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Palynomorph and Palynofacies Assemblages of Neutral-Alkaline and Acid Lakes South of Norseman, Southern Western Australia
Scholars' Mine Masters Theses Student Theses and Dissertations Summer 2012 Palynomorph and palynofacies assemblages of neutral-alkaline and acid lakes south of Norseman, Southern Western Australia Lutfia Grabel Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Grabel, Lutfia, "Palynomorph and palynofacies assemblages of neutral-alkaline and acid lakes south of Norseman, Southern Western Australia" (2012). Masters Theses. 5209. https://scholarsmine.mst.edu/masters_theses/5209 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. PALYNOMORPH AND PALYNOFACIES ASSEMBLAGES OF NEUTRAL- ALKALINE AND ACID LAKES SOUTH OF NORSEMAN, SOUTHERN WESTERN AUSTRALIA by LUTFIA GRABEL A THESIS Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN GEOLOGY 2012 Approved by Francisca E. Oboh-Ikuenobe, Advisor Wan Yang Melanie R. Mormile iii ABSTRACT The Yilgarn Craton in Western Australia hosts hundreds of shallow ephemeral hypersaline lakes, the majority of which have acid to neutral pH values. As part of a multidisciplinary study of the evolution of hypersalinity and acidity in the region, three drill cores were studied for their palynofacies and palynomorph contents in order to characterize palynofloral response to environmental changes. Drill cores from two acid lakes, Prado Lake (PL1-09 and PL2-09) and Twin Lake West (TLW1-09), and the neutral-alkaline Gastropod Lake (GLE1-09) south of Norseman recovered Miocene to Holocene sediments of the Revenge and Polar Bear formations. -
Mining Dump Structures Reference List
MINING DUMP STRUCTURES UPDATE OCTOBER 2012 REFERENCE LIST COUNTRY PROJECT TYPE MAIN FUNCTION HEIGHT [m] YEAR Luzamba Tip Wall Processing 11,4 1992 Catoca I Dump wall Processing 19,0 1995 Catoca II Dump wall Processing 16,0 1995 Catoca Tip Wall Processing 10,5 1996 Angola Escom Mining Tip Wall Processing 11,0 2002 Catoca Phase 1 Tip Wall Processing 13,6 2006 Catoca Phase 2 Tip Wall Processing 13,0 2006 Jopro 004 – Consulmet Tip Wall Processing 9,0 2007 Consulmet 2 Tip Wall Processing 9,0 2008 Veladero Project Dump structure Processing 27,8 2005 Argentina Pirquitas Project Dump structure Processing 18,0 2009 Veladero Project - Plant Expansion 85 KTPD Dump structure Processing 28,5 2009 Eastern Deepdale Pocket/Abutment Dump Structure Processing 16,0 1980 Saxonvale Raw Coal Handling Plant Dump Structure Processing 12,0 1981 Rom Hopper Walls Pacific Coal - Tarong Dump Structure Processing 19,5 1982 Boundary Hill Inpit Dump Wall - Dump Structure Processing 7,8 1982 Load Out Structure - Kangaroo Island Dump Structure Processing 6,0 1982 Mt. Tom Price Dump Structure - - 1982 Boundary Hill Inpit Dump Wall #2 Dump Structure Processing 8,0 1983 Kress Tipping Platform Stage I Dump Structure Processing 4,9 1984 Paddington Gold Project Dump Structure Processing 14,3 1984 Cork Tree Well Gold Mine Dump Wall Dump Structure Processing - 1985 Dump Wall - Cue Dump Structure Processing 8,3 1986 Telfer Mine Dump Structure Processing - 1986 Howick Colliery Temp Dump Wall Dump Structure Processing 8,4 1986 Wiluna Mine Dump Wall Dump Structure Processing - 1986 -
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. -
Resources and Energy Quarterly June 2020
10.1 Summary Figure 10.1: US dollar gold price and real US 10-Year Treasury yield . Due to the COVID-19 pandemic and its impacts, the gold price is 2,000 -1.0 forecast to reach an 8-year high, averaging about US$1,630 an ounce 1,800 -0.5 in 2020. An expected global economic rebound is projected to see the 1,600 0.0 price slide to around US$1,510 an ounce in 2022. 1,400 0.5 . Australia’s gold mine production is forecast to reach a peak of 381 1,200 1.0 tonnes in 2021–22, as high prices encourage an expansion in 1,000 1.5 production. cent Per 800 2.0 . The value of Australia’s gold exports is forecast to reach a record $32 billion in 2020–21, driven by higher prices and export volumes, before ounce troy a US$ 600 2.5 declining to $30 billion in 2021–22, as gold prices ease back. 400 3.0 200 3.5 10.2 Prices Jun–04 Jun–08 Jun–12 Jun–16 Jun–20 Gold prices rose strongly in the first half of 2020 US$ gold price Real US 10 Year Treasury bond yield (inverted, rhs) The London Bullion Market Association (LBMA) gold price has risen by 14 per cent so far in 2020, to US$1,727 an ounce on 17 June 2020 — well Source: Bloomberg (2020) above the average of US$1,479 an ounce in the second half of 2019. The US dollar gold price reached a seven and a half year high of US$1,748 an The LBMA gold price is estimated to average US$1,630 an ounce in 2020, ounce on 20 May 2020, benefitting from its status as a safe haven asset an increase of 17 per cent on 2019 (Figure 10.2). -
A Case Study of Newmont Boddington Gold Mine in Western Australia
Mine Closure 2012 — A.B. Fourie and M. Tibbett (eds) © 2012 Australian Centre for Geomechanics, Perth, ISBN 978-0-9870937-0-7 doi:10.36487/ACG_rep/1208_24_Amoah Long term closure planning for an evolving mine site – a case study of Newmont Boddington Gold Mine in Western Australia K. De Sousa Newmont Asia Pacific, Australia N. Amoah Newmont Asia Pacific, Australia Abstract Newmont Boddington Gold (NBG) mine is located 12 km northwest of the town of Boddington and about 120 km southeast of Perth in Western Australia (WA). Open pit mining of an oxide gold resource commenced at the operations in 1987. In 2008, NBG undertook an expansion program to increase future gold production to one million ounces per annum, potentially becoming the largest gold mine in Australia. Critical to the life cycle of such a large mining operation is the need to ensure that mine closure is well planned in advance and consistently managed throughout operation to minimise future liabilities. For example, the large quantities of waste (waste rock estimated to be over one billion tonnes over the life of the mine), vast open pits and areas for tailings storage and site operational facilities, geographically and ecologically sensitive location and socio-economic issues will all become significant legacy factors during mine closure and post closure stages. To mitigate closure liabilities, Newmont’s internal guidelines have strict requirements for the development and review of closure plans at all stages of mine life with annual analyses of closure liability costs. This is to ensure consistency with life of mine (LOM) plans, changes in operations, stakeholder expectations, regulatory requirements etc. -
Boddington Gold Mine - Extended Basement Operation and Changes to Existing Environmental Conditions
Boddington gold mine - Extended basement operation and changes to existing environmental conditions Worsley Alumina Pty Ltd Report and recommendations of the Environmental Protection Authority Environmental Protection Authority Perth, Western Australia Bulletin 850 April 1997 ISBN. 0 7309 8027 8 ISSN. 1030 - 0120 Summary This report is to provide Environmental Protection Authority (EPA) advice and recommendations to the Minister for the Environment on the environmental factors relevant to a proposal by Worsley Alumina Ply Ltd (Worsley), through the Boddington Gold Mine (BGM) joint venture, to modify the approvals relating to the company's existing mining operations and to mine basement ore in the same location as Worsley's Boddington Gold Mine. The proposal envisages substantial extension of basement ore mining, the mining of minor oxide ore deposits outside the existing mining area, the construction of an additional residue disposal area, an increase in ore processing and the release of excess water to the Hotham River and Thirty-Four Mile Brook. It is the EPA's opinion that the following are the environmental factors relevant to the proposal: a) declared rare flora, priority flora and vegetation communities; b) threatened fauna, specially protected fauna and priority fauna; c) water resource quality; d) water resource quantity; e) gaseous emissions including greenhouse gases and odours; f) System 6 recommendation area C42 (Duncan MPA); g) landform; and h) mechanisms for environmental management. The EPA is of the view that the proposal should be subject to the environmental conditions which cunently apply to the existing gold mine except where the following recommendations or procedures supersede those conditions. -
Trading Partners: Tectonic Ancestry of Southern Africa and Western Australia, In
Precambrian Research 224 (2013) 11–22 Contents lists available at SciVerse ScienceDirect Precambrian Research journa l homepage: www.elsevier.com/locate/precamres Trading partners: Tectonic ancestry of southern Africa and western Australia, in Archean supercratons Vaalbara and Zimgarn a,b,∗ c d,e f g Aleksey V. Smirnov , David A.D. Evans , Richard E. Ernst , Ulf Söderlund , Zheng-Xiang Li a Department of Geological and Mining Engineering and Sciences, Michigan Technological University, Houghton, MI 49931, USA b Department of Physics, Michigan Technological University, Houghton, MI 49931, USA c Department of Geology and Geophysics, Yale University, New Haven, CT 06520, USA d Ernst Geosciences, Ottawa K1T 3Y2, Canada e Carleton University, Ottawa K1S 5B6, Canada f Department of Earth and Ecosystem Sciences, Division of Geology, Lund University, SE 223 62 Lund, Sweden g Center of Excellence for Core to Crust Fluid Systems, Department of Applied Geology, Curtin University, Perth, WA 6845, Australia a r t i c l e i n f o a b s t r a c t Article history: Original connections among the world’s extant Archean cratons are becoming tractable by the use of Received 26 April 2012 integrated paleomagnetic and geochronologic studies on Paleoproterozoic mafic dyke swarms. Here we Received in revised form ∼ report new high-quality paleomagnetic data from the 2.41 Ga Widgiemooltha dyke swarm of the Yil- 19 September 2012 garn craton in western Australia, confirming earlier results from that unit, in which the primary origin Accepted 21 September 2012 of characteristic remanent magnetization is now confirmed by baked-contact tests. The correspond- Available online xxx ◦ ◦ ◦ ing paleomagnetic pole (10.2 S, 159.2 E, A95 = 7.5 ), in combination with newly available ages on dykes from Zimbabwe, allow for a direct connection between the Zimbabwe and Yilgarn cratons at 2.41 Ga, Keywords: Paleomagnetism with implied connections as early as their cratonization intervals at 2.7–2.6 Ga. -
EAST YILGARN GEOSCIENCE DATABASE, 1:100 000 GEOLOGY of the LEONORA– LAVERTON REGION, EASTERN GOLDFIELDS GRANITE–GREENSTONE TERRANE — an EXPLANATORY NOTE by M
REPORT EAST YILGARN GEOSCIENCE DATABASE 84 1:100 000 GEOLOGY OF THE LEONORA–LAVERTON REGION EASTERN GOLDFIELDS GRANITE–GREENSTONE TERRANE — AN EXPLANATORY NOTE by M. G. M. Painter, P. B. Groenewald, and M. McCabe GEOLOGICAL SURVEY OF WESTERN AUSTRALIA REPORT 84 EAST YILGARN GEOSCIENCE DATABASE, 1:100 000 GEOLOGY OF THE LEONORA– LAVERTON REGION, EASTERN GOLDFIELDS GRANITE–GREENSTONE TERRANE — AN EXPLANATORY NOTE by M. G. M. Painter, P. B. Groenewald, and M. McCabe Perth 2003 MINISTER FOR STATE DEVELOPMENT Hon. Clive Brown MLA DIRECTOR GENERAL, DEPARTMENT OF INDUSTRY AND RESOURCES Jim Limerick DIRECTOR, GEOLOGICAL SURVEY OF WESTERN AUSTRALIA Tim Griffin REFERENCE The recommended reference for this publication is: PAINTER, M. G. M., GROENEWALD, P. B., and McCABE, M., 2003, East Yilgarn Geoscience Database, 1:100 000 geology of the Leonora–Laverton region, Eastern Goldfields Granite–Greenstone Terrane — an explanatory note: Western Australia Geological Survey, Report 84, 45p. National Library of Australia Cataloguing-in-publication entry Painter, M. G. M. East Yilgarn Geoscience Database, 1:100 000 geology of the Leonora–Laverton region, Eastern Goldfields Granite–Greenstone Terrane — an explanatory note Bibliography. ISBN 0 7307 5739 0 1. Geology — Western Australia — Eastern Goldfields — Databases. 2. Geological mapping — Western Australia — Eastern Goldfields — Databases. I. Groenewald, P. B. II. McCabe, M., 1965–. III. Geological Survey of Western Australia. IV. Title. (Series: Report (Geological Survey of Western Australia); 84). 559.416 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. -
GSA TODAY North-Central, P
Vol. 9, No. 10 October 1999 INSIDE • 1999 Honorary Fellows, p. 16 • Awards Nominations, p. 18, 20 • 2000 Section Meetings GSA TODAY North-Central, p. 27 A Publication of the Geological Society of America Rocky Mountain, p. 28 Cordilleran, p. 30 Refining Rodinia: Geologic Evidence for the Australia–Western U.S. connection in the Proterozoic Karl E. Karlstrom, [email protected], Stephen S. Harlan*, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 Michael L. Williams, Department of Geosciences, University of Massachusetts, Amherst, MA, 01003-5820, [email protected] James McLelland, Department of Geology, Colgate University, Hamilton, NY 13346, [email protected] John W. Geissman, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, [email protected] Karl-Inge Åhäll, Earth Sciences Centre, Göteborg University, Box 460, SE-405 30 Göteborg, Sweden, [email protected] ABSTRACT BALTICA Prior to the Grenvillian continent- continent collision at about 1.0 Ga, the southern margin of Laurentia was a long-lived convergent margin that SWEAT TRANSSCANDINAVIAN extended from Greenland to southern W. GOTHIAM California. The truncation of these 1.8–1.0 Ga orogenic belts in southwest- ern and northeastern Laurentia suggests KETILIDEAN that they once extended farther. We propose that Australia contains the con- tinuation of these belts to the southwest LABRADORIAN and that Baltica was the continuation to the northeast. The combined orogenic LAURENTIA system was comparable in -
Early Diagenesis by Modern Acid Brines in Western Australia and Implications for the History of Sedimentary Modification on Mars
EARLY DIAGENESIS BY MODERN ACID BRINES IN WESTERN AUSTRALIA AND IMPLICATIONS FOR THE HISTORY OF SEDIMENTARY MODIFICATION ON MARS BRENDA B. BOWEN Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907 USA e-mail: [email protected], KATHLEEN C. BENISON Department of Earth and Atmospheric Sciences, Central Michigan University, Mt. Pleasant, Michigan 48859 USA AND STACY STORY Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907 USA ABSTRACT: Mineralogical and geochemical data collected from multiple sites on Mars suggest that acid saline surface waters and groundwater existed there in the past. The geologic context and sedimentology suggest that these acid saline waters were associated with groundwater-fed ephemeral lakes. Ephemeral acid saline lakes in southern Western Australia (WA) are some of the few known natural systems that have the same combination of extreme acid brine chemistry and lacustrine depositional setting as is observed on Mars. Thus, the WA acid saline environments provide a modern analog for understanding past depositional and diagenetic processes that may have occurred on Mars. Here, we examine surface sediments and sedimentary rocks that have been in contact with acid (pH down to ;1.5) and saline brines (total dissolved solids up to ;32%) in southern Western Australia. Through sedimentological, mineralogical, geochemical, and petrographic analyses, we identify the impacts of early diagenesis in and adjacent to eight acid saline lakes and evaluate the processes that have been important in creating these deposits. The combination of extreme chemistry, spatial variability, arid climate, and reworking by winds and floods contributes to make spatially complex depositional products that are a combination of siliciclastics and chemical sediments. -
Newmont Boddington Gold Closure Plan
Newmont Boddington Gold Closure Plan M70/21, M70/22, M70/23, M70/24, M70/25, M70/564, M70/799, M70/1031, ML264SA(1), ML264SA(2), G70/215, G70/218, G70/219, L70/28, L70/95, L70/96 Submission Date December 2012 Version Number CR35945 Contact Details Javier Brodalka, Environment Manager Phone: (08) 9883 4251 Email: [email protected] Date Revision Description of Originator Reviewer(s) Approval Revision December ‐ ‐ K. De Sousa M. Durack, S. J. Brodalka 2012 Myles, R. Kok, A. James Newmont Boddington Gold – Closure Plan Closure Plan Checklist No. Mine Closure Plan Checklist Y/N/NA Section Comments 1 Has the Checklist been endorsed by a senior Y Checklist representative within the tenement holder/ operating company? 2 How many copies were submitted to DMP? Hard copies = 2 Electronic copies = 1 Cover Page, Table of Contents 3 Does the cover page include: Y Cover Page Project title Company name Contact details (including telephone numbers and email addresses) Document ID and version number Date of submission 4 Has a Table of Contents been provided? Y Table of Contents Scope and Project Summary 5 State why the MCP is submitted. Y 1.2 6 Does the project summary include: Y Section 2 Land ownership details 2.2 Location of the project 2.1 Comprehensive site plans 2.4 Background information on the history 2.3 and status of the project Legal Obligations and Commitments 7 Has a consolidated summary or registers of Y Section 3 Appendices 1‐3 closure obligations and commitments been included? Data Collection and Analysis 8 Has information -
Three-Dimensional Computer-Based Gold Prospectivity Mapping Using Conventional Geographic Information Systems, Three-Dimensional
Three-Dimensional Computer-Based Gold Prospectivity Mapping using Conventional Geographic Information systems, Three- Dimensional Mine Visualization Software and Custom Built Spatial Analysis Tools Eduardo Videla1 and Carl M. Knox-Robinson2 Centre for Teaching and Research in Strategic Mineral Deposits Department of Geology and Geophysics The University of Western Australia NEDLANDS WA 6907, Australia [email protected] [email protected] Presented at the second annual conference of GeoComputation ‘97 & SIRC ‘97, University of Otago, New Zealand, 26-29 August 1997 Effective mineral exploration requires a detailed knowl- the research aims to identify potential continuations of edge of the factors and processes which result in the for- known ore bodies, and to attempt to locate new prospec- mation of economic deposits. To apply this knowledge, a tive areas for gold mineralisation further to the south of sound three-dimensional understanding of the geology and the present goldfield. structure of a region is required. In most cases, surface The Wiluna goldfield comprises a region approximately geology can be mapped with a high degree of accuracy, 3km x 5km, and is situated in the northern part of the however, the geology at depth has to be inferred from Archaean Yilgarn Block of Western Australia, approximately geophysical methods, or through drilling programs, and is four kilometres south of the Wiluna townsite. The area therefore mapped at much lower spatial resolution. This has been mined for gold since the early 1900s, and pres- anisotropy in spatial-data quality, coupled with the scarcity ently comprises 11 open-cut and underground gold mines. of three dimensional geographic information systems (GIS), Geological information for the region includes detailed makes computer-based exploration at a camp- or district- surface mapping and over 6,000 unevenly distributed drill scale very difficult.