Mineral Occurrences and Exploration Potential of the Paterson Area

Total Page:16

File Type:pdf, Size:1020Kb

Mineral Occurrences and Exploration Potential of the Paterson Area Department of Industryand Resources REPORT 97 MINERAL OCCURRENCES AND EXPLORATION POTENTIAL OF THE PATERSON AREA by K. M Ferguson, L. Bagas, and I. Ruddock Keep 3 mm border around photo. Resize white box as required. Geological Surveyof Western Australia GEOLOGICAL SURVEY OF WESTERN AUSTRALIA REPORT 97 MINERAL OCCURRENCES AND EXPLORATION POTENTIAL OF THE PATERSON AREA by K. M. Ferguson, L. Bagas, and I. Ruddock Perth 2005 MINISTER FOR STATE DEVELOPMENT Hon. Alan Carpenter MLA DIRECTOR GENERAL, DEPARTMENT OF INDUSTRY AND RESOURCES Jim Limerick DIRECTOR, GEOLOGICAL SURVEY OF WESTERN AUSTRALIA Tim Griffi n REFERENCE The recommended reference for this publication is: FERGUSON, K. M., BAGAS, L., and RUDDOCK, I., 2005, Mineral occurrences and exploration potential of the Paterson area: Western Australia Geological Survey, Report 97, 43p. National Library of Australia Cataloguing-in-publication entry Ferguson, K. M. Mineral occurrences and exploration potential of the Paterson area. Bibliography. ISBN 1 74168 018 2. 1. Mines and mineral resources — Western Australia — Paterson Range Region. 2. Minerals — Western Australia — Paterson Range Region. 3. Geology, Economic — Western Australia — Paterson Range Region. 4. Paterson Range Region (W.A.). I. Bagas, L. (Leon). II. Ruddock, Ian. III. (Title. (Series: Report (Geological Survey of Western Australia); 97). 553.409941 ISSN 0508–4741 Grid references in this publication refer to the Geocentric Datum of Australia 1994 (GDA94). Locations mentioned in the text are referenced using Map Grid Australia (MGA) coordinates, Zone 51. All locations are quoted to at least the nearest 100 m. Copy editors: A. S. Forbes, L. Day Cartography: M. Prause Desktop publishing: K. S. Noonan Published 2005 by Geological Survey of Western Australia This Report is published in digital format (PDF), as part of a digital dataset on CD, and is available online at www.doir.wa.gov.au/gswa/onlinepublications. Laser-printed copies can be ordered from the Information Centre for the cost of printing and binding. Further details of geological publications and maps produced by the Geological Survey of Western Australia are available from: Information Centre Department of Industry and Resources 100 Plain Street EAST PERTH, WESTERN AUSTRALIA 6004 Telephone: +61 8 9222 3459 Facsimile: +61 8 9222 3444 www.doir.wa.gov.au/gswa/onlinepublications Cover photograph: Coolbro Sandstone (foreground and background) in the Throssell Range about 12 km south-southwest of Nifty copper mine, looking east (MGA 348650E 7591950N). Coolbro Sandstone is overlain further east by poorly outcropping Broadhurst Formation that is highly prospective for stratabound base-metal mineralization; to the south the Coolbro Sandstone overlies the unconformity with the Rudall Complex that is highly prospective for vein and hydrothermal uranium mineralization Contents Abstract ..................................................................................................................................................................1 Present study ..........................................................................................................................................................2 Location and access ................................................................................................................................................2 Climate and vegetation ...........................................................................................................................................2 Physiography ..........................................................................................................................................................2 Carboniferous to Permian land surface ...........................................................................................................2 Cenozoic land surface .....................................................................................................................................3 Erosional, relict or residual land surface ..................................................................................................3 Depositional land surface .........................................................................................................................3 Previous work .........................................................................................................................................................5 Regional geology ...................................................................................................................................................5 Paterson Orogen ..............................................................................................................................................5 Paleoproterozoic to Mesoproterozoic Rudall Complex ...........................................................................6 Talbot Terrane ..................................................................................................................................6 Connaughton Terrane ........................................................................................................................6 Paleoproterozoic orthogneiss ............................................................................................................6 Paleoproterozoic deformation and metamorphism in the Talbot and Connaughton Terranes ..........7 Tabletop Terrane ...............................................................................................................................7 Pungkuli–Taliwanya Formations .............................................................................................................7 Taliwanya Formation .......................................................................................................................7 Pungkuli Formation .........................................................................................................................7 Unassigned sandstone ......................................................................................................................8 Neoproterozoic northwestern Offi cer Basin ............................................................................................8 Tarcunyah Group ..............................................................................................................................9 Sunbeam Group ...............................................................................................................................9 Boondawari Formation ....................................................................................................................9 Disappointment Group .....................................................................................................................9 Durba Sandstone ..............................................................................................................................9 Neoproterozoic Yeneena Basin ..............................................................................................................10 Throssell Range Group ...................................................................................................................10 Coolbro Sandstone ...................................................................................................................10 Broadhurst Formation ..............................................................................................................10 Isdell Formation .......................................................................................................................10 Lamil Group ....................................................................................................................................10 Malu Formation .......................................................................................................................10 Telfer Member ..................................................................................................................11 Puntapunta Formation ..............................................................................................................11 Wilki Formation .......................................................................................................................11 Age of the Throssell Range and Lamil Groups ..............................................................................11 Miles Orogeny ........................................................................................................................................11 Mount Crofton Granite and associated granitic rocks ..........................................................................11 Paterson Orogeny ...................................................................................................................................11 Possible kimberlite dykes ......................................................................................................................12 Phanerozoic Canning and Gunbarrel Basins .................................................................................................12 Carboniferous to Permian rocks .............................................................................................................12 Paterson Formation ........................................................................................................................12 Poole Sandstone and Noonkanbah Formation ...............................................................................12
Recommended publications
  • THE ARCHAEAN and Earllest PROTEROZOIC EVOLUTION and METALLOGENY of Australla
    Revista Brasileira de Geociências 12(1-3): 135-148, Mar.-Sel.. 1982 - Silo Paulo THE ARCHAEAN AND EARLlEST PROTEROZOIC EVOLUTION AND METALLOGENY OF AUSTRALlA DA VID I. OROVES' ABSTRACT Proterozoic fold belts in Austrália developed by lhe reworking of Archaean base­ mcnt. The nature of this basement and the record of Archaean-earliest Proterozoic evolution and metallogeny is best prescrved in the Western Australian Shield. ln the Yilgarn Craton. a poorly-mineralized high-grade gneiss terrain rccords a complex,ca. 1.0 b.y. history back to ca. 3.6b.y. This terrain is probably basement to lhe ca. 2.9~2.7 b.y. granitoid­ -greenstone terrains to lhe east-Cratonization was essentially complete by ca, 2.6 b.y. Evolution of the granitoid-greenstone terrains ofthe Pilbara Craton occurred between ca. 3.5b.y. ano 2.8 b.y. The Iectonic seuing of ali granitoid-greenstone terrains rcmains equivocaI. Despitc coincidcnt cale­ -alkalinc volcanism and granitoid emplacemcnt , and broad polarity analogous to modem are and marginal basin systcrns. thcre is no direct evidencc for plate tectonic processes. Important diffcrences in regional continuity of volcanic scqucnccs, lithofacies. regional tectonic pauerns and meta1Jogeny of lhe terrains may relate to the amount of crusta! extension during basin formation. At onc extreme, basins possibly reprcsenting low total cxrensíon (e.g. east Pilbara l are poorly mi­ ncralizcd with some porphyry-stylc Mo-Cu and small sulphute-rich volcanogenic 01' evaporitic deposits reflecting the resultam subaerial to shaJlow-water environment. ln contrast, basins inter­ prctcd to have formcd during greater crusta! cxrcnsion (e.g.
    [Show full text]
  • Telfer W with Pr 800,000 Copper Signific Resourc
    4420 Newcrest Cover 04 6pp 16/9/04 9:52 AM Page 2 Telfer will be the largest gold mine in Australia, with projected annual production of more than 800,000 ounces of gold and 30,000 tonnes of copper for 24 years, positioning Newcrest as a significant and profitable Australian-based resources business. Newcrest Mining Limited Newcrest – The Sustainable Section 5 Resource Business 1 Sustainability and People 38 Section 1 Health and Safety 40 Our Results 2 Environment 42 Human Resources 43 Performance in Brief 2 Chairman’s Review 4 Section 6 ABN: 20 005 683 625 ABN: Managing Director and Corporate Governance 44 Chief Executive Officer’s Report 5 Board of Directors 45 Newcrest Senior Management 10 Corporate Governance 46 Financial Report 11 Section 7 Section 2 Concise Annual Report 2004 Financials 49 Operations 12 Directors’ Report 50 Cadia Valley Operations 14 Management Discussion and Analysis Ridgeway Gold/Copper Mine 14 of the Financial Statements 56 Cadia Hill Gold/Copper Mine 16 Statement of Financial Performance 58 Toguraci Gold Mine 19 Statement of Financial Position 59 Section 3 Statement of Cash Flows 60 Projects 22 Notes to the Concise Financial Report 61 Directors’ Declaration 68 Telfer Gold/Copper Project 24 Independent Audit Report 69 Cracow 26 Cadia East 28 Shareholder Information 70 Boddington Expansion Project 29 Five Year Summary 72 Section 4 Corporate Directory IBC Exploration 30 Strategy and Review 32 Mineral Resources and Ore Reserves 34 Newcrest Mining Limited Newcrest ABN: 20 005 683 625 Notice of Meeting Notice is hereby given that the 24th Annual General Newcrest Mining Limited Meeting will be held at the Hyatt Regency Hotel, Concise Annual Report 2004 99 Adelaide Terrace, Perth, Western Australia on Wednesday 27 October 2004 at 9.30am.
    [Show full text]
  • A Structural Examination of the Telfer Gold-Copper Deposit And
    ResearchOnline@JCU This file is part of the following reference: Hewson, Simon Andrew John (1996) A structural examination of the Telfer gold-copper deposit and surrounding region, northwest Western Australia: the role of polyphase orogenic deformation in ore-deposit development and implications for exploration. PhD thesis, James Cook University. Access to this file is available from: http://eprints.jcu.edu.au/27718/ If you believe that this work constitutes a copyright infringement, please contact [email protected] and quote http://eprints.jcu.edu.au/27718/ A Structural Examination of the Telfer Gold-Copper Deposit and Surrounding Region. northwest Western Australia: The Role of Polyphase Orogenic Deformation in Ore-deposit Development and Implications for Exploration. VOLUME 1 Thesis submitted by Simon Andrew John HEWSON BSc (Hans) (Curtin) in October, 1996 for the degree of Doctor of Philosophy in the Department of Earth Sciences at James Cook University of North Queensland. I, the undersigned, the author of this thesis, understand that the following restriction placed by me on access to this thesis will not extend beyond three years from the date on which the thesis is submitted to the University. I wish that access to this thesis not to be permitted for a period of three years. After this period has elapsed I understand that James Cook University of North Queensland will make it available for use within the University Library and, by microfilm or other photographic means, allow access to users in other approved libraries. All users consulting this thesis will have to sign the following statement: " In consulting this thesis I agree not to copy or closely para-phrase it in whole or in part without the written consent of the author; and to make proper written acknowledgement for any assistance which I have obtained from it.
    [Show full text]
  • Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant
    U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP CP-37 U.S. GEOLOGICAL SURVEY Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant 1:10,000,000 ICIRCUM-PACIFIC i • \ COUNCIL AND MINERAL RESOURCES 1991 CIRCUM-PACIFIC COUNCIL FOR ENERGY AND MINERAL RESOURCES Michel T. Halbouty, Chairman CIRCUM-PACIFIC MAP PROJECT John A. Reinemund, Director George Gryc, General Chairman Erwin Scheibner, Advisor, Tectonic Map Series EXPLANATORY NOTES FOR THE TECTONIC MAP OF THE CIRCUM-PACIFIC REGION SOUTHWEST QUADRANT 1:10,000,000 By Erwin Scheibner, Geological Survey of New South Wales, Sydney, 2001 N.S.W., Australia Tadashi Sato, Institute of Geoscience, University of Tsukuba, Ibaraki 305, Japan H. Frederick Doutch, Bureau of Mineral Resources, Canberra, A.C.T. 2601, Australia Warren O. Addicott, U.S. Geological Survey, Menlo Park, California 94025, U.S.A. M. J. Terman, U.S. Geological Survey, Reston, Virginia 22092, U.S.A. George W. Moore, Department of Geosciences, Oregon State University, Corvallis, Oregon 97331, U.S.A. 1991 Explanatory Notes to Supplement the TECTONIC MAP OF THE CIRCUM-PACIFTC REGION SOUTHWEST QUADRANT W. D. Palfreyman, Chairman Southwest Quadrant Panel CHIEF COMPILERS AND TECTONIC INTERPRETATIONS E. Scheibner, Geological Survey of New South Wales, Sydney, N.S.W. 2001 Australia T. Sato, Institute of Geosciences, University of Tsukuba, Ibaraki 305, Japan C. Craddock, Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, Wisconsin 53706, U.S.A. TECTONIC ELEMENTS AND STRUCTURAL DATA AND INTERPRETATIONS J.-M. Auzende et al, Institut Francais de Recherche pour 1'Exploitacion de la Mer (IFREMER), Centre de Brest, B.
    [Show full text]
  • For Personal Use Only
    To: Company Announcements Office LEVEL 9 600 ST KILDA ROAD MELBOURNE From: Francesca Lee VICTORIA 3004 AUSTRALIA Date: 13 February 2015 PO BOX 6213 Subject: Annual Mineral Resources and Ore Reserves ST KILDA ROAD CENTRAL Statement Explanatory Notes MELBOURNE 8008 T +613 9522 5333 F +613 9525 2996 www.newcrest.com.au Please find attached Newcrest Mining Limited’s Annual Mineral Resources and Ore Reserves Statement Explanatory Notes for the year ended 31 December 2014, for immediate release to the market. Yours sincerely Francesca Lee Company Secretary For personal use only A MEMBER OF THE NEWCREST MINING GROUP ABN 20 005 683 625 Explanatory Notes Newcrest Mining 13 February 2015 Annual Mineral Resources and Ore Reserves Statement – 31 December 2014 EXECUTIVE SUMMARY Newcrest Mining Limited has updated its Mineral Resource and Ore Reserve estimates for the twelve month period ending 31 December 2014 and for this purpose, has completed a detailed review of all production sources. The review has taken into account updated long term metal price, foreign exchange and cost assumptions, and mining and metallurgy performance to inform cut-off grades and physical mining parameters. This has resulted in the most marginal ounces being removed from the portfolio and these are reflected in changes to Mineral Resources and Ore Reserves. Group Mineral Resources As at 31 December 2014, Group Mineral Resources are estimated to contain 140 million ounces of gold, 20 million tonnes of copper and 130 million ounces of silver. This represents a decrease of approximately 8 million ounces of gold (~5%), 0.4 million tonnes of copper (~2%) and 1 million ounces of silver (~1%), compared with the estimate as at 31 December 2013.
    [Show full text]
  • Geological Survey of Western Australia Annual Review 1995–96
    GEOLOGICAL SURVEY OF WESTERN AUSTRALIA ANNUAL REVIEW 1995–96 GEOLOGICAL SURVEY OF WESTERN AUSTRALIA GEOLOGICAL SURVEY OF WESTERN AUSTRALIA ANNUAL REVIEW 1995–96 Perth 1996 MINISTER FOR MINES The Hon. Kevin Minson, MLA DIRECTOR GENERAL K. R. Perry DIRECTOR, GEOLOGICAL SURVEY OF WESTERN AUSTRALIA Pietro Guj Copy editor: I. R. Nowak The recommended reference for this publication is: (a) For reference to an individual contribution SHEPPARD, S., 1996, Mafic–felsic magma mingling in the Bow River batholith of the Halls Creek Orogen: Western Australia Geological Survey, Annual Review 1995–96, p. 56–60. (b) For general reference to the publication GEOLOGICAL SURVEY OF WESTERN AUSTRALIA, 1996, Geological Survey of Western Australia Annual Review 1995–96: Western Australia Geological Survey, 223p. ISBN 0 7309 6543 0 ISSN 1324-504 X Cover: Mississippi Valley-type marcasite–sphalerite ore from Goongewa mine, Lennard Shelf, Canning Basin. Deposit is hosted in platform-facies limestones of the Devonian reef complexes. Frontispiece: Helicopter taking off from base station during GSWA gravity survey of the Merlinleigh Sub-basin near Gascoyne Junction. One GPS antenna is set on a tripod over the base station and another is mounted on the helicopter to fix the gravity stations by differential GPS technique. Foreword Foreword It gives me pleasure to introduce you to the Geological Survey of Western Australia Annual Review for 1995–96 — our third issue. I take this opportunity to thank you, the reader, for your constructive feedback on the previous issues which, I hope, has been reflected in an improvement in quality and relevance. I have also been very flattered by, but have resisted, the suggestion that GSWA should charge for its Annual Review.
    [Show full text]
  • Telfer Project, Expansion of Telfer Gold Mine, Great Sandy Desert
    Telfer Project, Expansion of Telfer Gold Mine, Great Sandy Desert Newcrest Mining Limited Report and recommendations of the Environmental Protection Authority Environmental Protection Authority Perth, Western Australia Bulletin 1059 August 2002 ISBN. 0 7307 6694 2 ISSN. 1030 - 0120 Assessment No. 1445 Contents Page 1. INTRODUCTION AND BACKGROUND......................................................1 2. THE PROPOSAL.............................................................................................2 3. CONSULTATION............................................................................................7 4. RELEVANT ENVIRONMENTAL FACTORS ..............................................7 4.1 FLORA AND FAUNA ......................................................................................7 4.2 DEWATERING AND BOREFIELD OPERATIONS..................................................8 4.3 GREENHOUSE GAS EMISSIONS.......................................................................9 4.4 ACID MINE DRAINAGE...............................................................................10 4.5 MINE CLOSURE ..........................................................................................10 5. CONDITIONS AND COMMITMENTS .......................................................11 6. CONCLUSIONS.............................................................................................12 7. RECOMMENDATIONS................................................................................12 Table Table 1: Summary of key proposal characteristics.................................................6
    [Show full text]
  • 2019 Annual Report FORGING a STRONGER NEWCREST
    2019 Annual Report FORGING A STRONGER NEWCREST The success of FY19 reflects the enormous amount of effort applied by our people towards delivering on our commitments and our potential. SANDEEP BISWAS MANAGING DIRECTOR AND CHIEF EXECUTIVE OFFICER To be the Miner of Choice. To be the Miner of Choice for VISION our people, shareholders, host OUR communities, partners and suppliers. To safely deliver superior returns to our stakeholders from finding, developing and MISSION operating gold/copper mines. OUR NEWCREST 2019 ANNUAL REPORT 1 CONTENTS FORGING A STRONGER NEWCREST Forging a stronger Newcrest 2 Asset overview 4 Key Achievements for FY19 6 Safety & Sustainability 12 People 13 Releasing orebody potential 14 NEWCREST’S VALUE PROPOSITION Long reserve life 16 Delivering on commitments 16 Low cost production 16 Organic growth options 17 Financially robust 18 Exploration & technical capability 19 OUR COMPANY Chairman’s Report 8 Managing Director’s Review 10 The Board 20 Mineral Resources & Ore Reserves 24 Corporate Governance Statement 32 Directors’ Report 34 Financial Report 89 Corporate Directory 149 Coarse ore stockpile at Cadia, New South Wales, Australia FORGING A STRONGER NEWCREST The health and safety of our people 2 Forging a stronger is of primary importance at Newcrest. Newcrest Our clear focus remains on eliminating To achieve Newcrest’s full potential FORGING A STRONGER FORGING A STRONGER NEWCREST fatalities and life-changing injuries from for our stakeholders, our company our business, while striving to make strategy focuses on five key pillars, continual progress on reducing all injuries each with associated aspirations. and health impacts. We believe that a strong and enduring commitment to the health and safety of our workforce best reflects our values and underpins and sustains optimal business performance.
    [Show full text]
  • Early Palaeozoic Continental Growth in the Tasmanides of Northeast Gondwana and Its Implications for Rodinia Assembly and Rifting Chris L
    University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers Faculty of Science, Medicine and Health 2015 Early Palaeozoic continental growth in the Tasmanides of northeast Gondwana and its implications for Rodinia assembly and rifting Chris L. Fergusson University of Wollongong, [email protected] R A. Henderson James Cook University Publication Details Fergusson, C. L. & Henderson, R. A. (2015). Early Palaeozoic continental growth in the Tasmanides of northeast Gondwana and its implications for Rodinia assembly and rifting. Gondwana Research, 28 (3), 933-953. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Early Palaeozoic continental growth in the Tasmanides of northeast Gondwana and its implications for Rodinia assembly and rifting Abstract Gondwana formed in the Neoproterozoic to Cambrian mainly from collision along the East African and Kuunga orogens at about the same time that the Gondwana palaeo-Pacific facing margin became a long-lived active margin and formed the Terra Australis Orogen. This orogen, and in particular the Tasman Orogenic Belt (the Tasmanides) sector of eastern Australia, is distinguished by widespread shortening of quartz turbidite successions and underlying oceanic basement, with less abundant island arc assemblages. Early Palaeozoic accretionary development of the Tasmanides followed Rodinia breakup at 800-750 Ma to form the palaeo-Pacific cO ean. In eastern Australia, a second rifting episode at 600-580 Ma is more widely developed with siliciclastic sedimentation and rift-related igneous activity. In parts of the Delamerian Orogen of South Australia and northwestern New South Wales and in the exposed northern Thomson Orogen of north and central Queensland, the rift-related sedimentary successions have a dominant 1.3 to 1 Ga detrital zircon age signature implying local sources.
    [Show full text]
  • Long Term Landscape Evolution of the Western Australian Shield
    Joe Jennings: Father of modern Australian geomorphology BRAD PILLANS Research School of Earth Sciences, The Australian National University, Canberra, ACT, 0200, Australia ([email protected]) Joe Jennings was appointed to the Geography Department at the Australian National University (ANU) in 1953, and over the next three decades he had a profound and lasting effect on Australian geomorphology. Although best remembered as a karst geomorphologist, Joe had wide-ranging research interests and boundless enthusiasm for the entire discipline of geomorphology. Nowhere is this better evidenced than in the graduate students he supervised (with year of completion in brackets), including Eric Bird (1959), Nel Caine (1966), Ian Douglas (1966), Martin Williams (1969), Jim Bowler (1970), Bud Frank (1972), John Chappell (1973), Colin Pain (1973), Ross Coventry (1973), Chris Whitaker (1976), Joyce Lundberg (1976) and David Gillieson (1982). As a PhD student of John Chappell, and therefore an academic grandson of Joe, I was privileged to know him in the late 1970’s and early 1980’s at ANU. In this paper I have constructed a “family tree” of Joe’s academic descendents. Introduction Joseph Newell Jennings (1916-1984), or Joe to everyone who knew him (Fig. 1), was appointed to the fledgling Geography Department at the Australian National University (ANU) in 1953, and over the next three decades he had a profound and lasting effect on Australian geomorphology. Joe is best remembered as a karst geomorphologist, but in fact he had wide-ranging research interests and boundless enthusiasm for the entire discipline of geomorphology - see obituary and publication list in Spate & Spate (1985).
    [Show full text]
  • REFORMING AUSTRALIAN SHIELD LAWS Press Freedom Policy Papers
    Press Freedom Policy Papers Reform Briefing 2/2021 Anna Kretowicz REFORMING AUSTRALIAN SHIELD LAWS Press Freedom Policy Papers SUMMARY KEY POINTS • Shield laws allow journalists to maintain the confidentiality of information that would disclose the identity of a confidential source. • Shield laws are necessary to enable a free flow of information between members of the public and the news media. Sources, including whistleblowers, are less likely to supply the media with information if they believe that journalists will be unable to maintain their anonymity. • The scope of the protection conferred by Australia’s existing shield laws varies between different jurisdictions. This is in part due to the absence of a uniform definition of ‘journalist’. • In most Australian jurisdictions, shield laws do not prevent law enforcement agencies from accessing a journalist’s confidential information under a regular search and seizure warrant. REFORM CONSIDERATIONS • Shield laws should be harmonised nationwide. • Shield laws should be extended to police investigations. • The terms ‘journalist’ and ‘news medium’ should be defined in a consistent and broad way in order to maximise the protection of confidential sources in the modern media environment. law.uq.edu.au/research/press-freedom 2 Press Freedom Policy Papers REFORMING AUSTRALIAN SHIELD LAWS Reform Briefing 2/2021 “Journalists are bound by their code of ethics not to disclose sources, and to demand that they do is asking them to break a covenant recognised the world over as crucial to uncovering misconduct – when authorities would prefer the public to stay in the dark.”1 - The Board of the National Press Club of Australia This statement was released the day after the that could identify a source.
    [Show full text]
  • Kimberley & Pilbara
    KIMBERLEY & PILBARA • Landscape hotspots • Starring in movies • Brilliant beaches • Epic waterfalls • Heritage pubs SPECIAL PUBLICATION • Great fishing March 11-12, 2017 • Wildflowers the EXPERIENCE THE PEOPLE & PLACES OF A LAST FRONTIER March 11-12, 2017 2 sevenwesttravelclub.com.au 3 Welcome to a world of wonders ON THE BIG SCREEN P4 Ancient landscapes of the Kimberley and the Pilbara ᔡ Glen Chidlow have starred in many films. Chief executive, Australia’s North West tourism BEACHES P8 NORTH WEST MAP P9 or us Sandgropers, NATIONAL PARKS P10 compass points play a MEET THE LOCALS P16 Stephen Scourfield at big part in establishing EVENTS P18 Python Pool in the Pilbara. our place in the world. WATERING HOLES P20 Firstly we come from BOOKS P22 FWA — that huge State that takes WILDFLOWERS P23 up almost one-third of mainland DRIVE ADVENTURES P24 Australia. GREAT FISHING P26 When travelling within our KIMBERLEY COAST P28 A wealth of themes State, we generally refer to two WATERFALLS P30 localities; you can go down The Great North West is ᔡ Stephen Scourfield Season. Waterfalls have been in south or you can head up north. a vast area with few full roar, with flows likely to last Each conjures up a distinct For Kimberley planning, he Great North West all dry season. expectation in terms of holiday accommodation and activities, people and amazing feels remote. It has been one of the biggest experience and it is in these go to australiasnorthwest.com landscapes and stories There are big wet seasons on record. pages that we outline the best of landscapes, epic Kununurra, in the East the Kimberley and Pilbara river systems, Kimberley, received double the Tranges that glow red in the rainfall if usually does within evening.
    [Show full text]