West African Goldfields
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Arend J Hoogervorst1 B.Sc.(Hons), Mphil., Pr.Sci
Audits & Training Eagle Environmental Arend J Hoogervorst1 B.Sc.(Hons), MPhil., Pr.Sci. Nat., MIEnvSci., C.Env., MIWM Environmental Audits Undertaken, Lectures given, and Training Courses Presented2 A) AUDITS UNDERTAKEN (1991 – Present) (Summary statistics at end of section.) Key ECA - Environmental Compliance Audit EMA - Environmental Management Audit EDDA -Environmental Due Diligence Audit EA- External or Supplier Audit or Verification Audit HSEC – Health, Safety, Environment & Community Audit (SHE) – denotes safety and occupational health issues also dealt with * denotes AJH was lead environmental auditor # denotes AJH was contracted specialist local environmental auditor for overseas environmental consultancy, auditing firm or client + denotes work undertaken as an ICMI-accredited Lead Auditor (Cyanide Code) No of days shown indicates number of actual days on site for audit. [number] denotes number of days involved in audit preparation and report write up. 1991 *2 day [4] ECA - AECI Chlor-Alkali Plastics, Umbogintwini, KwaZulu-Natal, South Africa. November 1991. *2 day [4] ECA - AECI Chlor-Alkali Plastics- Environmental Services, Umbogintwini, KwaZulu-Natal, South Africa. November 1991. *2 Day [4] ECA - Soda Ash Botswana, Sua Pan, Botswana. November 1991. 1992 *2 Day [4] EA - Waste-tech Margolis, hazardous landfill site, Gauteng, South Africa. February 1992. *2 Day [4] EA - Thor Chemicals Mercury Reprocessing Plant, Cato Ridge, KwaZulu-Natal, South Africa. March 1992. 2 Day [4] EMA - AECI Explosives Plant, Modderfontein, Gauteng, South Africa. March 1992. *2 Day [4] EMA - Anikem Water Treatment Chemicals, Umbogintwini, KwaZulu-Natal, South Africa. March 1992. *2 Day [4] EMA - AECI Chlor-Alkali Plastics Operations Services Group, Midland Factory, Sasolburg. March 1992. *2 Day [4] EMA - SA Tioxide factory, Umbogintwini, KwaZulu-Natal, South Africa. -
A Review of the Birimian Supergroup- and Tarkwaian Group-Hosted Gold Deposits of Ghana
177 A review of the Birimian Supergroup- and Tarkwaian Group-hosted gold deposits of Ghana Albertus J. B. Smith1,2*, George Henry1,2 and Susan Frost-Killian3 1 DST-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis, Department of Geology, University of Johannesburg, Auckland Park, 2006, South Africa. *Corresponding author e-mail address: [email protected] 2 Palaeoproterozoic Mineralisation Research Group, Department of Geology, University of Johannesburg, Auckland Park, 2006, South Africa 3 The MSA Group, 20B Rothesay Avenue, Craighall Park, 2196, South Africa DOI: 10.18814/epiiugs/2016/v39i2/95775 Ghana is the largest producer of gold in West Africa, veins. The vein- and sulphide-hosted gold is strongly a region with over 2,500 years of history with regards to associated with deformational fabrics formed by the gold production and trade. Modern exploration for and Eburnean extensional and compressional events, mining of gold in Ghana dates from 1874 with the respectively, suggesting that disseminated sulphide establishment of the British Gold Coast Colony, which mineralisation predates quartz vein-hosted was followed in 1957 by the independence of Ghana and mineralisation. The fluid from which the gold precipitated increased gold production since the early 1980s through is believed to have been of metamorphic origin and Ghana’s Economic Recovery Plan. At the time of writing, carbon dioxide (CO2) dominated, with lesser water (H2O) gold production (108.2 tonnes or 3.48 million ounces and nitrogen (N2) and minor methane (CH4). Gold [Moz] in 2014) accounted for approximately one-third precipitation was probably caused by decrease in of Ghana’s export revenues, with 36% of gold production pressure, temperature and CO2-H2O immiscibility, at coming from small-scale mining. -
Research Article Pan-African Paleostresses and Reactivation of the Eburnean Basement Complex in Southeast Ghana (West Africa)
Hindawi Publishing Corporation Journal of Geological Research Volume 2012, Article ID 938927, 15 pages doi:10.1155/2012/938927 Research Article Pan-African Paleostresses and Reactivation of the Eburnean Basement Complex in Southeast Ghana (West Africa) Mahaman Sani Tairou,1 Pascal Affaton,2 Solomon Anum,3 and Thomas Jules Fleury2 1 D´epartement de G´eologie, Facult´e des Sciences, Universit´edeLom´e, BP 1515, Lom´e, Togo 2 Aix-Marseille Universit´e, CNRS, IRD, CEREGE UMR34, 13545 Aix en Provence Cedex 04, France 3 Geological Survey Department, Koforidua Eastern Region, P.O. Box 672, Koforidua, Ghana Correspondence should be addressed to Mahaman Sani Tairou, [email protected] Received 28 March 2012; Revised 18 May 2012; Accepted 25 May 2012 Academic Editor: Quan-Lin Hou Copyright © 2012 Mahaman Sani Tairou et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. This faulting tectonics analysis concerns the southernmost segment of the Dahomeyide Orogen and the West-African craton eastern margin in southeast Ghana. The analysis of strike-slip faults in the frontal units of the Dahomeyide Belt indicates that four distinct compressive events (NE-SW, ENE-WSW to E-W, ESE-WNW to SE-NW and SE-NW to SSE-NNW) originated the juxtaposition of the Pan-African Mobile Zone and the West-African craton. These paleostress systems define a clockwise rotation of the compressional axis during the structuring of the Dahomeyide Orogen (650–550 Ma). The SE-NW and SSE-NNW to N-S compressional axes in the cratonic domain and its cover (Volta Basin) suggest that the reactivation of the eastern edge of the West African craton is coeval with the last stages of the Pan-African tectogenesis in southeast Ghana. -
Ore Genesis and Modelling of the Sadiola Hill Gold Mine, Mali Geology Honours Project
ORE GENESIS AND MODELLING OF THE SADIOLA HILL GOLD MINE, MALI GEOLOGY HONOURS PROJECT Ramabulana Tshifularo Student number: 462480 Supervisor: Prof Kim A.A. Hein Acknowledgements I would like to thank my supervisor, Prof. Kim Hein for giving me the opportunity to be part of her team and, for helping and motivating me during the course of the project. Thanks for your patience, constructive comments and encouragement. Thanks to my family and my friends for the encouragements and support. Table of contents Abstract……………………………………………………………………………………..i Chapter: 1 1.1 Introduction……………………………………………………..........................................1 1.2 Location and Physiography……………………………………………………………...2 1.3 Aims and Objectives…………………………………………………………………….3 1.4 Abbreviations and acronyms…………………………………………………………….3 Chapter 2 2.1 Regional Geology………………………………………………………………………..4 2.1.1 Geology of the West African Craton…………………………………………………..4 2.1.2 Geology of the Kedougou-Kéniéba Inlier……………………………………………..5 2.2 Mine geology…………………………………………………………………………….6 Lithology………………………………………………………………………………8 Structure……………………………………………………………………………….8 Metamorphism………………………………………………………………………...9 Gold mineralisation and metallogenesis………………………………………………9 2.4 Previously suggested genetic models…………………………………………………..10 Chapter3: Methodology…………………………………………………………………....11 Chapter 4: Host rocks in drill core…......................................................................................13 4.1 Drill core description….........................................................................................................13 -
Provisional Programme
June 2016 DOWNLOADS PROVISIONAL PROGRAMME The provisional technical program was set during the first week in June, although the schedule of times and venues for 4th Announcement Circular presentations and posters will only be finalized mid- July. Currently, there are 4,824 accepted abstracts from over 5,200 submissions, of which 3087 are oral presentations and 1,737 are posters. These are divided between the three core topics, Geoscience in Society (31%), Geology in the Economy (24%) and Fundamental Geoscience (45%). There are between three and fifteen major symposia or general sessions per theme of which there are 48. There are nine plenary presentations, all of which are directed at themes of particular current relevance in the global earth sciences. See the website. Topics include: Formation of continental crust Science and the professions: service to society Climate and human evolution The mining industry and society Shale gas - the technical challenges Extraction technologies and the life cycle of metals Earthquakes in Africa Palaeobiology from fossil bones Under the core theme, Geoscience in Society, there are a considerable number of geoheritage and geoconservation presentations. Climate change is a high interest topic (as predicted!). Communication to the public sector is addressed, as is mapping of Africa and the world. Geohazards, engineering geology and environmental geoscience all SOCIAL MEDIA have strong support. Geoeducation at secondary and tertiary level is well represented. There is considerable interest in professionalism in the geosciences and geoethics. All of these topics are typically under-represented in conferences world-wide, and anyone interested in these subjects should definitely have a close look at this part of the program. -
Year End 2020
AngloGold Ashanti Limited (Incorporated in the Republic of South Africa) Reg. No. 1944/017354/06 ISIN: ZAE000043485 – JSE share code: ANG CUSIP: 035128206 – NYSE share code: AU (“AngloGold Ashanti” or “AGA” or the “Company”) Report for the six months and year ended 31 December 2020 Johannesburg, 22 February 2021 - AngloGold Ashanti is pleased to provide its financial and operational update for the six months and year ended 31 December 2020. • Added Ore Reserve of 6.1Moz on a gross basis, 2.6Moz on a net basis, for a net increase of 10% year-on-year - reserve life ∧ increased to about 11 years • Free cash flow increased 485% year-on-year to $743m in 2020 – excluding asset sale proceeds – from $127m in 2019 • Free cash flow before growth capital up 124% year-on-year to $1,003m in 2020, from $448m in 2019 • Net cash inflow from operating activities increased 58% to $1,654m in 2020, from $1,047m in 2019 • Achieved 2020 full year guidance: Production of 3.047Moz in 2020, which includes COVID-19 impacts estimated at 140,000oz • All-in sustaining costs (AISC) margin from continuing operations rose to 40% in 2020, from 28% in 2019 • Profit from continuing operations increased 160% year-on-year to $946m in 2020, from $364m in 2019 • Adjusted EBITDA up 50% year-on-year to $2,593m in 2020, from $1,723m in 2019; highest since 2012 • Dividend increased more than fivefold to 48 US cents per share in 2020, from 9 US cents per share in 2019 • Adjusted net debt from continuing operations down by 62% year-on-year to $597m in 2020, from $1,581m in 2019; -
Anglogold Ashanti Holdings Plc Anglogold Ashanti Limited
Use these links to rapidly review the document TABLE OF CONTENTS Prospectus Supplement TABLE OF CONTENTS TABLE OF CONTENTS 3 Table of Contents Filed pursuant to Rule 424(b)(5) Registration Nos. 333-182712 and 333-182712-02 CALCULATION OF REGISTRATION FEE Amount of Registration Title of Each Class of Aggregate Securities to be Registered Offering Price Fee (1) 5.125% Notes due 2022 of AngloGold Ashanti Holdings plc $750,000,000 $85,950 Guarantee of AngloGold Ashanti Limited in connection with the 5.125% Notes due 2022 (2) — — (1) Calculated in accordance with Rule 457(r) under the Securities Act of 1933. (2) Pursuant to Rule 457(n) under the Securities Act of 1933, no separate fee is payable with respect to the guarantee of AngloGold Ashanti Limited in connection with the guaranteed debt securities. Prospectus Supplement to Prospectus dated July 17, 2012 GRAPHIC AngloGold Ashanti Holdings plc $750,000,000 5.125% notes due 2022 Fully and Unconditionally Guaranteed by AngloGold Ashanti Limited The 5.125% notes due 2022, or the "notes", will bear interest at a rate of 5.125% per year. AngloGold Ashanti Holdings plc, or "Holdings", will pay interest on the notes each February 1 and August 1, commencing on February 1, 2013. Unless Holdings redeems the notes earlier, the notes will mature on August 1, 2022. The notes will rank equally with Holdings' senior, unsecured debt obligations and the guarantee will rank equally with all other senior, unsecured debt obligations of AngloGold Ashanti Limited. Holdings may redeem some or all of the notes at any time and from time to time at the redemption price determined in the manner described in this prospectus supplement. -
The Geology of the Gold Deposits of Prestea Gold Belt of Ghana*
The Geology of the Gold Deposits of Prestea Gold Belt of Ghana* K. Dzigbodi-Adjimah and D. Nana Asamoah Dzigbodi-Adjimah, K. and Nana Asamoah, D., (2009), “The Geology of the Gold Deposits of Prestea Gold Belt of Ghana”, Ghana Mining Journal, Vol. 11, pp. 7 - 18. Abstract This paper presents the geology of the gold deposits along the Prestea gold belt of Ghana to assist exploration work for new orebodies along the belt. Prestea district is the third largest gold producer in West Africa after Obuasi and Tarkwa districts (over 250 metric tonnes Au during the last century). The gold deposits are structurally controlled and occur in a deep-seated fault or fissure zone that is regarded as the ore channel. This structure, which lies at the contact between metavolcanic and metasedimentary rocks in Birimian rocks, is more open (and contains more quartz lodes) at the southern end around Prestea than at Bogoso to the north. The gold deposits consist of the Quartz Vein Type, (QVT) and the Dis- seminated Sulphide Type (DST). The QVT orebodies, which generally carry higher Au grades, lie within a graphitic gouge in the fissure zones whilst the DST is found mostly in sheared or crushed rocks near the fissure zones. Deposits were grouped into three in terms of geographic location and state of development; The deposits south of Prestea are the least developed but have been extensively explored by Takoradi Gold Company. Those at Prestea have been worked exclusively as underground mines on QVT orebodies by Prestea Goldfields Limited and its forerunners; Ariston and Ghana Main Reef companies until 1998 whilst the deposits north of Prestea, which were first worked as surface mines (on DST orebodies) by Marlu Mines up to 1952, were revived by Billiton Bogoso Gold in 1990. -
Geochemistry of an Ultramafic-Rodingite Rock Association in the Paleoproterozoic Dixcove Greenstone Belt, Southwestern Ghana
Journal of African Earth Sciences 45 (2006) 333–346 www.elsevier.com/locate/jafrearsci Geochemistry of an ultramafic-rodingite rock association in the Paleoproterozoic Dixcove greenstone belt, southwestern Ghana Kodjopa Attoh a,*, Matthew J. Evans a,1, M.E. Bickford b a Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA b Department of Earth Sciences, Syracuse University, Syracuse, NY 13244, USA Received 11 January 2005; received in revised form 20 February 2006; accepted 2 March 2006 Available online 18 May 2006 Abstract Rodingite occurs in ultramafic rocks within the Paleoproterozoic (Birimian) Dixcove greenstone belt in southwestern Ghana. U–Pb analyses of zircons from granitoids intrusive into the greenstone belt constrain the age of the rodingite-ultramafic association to be older than 2159 Ma. The ultramafic complex consists of variably serpentinized dunite and harzburgite overlain by gabbroic rocks, which together show petrographic and geochemical characteristics consistent with their formation by fractional crystallization involving olivine and plagioclase cumulates. Major and trace element concentrations and patterns in the ultramafic–mafic cumulate rocks and associated plagiogranite are similar to rocks in ophiolitic suites. The rodingites, which occur as irregular pods and lenses, and as veins and blocks in the serpentinized zones, are characterized by high Al2O3 and CaO contents, which together with petrographic evidence indicate their formation from plagioclase-rich protoliths. The peridotites are highly depleted in REE and display flat, chondrite-normalized REE pat- terns with variable, but mostly small, positive Eu anomalies whereas the rodingites, which are also highly depleted, with overall REE contents from 0.04 to 1.2 times chondrite values, display distinct large positive Eu anomalies. -
The Mineral Industry of Mali in 1998
THE MINERAL INDUSTRY OF MALI By Philip M. Mobbs Gold was the most economically significant mineral the area encompassing the Kéniéba gold district and the commodity produced in Mali during 1998. Gold production exploitation permits at Loulo and Sadiola included Afko Corp. from the Sadiola Hill Mine, the Syama Mine, and artisanal Mali, a subsidiary of Afko Korea Inc., on a Kéniéba area production reached an estimated 25 metric tons. Mali was tied property and African Goldfields Corp., a subsidiary of African for third with Zimbabwe on the list of African gold producers, Selection Mining Corp. of Canada, on the Kofi and the Metedia after South Africa and Ghana. Despite 1998 being a difficult Est concessions. Exploration on the Djlimagara property year for mining companies to raise capital, gold exploration continued as Anglogold (42.5%) joined the venture of Barrick continued during the year in the Birimian Series greenstone Gold Corp. of Canada (42.5%) and the Government (15%). belts in the southern and southwestern parts of the country. Emerging Africa Gold (EAG) Inc. of Canada explored the The gross domestic product (GDP) of landlocked Mali was Mankouke West, the Kourou, and the Siribaya permits. The $2.5 billion in 1997, the latest year for which data are joint venture of Emerging African Gold (75%) and Geo-L of available. The agriculture sector contributed nearly 50% to the Russia (25%) held the Koulo permit. Golden Eagle Mining GDP. Gold accounted for about 36% of the country’s 1997 Ltd. was earning a percentage of African Selection Mining’s exports of $562 million. -
Geometry and Genesis of the Giant Obuasi Gold Deposit, Ghana
Geometry and genesis of the giant Obuasi gold deposit, Ghana Denis Fougerouse, BSc, MSc This thesis is presented for the degree of Doctor of Philosophy. Centre for Exploration Targeting School of Earth and Environment The University of Western Australia July 2015 Supervisors: Dr Steven Micklethwaite Dr Stanislav Ulrich Dr John M Miller Professor T Campbell McCuaig ii "It never gets easier, you just go faster" Gregory James LeMond iv Abstract Abstract The supergiant Obuasi gold deposit is the largest deposit hosted in the Paleoproterozoic Birimian terranes of West Africa (62 Moz, cumulative past production and resources). The deposit is hosted in Kumasi Group sedimentary rocks composed of carbonaceous phyllites, slates, psammites, and volcaniclastic rocks intruded by different generations of felsic dykes and granites. In this study, the deformation history of the Obuasi district was re-evaluated and a three stage sequence defined based on observations from the regional to microscopic scale. The D1Ob stage is weakly recorded in the sedimentary rocks as a layer-parallel fabric. The D2Ob event is the main deformation stage and corresponds to a NW-SE shortening, involving tight to isoclinal folding, a pervasive subvertical S2Ob cleavage striking NE, as well as intense sub-horizontal stretching. Finally, a N-S shortening event (D3Ob) formed an ENE-striking, variably dipping S3Ob crenulation cleavage. Three ore bodies characteristic of the three main parallel mineralised trends were studied in details: the Anyankyerem in the Binsere trend; the Sibi deposit in the Gyabunsu trend, and the Obuasi deposit in the main trend. In the Obuasi deposit, two distinct styles of gold mineralisation occur; (1) gold-bearing sulphides, dominantly arsenopyrite, disseminated in metasedimentary rocks and (2) native gold hosted in quartz veins up to 25 m wide. -
Insights on the Crustal Evolution of the West African (Raton from Hf Isotopes in Detrital Zircons from the Anti-Atlas Belt
Insights on the crustal evolution of the West African (raton from Hf isotopes in detrital zircons from the Anti-Atlas belt a b c d b ]acobo Abati ,., Abdel Mohsine Aghzer , 1 , Axel Gerdes , ,2, Nasser Ennih • Departamento de Petrologfa y Geoquimica and Instituto de Geologia Econ6mica, Universidad Comp!utense/Consejo Superior de Investigaciones Cientificas. 28040 Madrid, Spain b Departament Ge% gie. Faculte des Sciences, Universite Chouaib Doukkali, EIJadida. Morocco c InstitutftirGeowissenschaften. Minera/ogie, Goethe-UniversityFrankfurt (GUF),Altenhoferallee 1. D-60438 Frankfurt amMain, Gennany d Department of Earth Sciences, SteIIenbosch University.Private BagXl. Matieland 7602, South Africa ABSTRACT The Lu-Hf isotopic composition of detrital zircons has been used to investigate the crustal evolution of the northern part of the West African (raton (WAC). The zircons were separated from six samples of siliciclastic sedimentary rocks from the main Neoproterozic stratigraphic units of the Anti-Atlas belt, from the SiIWa and Zenaga inliers. The data suggest that the north part of the WAC formed during three cycles of juvenile crust formation with variable amount of reworking of older crust. The younger group of zircons, with a main population clustering around 610 Ma, has a predominant juvenile character and Keyworili: evidences of moderate mixing with Paleoproterozoic and Neoarchean crust, which supports that most Anti-Atlas belt igneous and metamorphic rocks where zircons originally crystallized were formed in an ensialic mag Morocco Hfisotopes matic arc environment. The group of zircons in the age range 1.79-2.3 Ca corresponds to the major crust Detrital zircon forming event in the WAC: the Eburnian orogeny.