru g s dolomite, BIF, s Ôk PERTH n3c ce Rock 4a Barker Lake 4b s6e ZANTHUS hale ROTTNEST HELENA R g4 ISLAND M Quairadin n4a Lake Percy 31° a 5a c g E n b3b f4b N Willey Lakes I s6e a n3 DL S c c BROOKTON HIGHWAY b3 E d7d NARETHA i n3c b O LL Mt Dale LAKE COWAN O p K B W HI NG WINANA ü everley b4a A Pon k g4 Narebe dana ro Garden I en R 2500 CANNING R Mt Kok b3b Mundale Symons Hill T GREAT eby ROC b3b Lake s4b

KINGHAM Yengening Lakes s4a g4 R D A R L I N G G N I L R A D S Warnbro Sound Mc outh Kumminin d4b E Fortescue Westdale Mt Holland f4b S MADURA– F Group Becher Point Mt Thirsty RA 5 sha n3c F ük Úk le, chert, ba 4c Serpentine Dam AVON RIVER C salt s3b orriginLake Kurrenkutten EUCLA–NOONAERA PINJARRA Brookton DRYD f4b Moonera Horseshoe Cave EN LAKE JOHNSTON Frase Arubiddy F4 MA HILLS r Range basalt, san NDURAH Óv b4a Noresema Mullamulling Cave dstone, carb North Dandal n3c Pingel CORRIGIN Hyden d4b n Newman Rock onate rocks N up ly Kondinin Firestick Cave Glen Gr s4 260 oup s 0 b4 Southern basalt, sa F3 i Lake O'Connor a H Weebubbie Cave ndst t Bullaring Lake Carmody D ills Eucla one, conglom G basalt g4 Cape Bouvard PINJARR Yealering McCann Rock UNDAS erate gy4 n A SOUTHERN HYDEN Karlga H Murra-El-Elevyn Cave a n3c Lake Yealering rin LAKE HOPE s3c ILLS Harms Lake Mundrabil l la R t Coolup Dwellingup Mt Gordon Mundrabilla oadhouse LAKE JOHNSTON Madu F2 A Wander b3b Cocklebiddy ra Pole sandstone, d MURRAY RIVER BODDING ing Kulin Jilakin Lake Lake Hurlstone Óv Roadhouse lle Group acite, rhyo f 4b g

TON E G N A R BR lite 4 Ôk EMER Balladonia Noondoonia Tommy Grahams Cave basalt, koma 4 D Roadhou tiitic ba Po d n Ó warda R se salt, BIF 4 i Lake Clifton s n3c ANGE NORSEMAN t Cuballing SAND PLAIN HILLS F1 ba n4 f WAROONA s3b Wickepin Lake Gilmore g7e Woorlba HIGHWAY salt b3b Ôk PLAINS No Ri n3c f3b b3b Óv LAKE EYRE Caiguna ROE rie Group Cookernup Yarloo Mt Saddleback NARRO H DUNDAS BALLADONIA metabasa e 2700 p GIN arrismith n7 Balladon lt, felsic b4 u c ia Twilight vo N Harvey COOLGARDIE lcanicla s sc HARVEY Reservoir Widdingbillia Hill 32° tic rocks, BIF HIGHWAY Cove Quindanning Lake Camm n6e Mt Andrew Red Rocks Point e Williams Lake Sharpe CULVER Mur rt BIN Stirling Dam chison S o NINGUP YACKRIKINE Nanambin CLIFFS upergroup 4a ia Mu F n3c Lake G g basalt, cla RANGE race N 7e Gambanca Lake stic and Lake Grace North ewdegate Lake Kathleen B Point Dover c Aus RIVER Three Star Lake gy4b ooanya hemical sedim tralind ük Sal BAXTER entary rocks B Kuk LAKE mon Gums U k NBURY Allanson Mt Harris erin Lake Buchan PALLARUP Lake King Lake Tay e 2800 Burek DA ARTHUR n7c Toolinna Cove áb up s3b n3c RKAN Lake Grace South e C ALBANY Óv r GEOGRAPHE D OLLIE WA Dumbleyung ardanup åc GIN n3 C Mt Fisher Dumbleyung Lake Lake Lockhart Pyramid Lake Mt Coobaninya o

BAY ESPERANCE t Cape Naturaliste CAPEL Boyanup Wellington n4a g4 LAKE Point Culver G R E A T A U S T R A L I A N B I G H T i BUSS Dam COLLIE Grass Patc s3 f3 u 3c EL MAGENTA h q DUNSB TON MARTUP OROUGH DONN s3b n3 Lake Chinocup g7c ük d3 s Yalling YBROOK c HILLS up Ô DUMBLEYUNG Nyabin Mt Ridley Mt Buraminya k åc Moodiarrup g Pi NEWDEGATE n4a Ôk Mo HIGHWAY ngrup OLDFIELD g7 Ôk s3b ü e n7c Kirup RAVENSTHORPE k n6e De G 2900 YOUNG g7 D rey S ü Ravensthor c WYLIE SCARP upergr b BUSSELTON–AUGUSTA k pe Clyde Hill oup 3 ra Balingu Saddleback Hill WEST Scaddan Kau Rock s p Óv n7c Óv andstone, g3 a K HIGHWAY Mt Dean Brooks Peak BIF, ba Jarrah ATANNIN g7 salt, rh b Cowa wood Green G e yolite l Ôk ramup R bushe i G s Boyup B g4 b3b s7 racetown rook f3b g n d P 3b 6e MA MARGARET WHICHER ás KOJO Bro HIGHWAY Mt Ragged 3b RGARET RIVER n3c n3c NUP omehill RIVER h RIVER Scott Rocks t 3 n8c R Nannup n3c s3b FITZGERALD Jerdacuttu Munglinup Gibson r AN p o GE BR Gnow RIVER Mb ESPERANCE – MONDRAIN ISLAND n7c Witch IDGETOW angerup s R cliffe N n4a 3b N Cape Freycinet BLACKWOOD áb ük g7c MALCOLM – CAPE ARID 33° n3c Ongerup GAIRDNER g4 Tambellup Nu Nullagine G 300 roup p 0 Ôk n3 Jerramungup g7e Israelite Bay Hamelin Bay c Maintop Hill Fanny Cove Conding Point Dempster psammite, p Shoal Cape up elite se Mt Mack RIVER Powell Point , metabasalt n ü Hopetoun g7e ESPE g7e s7d W Whundoo i s3b k TONE RIVER RANC h r Cape Hamelin Ós áb GORDON RIVER g7c n E Group 7c b P MANJIMUP Mid Mt Barren Esperance ük asalt, dacite, r AUGUSTA RIVER Stokes Inlet n7c Point Malcolm hyolite 3a Cranbroo BREMER RIVER Bay Wharton s6e k COAST Cape Leeuwin FLINDERS Mb Rossiter Hammer Head Tagon g ük n7c Cape Le Grand Mt Le Grand n7c Úk 7e Daw I d8c BAY Pe RIVER Doubtful Island Bay Harbour s7c mberton RIVER Mt Arid Cape Pasley Tenter s6d Bay n7c n7c Cape Arid g áb DONNELLY n6d den Ôk 200 m Fran n 3100 WARREN kland IRLING RANGE Boxwood Hill ük n i Lake Muir RIVER ST MONDRAIN I 7c b2 t Bluff Knoll f ás PEMBERTON – IRWIN INLET n6e MIDDLE I Soane i Rocky Gully g Well Warramurrup Hill Doubtful Is n7c R E C H E R C H E sville Group 4 stead R SOUTH n6 Ôk e B sandston S MOUNT BARKER – ALBANY Mt Groper n6d Ô remer Bay T H E e, basalt e R k Dillon Bay Callcup Hill No MO A R C H I P E L A G O N n rthcliffe UNT BAR n6e O F 1000 m a 2c KER SOUTH r WESTERN g7e PO n6e BREMER BAY g7e Cooper I d2 r Mt Roe R EA ON e GUR ük G g U R T 7e R P E H A E 2000 m NGE N RA R Roebour N ne G a Point D'Entrecasteaux n6d( GE Salisbury I C roup g7e) s r n6d( 7d 3000 m ba g7e n salt, a 320 ) 6d(g7e) R komatii 0 SHANNON Mt Frankland te, che Mt Romance rt b l FRANKLAND KALGAN R n6d A g2 i (g7e) P BE n6d Ôk Walpole NNE (g7e) t HIGHWAY RAN TT DENMARK Mt Manypeaks s G 34° s2 a Chatham I E Bald I 2b Two Peoplesg Bay E 2 Foul Bay 7e

William Bay Point Ôk King Georgeg7e SoundCape Vancouver Hillier Knapp Ôk 4000 m Pilba Head ra Supergroup TorbayALBANYn6d basalt, komatiite f2 3300 Head (g7e) , dacite, rhyolite P b2 Eclipse I n2 2a

3400 g1 1d

S O U T H E R N O C E A N 5000 m

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3600 1 114° 115° 1b 116° 117° 118° 3700 119° n1 120° 121° 1a 122° 36° f 123° felsic volcanic d mafic and ultrama n 3800 124° rocks fic gne W intrusion iss 125° s E Age 126° s (Ma) sedime b O ntary ma g rogeny 127° fic and ultramafic rocks granite intrusi 128° volcanic rocks ons 129° Sedimentary a (syenite gy) Event nd volcanic rock in major litho s stratigraphic units (mainly low Sedim metamorphic gr entary, volca ade) nic and intrusive (low to high me rocks tamorphic grade) Orogenic and tectonic events FigureFigure 11. GeGeologicalological map of Western Australia, 22015015

A PDF ooff the mamapp and the associated didigitalgital data ffilesiles can be downloaded ffromrom the Data and Software Centre at .

For more information, contact David Martin ([email protected]).

Fieldnotes January 2016 7 3D Geomodel Series

Publication of the first GSWA 3D models

The first 3D geology digital packages (‘3D Geomodel Series’) number of prospective large igneous complexes within the Yilgarn were released to the public on 30 November 2015. They include to be modelled; applying the same techniques to many other a full representation of the area in three dimensions as well similar rock assemblages could vastly increase the exploration as the standard 2D digital data suite. All aspects of the model space for magmatic intrusion-related commodities such as nickel can be viewed with Geoscience Analyst, an easy-to-use free and copper. third-party viewing software that is included in the package. Also provided are the 3D contents of the package in widely The Sandstone model, which includes significant gold used file formats for import into the users’ own software. With deposits, explores the deep fault geometries across the the publication of three-dimensional geological models, the Northern Yilgarn Craton. Such structural models at the Geological Survey of Western Australia (GSWA) is enabling a scale of the Earth’s crust can image the architecture of a better understanding of the Earth’s structure, and an improved mineral system from ancient mantle-tapping fault zones to knowledge base to underpin exploration for mineral and energy resources.

Faults, fracture zones and shear zones can be pathways for fluids and melts within the solid Earth. The Earth’s 3D structure therefore not only reflects the distribution of physical properties of the rock mass in bedrock, sedimentary basins and regolith cover, but often relates very closely to the spatial distribution of mineral deposits and energy resources that formed as a consequence of fluid flow in the Earth’s crust. 3D structural modelling and numerical simulation of geological processes are emerging techniques that can be used to extend knowledge from exposed and well-understood areas to inaccessible or data-poor parts of the Earth’s crust and lithosphere, and to test the validity of conceptual models and interpretations.

The construction of 3D models utilizes the full spectrum of extensive geological mapping and geophysical (magnetic, gravity, deep seismic reflection) data acquired by GSWA as part of the Figure 1. Geological sections from the 1:100 000 map series and seismic interpretations which went into Exploration Incentive Scheme (EIS). Differences building the Windimurra model. Grey lines show the model faults. in the physical properties within the Earth allow inversion of the data to give property distributions from which boundaries can be inferred at depth. No geophysical dataset contains uniquely correct solutions when the question of depth versus density/ susceptibility/seismic velocity is concerned, but when all datasets are used in conjunction, the correlations increase and the ambiguity decreases. Modelling synthesizes these data into a product which simultaneously explores and unites the 3D information contained within each dataset.

The first two 3D Geomodel Series products released are the Windimurra, and the Sandstone models. These regions, located in the northern Yilgarn Craton, have known deposits of vanadium and gold. The models enhance exploration potential for more gold, platinum group elements, nickel, and copper.

At Windimurra in the Murchison Domain of the Yilgarn Craton, the 3D model predicts where ultramafic rocks, prospective for chrome and platinum group elements, may continue at depth Figure 2. Model surfaces from the Windimurra model within the framework of the seismic beneath the surface. Windimurra is the first of a interpretations 8 Fieldnotes January 2016 3D Geomodel Series

Figure 3. The Sandstone greenstone mineralizedm rocks near the surface. A more comprehensive fault belt model surfaces were derived modelmom that spans across several mineral camps in the Northern from surface geological YilgarnYil Craton is due to be released in 2016. mapping, gravity and magnetic potential field inversions InIn early 2015, a 3D model of the Canning Basin was released as and a deep partpap of a collaborative project between GSWA and the Centre for seismic EnergyEnE Geoscience at The University of Western Australia. This reflection modelmom provides an important contribution to better understand survey. thethe geological evolution of the Canning Basin. The model also helpsheh to identify prospective areas for petroleum production and carboncac sequestration, and petroleum and shale gas potential of thethe Canning basin.

TheThT digital models are available on USB flash drives that contain all thethe software for viewing the model in 3D. The USBs also include accompanyingac GSWA Records which provide detailed background informationinf for the 2D GIS components of the digital packages.

Windimurra,W 2015: 3D Geomodel Series and Sandstone, 2015: 3D3 Geomodel Series are accessible via the DMP eBookshop at .

ForFoF more information, contact RuthRuR Murdie ([email protected]).

Figure 4. The Canning Basin model shows the depth to basement, several generations of faults, and the wells from where the data originated.

Fieldnotes January 2016 9 Roger Hocking bids farewell to GSWA

The retiring type

After 41 years at the Geological and stumpy Devonian coral (Disphyllum hockingi). Survey of Western Australia (GSWA), Roger Hocking has Over the next ten years of field- and office-based studies that retired. included the publication of numerous Explanatory Notes, Reports, papers, and a Bulletin, Roger’s name became synonymous with Roger arrived in Perth from New the Carnarvon Basin. For petroleum exploration companies and England in New South Wales on many generations of geology students he was ‘Mr Carnarvon 10 December 1974 and joined Basin’. During the 1980s Roger also contributed significantly GSWA the next day. Roger was to the understanding of other Phanerozoic basins in the State attracted by Perth’s proximity to — reflected in Memoir 3 and also in the 1988 State geological the coast and the opportunities map, which he co-authored. In the late 1980s to early 1990s he for surfing the Indian Ocean continued work on the Carnarvon Basin, carrying out core-based waves. In fact, photographic studies of the North West Shelf. evidence suggests he fitted the surfie model of the 70s — lean, By 1993, Roger’s main area of research had moved to the Lennard with long sun-bleached hair. Shelf Devonian reef complex. These fossilized reefs — the Great Barrier Reef of the Devonian — kept Roger busy for the next four He was initially attracted to the coastal gorges as well as the years culminating in co-authorship of a special series of eight spectacular scenery of the Murchison River Gorges at Kalbarri. maps that would ultimately accompany Bulletin 145, published in His work on the early Paleozoic Tumblagooda Sandstone offered 2009 under the authorship of PE Playford, RM Hocking and AE an exciting location for research for his Master’s degree, which Cockbain. He nostalgically recalls the luxury of being able to bathe he completed in the mid-1980s. Roger’s foundation work on this almost every night in beautiful rock pools during these long field little-described formation was recognized by a work colleague seasons — and maintaining a suntan that lasted four years. It was who named a fossilized arthropod escape burrow after him during this time that Roger’s prowess at campfire cooking was — Tumblagoodichnus hockingi! Further accolades followed, passed on to those ‘younger geologists’ who worked with him, as with his name also put to a coarse and warty-textured Permian well as his tastes in somewhat obscure 1960s and 1970s music. brachiopod (Neochonetes (Sommeriella) hockingi), and a short In 1997, Roger commenced mapping in the Paleoproterozoic Earaheedy Basin. His ‘holistic view of the scope of the project boundaries’ led to him working on neighbouring Neoproterozoic successions, as well as discovering the first recorded gold mineralization at Quadrio Lake in the Little Sandy Desert. He transitioned seamlessly from the Phanerozoic to the Proterozoic. In 2007 Roger took up the mantle of Chief Geoscientist. In this role he utilized his broad-ranging experience of most of Western Australia’s basins to offer high-level advice and expertise to enhance understanding of the geological framework of Western Australia both within and outside GSWA, and was a mentor to many younger GSWA recruits. He also sought opportunities to promote the many outstanding geological features of Western Australia in the area of geotourism.

After co-authoring the 1998 State map, he has been instrumental in bringing the next State map into the digital world of 2015; its release date serendipitously aligned with his date of commencement at GSWA.

We wish Roger well in the new phase of his life.

10 Fieldnotes January 2016 Geophysical surveys

GSWA regional geophysics KUNUNURRA surveys: December 2015 update BROOME

The latest release of Geological Survey of Western Australia (GSWA) regional KARRATHA 2 geophysical surveys is the Ngururrpa gravity survey. Data downloads Final data releases from the Geophysical Archive Data Delivery System can CARNARVON be found at . MEEKATHARRA WARBURTON

Grids and images from the GSWA website are Airborne mag-rad surveys available from . Ground gravity surveys 1 Subscribe to the GSWA eNewsletter for alerts of

KALGOORLIE preliminary and final data release dates. EUCLA PERTH Survey outline shapefiles are available online at . 3 For more information, contact David Howard ([email protected]). ESPERANCE

ID Area/Name Method Configuration Units Status Start End Release 1 Yalgoo 2015 Mag-Rad 100 m; E/W 111 000 km Pre-release 31/05/15 27/09/15 10/12/15 2 Ngururrpa 2015 Gravity Grid 2.5 km 4 964 stns Released 10/05/15 13/06/15 30/07/15 3 SW Yilgarn 2015 Gravity Roads 2 km 23 719 stns Processing 12/06/15 02/12/15 Mar-16* Mag-Rad = Magnetic/Radiometric Perth and Peel Green Growth Plan The impact of future development in the Perth and Peel Significant input was mademade regions is the focus of the draft Perth and Peel Green Growth through the urban and Plan for 3.5 million (Green Growth Plan) which was released industrial planning processescesses for public comment on 17 December 2015. This Plan is the to avoid development inn lowlow culmination of the 4.5 year multigovernment agency strategic lying areas that would requirerequire assessment of the Perth and Peel Region. excessive BRM for fill, thusthus reducing the overall BRMM ddemand.emand. The Perth and Peel regions are projected to grow to 3.5 million people by 2050 — an increase of almost 70% on our The Green Growth Plan provides current population. Supporting this growth and delivering an greater certainty to basicic raw efficient and liveable city while protecting our unique natural material operators environment is a significant challenge. The State Government regarding where extractiontion prepared the Green Growth Plan to meet this challenge, and can be considered and it will in this context it delivers two critical outcomes. It will cut resolve some long-standingding red tape by securing upfront Commonwealth environmental issues, such as limestonene supplysupply approvals, and streamline State environmental approvals for to the north of Perth. the development required to support growth to 3.5 million The State government iss seekingseeking people. It also plans for unprecedented protection of our public comment on the draft GGreenreen bushland, rivers, wildlife and wetlands. Growth Plan until 8 Aprilril 2016. The assessment managed by the Department of Premier and GSWA will continue to ccontributeontribute Cabinet was the largest undertaking of its kind in Australia. to the Plan during 20166 The Land Use Geoscience section of the Geological Survey of assisting with stakeholderder Western Australia (GSWA), in close collaboration with other feedback regarding BRMM government agencies, industry and other divisions within the matters. Department of Mines and Petroleum (DMP), played a key role BRM mapping associateded in identifying strategic basic raw materials (BRM) within the with the Green Growth Plan regions. GSWA’s assessment process involved Geographical is available from the Landnd UseUse Information System (GIS) based multicriteria decision making Planning layer in GeoVIEW.WA on to ensure the final footprint for BRM extraction took into DMP’s website at . consideration relevant factors such as biodiversity, resource availability, opportunities for sequential land use and access For more information, contact including transport costs. Warren Ormsby ([email protected]). Fieldnotes January 2016 11 Product releases ISSN 1325-9377 ISBN (PRINT) 978-1-74168-660-9 Any prices include GST ISSN 1834-2272 ISBN (PDF) 978-1-74168-659-3

RECORDS NON-SERIES MAP Record 2015/1 Geological Survey work program for 2015–16 Geological map of Western Australia, 1:2.5 million 2015 and beyond DATA PACKAGE Record 2015/3 Alteration mineral zonation associated with BIF- hosted iron ore: mineral mapping using hyperspectral drill Sandstone: 3D Geomodel core data Series (includes by L Chiarelli Record 2015/11 The Record 2015/8 Detrital zircon geochronology of upper Ediacaran Sandstone greenstone to lower Cambrian deposits (Supersequence 4), western belt, northern central Amadeus Basin: testing revised stratigraphic correlations Yilgarn Craton: 3D by PW Haines, MTD Wingate, CL Kirkland, and HJ Allen modelling using geological and geophysical constraints) 1:100 000 GEOLOGICAL SERIES MAP by RE Murdie, K Gessner, and SF Chen MOUNT MAGNET, WA Sheet 2441 by I Zibra Windimurra: 3D Geomodel Series (includes Record 2015/12 The Windimurra igneous complex, Yilgarn Craton: an Archean 1:100 000 GEOLOGICAL INFORMATION SERIES layered intrusion revealed by seismic data and 3D modelling) Western Capricorn Orogen, 2015 by TJ Ivanic and J Brett DMP launches new website The Department of Mines and Petroleum (DMP) is pleased the way our stakeholders want to use the site.’ to announce the launch of our brand new website. The site has many new features and enhancements including a greatly There are a few things to note: improved search function. It has been designed with our clients • Access to online systems is now on the right-hand side of every and stakeholders in mind — you! Its design is focused on being page. All your favourite systems are there (click on VIEW MORE user-centric and intuitive. to see the full list) and in some cases improved (e.g. GeoVIEW.WA now includes Statewide airphoto mosaic under ‘Landgate Aerial DMP Director General Richard Sellers said the department had Imagery’ and Explanatory Notes System as new ‘Search Tools’). spent the last couple of years researching and designing the new • Quicklinks on the left-hand side allow repeat customers to easily website. navigate to their form or system of interest; on the right-hand ‘The way people access information online has changed in the six side, the ‘Recently Viewed’ option keeps a memory to allow easy years since the current website was launched,’ he said earlier in navigations to pages visited on previous sessions/visits. the year. ‘The new website will be more intuitive and better reflect • New layers relating to the Perth–Peel Green Growth Plan have been added to GeoVIEW.WA under the Land Use Planning tab. • Resource Statistics has been moved to the Investors page. • There will be different news items shown on the GSWA landing page. • To see an overview of the site pertaining to GSWA, hover your mouse over ‘Geological Survey’ in the top navigation bar. Did you know? All the final reports submitted under the Co-funded Exploration Drilling program of the Exploration Incentive Scheme (EIS) can be found in WAMEX (via GeoVIEW.WA Search Tools) by selecting ‘Co-funded drilling’ in the ‘Report Type’ drop-down.

You can access the new website as before at . Note that previous shortcuts will need to be refreshed. Figure 1. 1 Landing page for the new DMP website

The Geological Survey of Western Australia (GSWA) has released almost 5000 geological products including books, maps and data packages. These can be found on our website at . Maps, USB data packages, and selected premium publications are available to purchase as hard copies via the online cart on the eBookshop at . Alternatively, these products can be purchased from the Information Centre, First Floor, Mineral House, 100 Plain Street, East Perth, WA 6004, Australia, Phone: +61 8 9222 3459; Fax: +61 8 9222 3444. Records, Reports, Bulletins and non-series books cannot be purchased in hard copy but are all available as PDFs to view, and as a free download.

Products were produced using information from various sources. The Department of Mines and Petroleum (DMP) and the State cannot guarantee the accuracy, currency or completeness of the information. DMP and the State accept no responsibility and disclaim all liablity for any loss, damage or costs incurred as a result of any use of or reliance whether wholly or in part upon the information provided in this publication or incorporated into it by reference.