A Review of the Birimian Supergroup- and Tarkwaian Group-Hosted Gold Deposits of Ghana
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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. -
Engineering & Mining Journal
Know-How | Performance | Reliability With MineView® and SmartFlow® Becker Mining Systems offers two comprehensive and scalable data management solutions for your Digital Mine. MineView® is a powerful state-of-the-art 3D SCADA system, that analyses incoming data from various mine equipment and visualises it in a 3D mine model. SmartFlow® takes Tagging & Tracking to a new level: collected asset data is centrally processed and smart software analytics allow for process optimization and improved safety. MINEVIEW BECKER MINING SYSTEMS AG We have been at the forefront of technology in Energy Distribution, Automation, Communication, Transportation and Roof Support since 1964. Together with our customers we create and deliver highest quality solutions and services to make operations run more profi tably, reliably and safely. For more information go to www.becker-mining.com/digitalmine Becker Mining is a trademark of Becker Mining Systems AG. © 2018 Becker Mining Systems AG or one of its affi liates. DECEMBER 2018 • VOL 219 • NUMBER 12 FEATURES China’s Miners Promote New Era of Openness and Cooperation Major reforms within the mining sector and the government will foster green mines at home and greater investment abroad ....................................42 Defeating the Deleterious Whether at the head of a circuit or scavenging tailings, today’s flotation innovations address challenges presented by declining grades, rising costs and aging plants ..................................................................................52 Staying on Top of -
Cloth, Commerce and History in Western Africa 1700-1850
The Texture of Change: Cloth, Commerce and History in Western Africa 1700-1850 The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Benjamin, Jody A. 2016. The Texture of Change: Cloth, Commerce and History in Western Africa 1700-1850. Doctoral dissertation, Harvard University, Graduate School of Arts & Sciences. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:33493374 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The Texture of Change: Cloth Commerce and History in West Africa, 1700-1850 A dissertation presented by Jody A. Benjamin to The Department of African and African American Studies in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of African and African American Studies Harvard University Cambridge, Massachusetts May 2016 © 2016 Jody A. Benjamin All rights reserved. Dissertation Adviser: Professor Emmanuel Akyeampong Jody A. Benjamin The Texture of Change: Cloth Commerce and History in West Africa, 1700-1850 Abstract This study re-examines historical change in western Africa during the eighteenth and nineteenth centuries through the lens of cotton textiles; that is by focusing on the production, exchange and consumption of cotton cloth, including the evolution of clothing practices, through which the region interacted with other parts of the world. It advances a recent scholarly emphasis to re-assert the centrality of African societies to the history of the early modern trade diasporas that shaped developments around the Atlantic Ocean. -
Quarter 1 2020 GROUP - Operating and Financial Review
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”) Market update report for the quarter ended 31 March 2020 Johannesburg, 11 May 2020 - AngloGold Ashanti is pleased to provide an operational update for the quarter ended 31 March 2020. • COVID-19 impact to production limited due to early management intervention and portfolio diversification at 11,000oz in Q1 2020 • Production of 716,000oz, supported by strong performances from Kibali, Geita and Iduapriem • All-in sustaining costs (AISC) of $1,047/oz up 4% year-on-year; AISC margin improved to 34%, up from 22% in Q1 2019 • Adjusted EBITDA up 54% year-on-year to $473m; Adjusted net debt to Adjusted EBITDA improves to 0.85 times • Free cash flow before growth capital increased 231% year-on-year to $94m; Cash flow from operating activities up 227% to $219m • Liquidity of $2bn at 31 March 2020; Settled $700m principal and final coupon on 10-year bond; Secured $1bn standby facility in April 2020 • Obuasi Phase 2 ramp-up completion expected towards end Q1 2021 due to equipment delivery delay; Colombia studies now seen in Q1 2021 • Critical spares inventories now average four months across sites to mitigate possible COVID-19 disruptions • AngloGold Ashanti involved in important humanitarian efforts in the fight against the COVID-19 pandemic • Sale processes for SA portfolio and Sadiola making steady progress; Decision taken -
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. -
Imams of Gonja the Kamaghate and the Transmission of Islam to the Volta Basin Les Imams De Gonja Et Kamaghate Et La Transmission De L’Islam Dans Le Bassin De La Volta
Cahiers d’études africaines 205 | 2012 Varia Imams of Gonja The Kamaghate and the Transmission of Islam to the Volta Basin Les imams de Gonja et Kamaghate et la transmission de l’islam dans le bassin de la Volta Andreas Walter Massing Electronic version URL: https://journals.openedition.org/etudesafricaines/16965 DOI: 10.4000/etudesafricaines.16965 ISSN: 1777-5353 Publisher Éditions de l’EHESS Printed version Date of publication: 15 March 2012 Number of pages: 57-101 ISBN: 978-2-7132-2348-8 ISSN: 0008-0055 Electronic reference Andreas Walter Massing, “Imams of Gonja”, Cahiers d’études africaines [Online], 205 | 2012, Online since 03 April 2014, connection on 03 May 2021. URL: http://journals.openedition.org/etudesafricaines/ 16965 ; DOI: https://doi.org/10.4000/etudesafricaines.16965 © Cahiers d’Études africaines Andreas Walter Massing Imams of Gonja The Kamaghate and the Transmission of Islam to the Volta Basin With this article I will illustrate the expansion of a network of Muslim lineages which has played a prominent role in the peaceful spread of Islam in West Africa and forms part of the Diakhanke tradition of al-Haji Salim Suware from Dia1. While the western branch of the Diakhanke in Senegambia and Guinea has received much attention from researchers2, the southern branch of mori lineages with their imamates extending from Dia/Djenne up the river Bani and its branches have been almost ignored. It has established centres of learning along the major southern trade routes and in the Sassandra- Bandama-Comoë-Volta river basins up to the Akan frontier3. The Kamaghate imamate has been established with the Gonja in the Volta basin but can be traced back to the Jula/Soninke of Begho, Kong, Samatiguila, Odienne and ultimately to the region of Djenne and Dia. -
I U R E P Orientation Phase R E P O R T G H a 1\F A
International Atomic Energy Agency DRAFT I U R E P ORIENTATION PHASE REPORT G H A 1\F A MR. JEW-PAUL GUELPA MR. WOLFRAM TO GEL December 1982 DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document UTTEENATIOITAL URANIBK RESOURCES. EVALUATION PROJECT -IURBP- IUSSP ORIENTATION FHAS3 MISSION REPORT BSPTOLIC OP GHANA Dr. J.Fo Guelpa December, 1982. Dro "W. Vogel PREFACE mission, was undertaken, by two consultants, Dr. JoP. Guelpa and Dr. W, Vogel, both, commenced the investigations in Ghana on 5th November, 1982 and completed their work on 16th December, 1982. A total of three days was spent in the field by the consultants* 1. Terse of Ilsferenie .. ., 5 2. General Geography .. .. 4 3. Clirate .. ... 7 4. Population aril I-lain Cities .. .. 9 5. Administrative Regions .. .. S- 6. Official Language, Public Holidays and System of Eeasureaervfc .. ., ll 7. Transport and Consronicatipn .. .. 11 8. Available "aps and Air Photographs .. 12 c. ITCK UB^ITK ICIITIKG n; GH^A • .. .. 13 1. Overview .. .. 13 2. Dianond .. ,. 15 3. Gold .. .. 17 . • 4. Batfzite .. • .. 'IS 5. Manganese .. .. 18 D. IBGI3LATICH ON UEAiTITJK EXPLCHASCtf AlTD XIIIDTG 19 3. KATIOKAL CAFACITI PCS URAFIUI! SXPLORATIC1T AIT3 D272L0P- 1. Ghana Atoiaic Energy CoEE&ssion .. 20 2. Ghana Geological Survey .. .. 22 3. Universities .. .. 24 F. GnOL'OGIC/i 3ST.12r.7 . .. 25 1. Introduction .. ' .. 25 2. The 'vest African Shield Area .. .. 27 2.1 Birician Systec .. .. 27 2.2 Eburnean Granites .. .. 32 2.3 Taria-;aian System .. .. 35 3. Sie Kobile Belt ... .. 3S 3.1 Dahoneyan System •• •• 35 3.2 ?cgc Series •• •• 4C 3 .3 Buen. -
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. -
Sa˜O Luıs Craton and Gurupi Belt (Brazil)
Sa˜o Luı´s Craton and Gurupi Belt (Brazil): possible links with the West African Craton and surrounding Pan-African belts E. L. KLEIN1,2 & C. A. V. MOURA3 1CPRM (Companhia de Pesquisa de Recursos Minerais)/Geological Survey of Brazil, Av. Dr. Freitas, 3645, Bele´m-PA, CEP 66095-110, Brazil (e-mail: [email protected]) 2Researcher at CNPq (Conselho Nacional de Desenvolvimento Cientı´fico e Tecnolo´gico) 3Laborato´rio de Geologia Isoto´pica/Para´-Iso, Universidade Federal do Para´, Centro de Geocieˆncias, CP 1611, Bele´m-PA, Brazil, CEP 66075-900 Abstract: The Sa˜o Luı´s Craton and the Palaeoproterozoic basement rocks of the Neoproterozoic Gurupi Belt in northern Brazil are part of an orogen having an early accretionary phase at 2240– 2150 Ma and a late collisional phase at 2080 + 20 Ma. Geological, geochronological and isotopic evidence, along with palaeogeographic reconstructions, strongly suggest that these Brazilian terrains were contiguous with the West African Craton in Palaeoproterozoic times, and that this landmass apparently survived subsequent continental break-up until its incorporation in Rodinia. The Gurupi Belt is an orogen developed in the southern margin of the West African–Sa˜o Luı´s Craton at c. 750–550 Ma, after the break up of Rodinia. Factors such as present-day and possible past geographical positions, the timing of a few well-characterized events, the structural polarity and internal structure of the belt, in addition to other indirect evidence, all favour correlation between the Gurupi Belt and other Brasiliano/Pan-African belts, especially the Me´dio Coreau´ domain of the Borborema Province and the Trans-Saharan Belt of Africa, despite the lack of proven physical links between them. -
Asanko Report
Technical Report on Asanko Gold Project, Ashanti Region Ghana 1 An Independent Qualified Persons’ Report On ASANKO GOLD MINE in the Ashanti Region, Ghana Effective Date: 30 September 2014 Issue Date: 24 October 2014 Reference: AGM_001 Authors: CJ Muller (Director): B.Sc. (Hons) (Geol.) Pr. Sci. Nat A. Umpire (Geology Manager) B.Sc. (Hons.) (Geol. Eng.), Pr.Sci.Nat B.Sc. Hons. (IT) MBA Suite 4 Coldstream Office Park Cnr Hendrik Potgieter & Van Staden Streets Little Falls, Roodepoort, South Africa Tel: +27 │ Fax: +27 Directors:, CJ Muller Registration CJM Consulting Technical Report on Asanko Gold Project, Ashanti Region Ghana 2 INFORMATION RISK This Report was prepared by CJM Consulting (Pty) Ltd (“CJM”). In the preparation of the Report, CJM has utilised information relating to operational methods and expectations provided to them by various sources. Where possible, CJM has verified this information from independent sources after making due enquiry of all material issues that are required in order to comply with the requirements of the NI 43-101 and SAMREC Reporting Codes. OPERATIONAL RISKS The business of mining and mineral exploration, development and production by their nature contain significant operational risks. The business depends upon, amongst other things, successful prospecting programmes and competent management. Profitability and asset values can be affected by unforeseen changes in operating circumstances and technical issues. POLITICAL AND ECONOMIC RISK Factors such as political and industrial disruption, currency fluctuation and interest rates could have an impact on future operations, and potential revenue streams can also be affected by these factors. The majority of these factors are, and will be, beyond the control of any operating entity. -
W Ai-Zei P Aper
WAI-ZEI PAPER WAI-ZEI Ablam Benjamin Akoutou, Rike Sohn, Matthias Vogl, Daniel Yeboah (eds.) Migration and Civil Society as Development Drivers - a Regional Perspective No. 23 2015 Nana Asantewa Afadzinu is Executive Director of the West Africa Civil Society Institute (WACSI) in Accra, Ghana. Ablam Benjamin Akoutou is Project Coordinator at WAI for the WAI-ZEI cooperation project. Mariama Awumbila is Associate Professor at the Department of Geography and Resource Deve- lopment and Centre for Migration Studies, University of Ghana Yaw Benneh is Senior Lecturer at Faculty of Law, and Senior Research Fellow at the Centre for Migration Studies, University of Ghana. Stefan Fröhlich is Professor of International Politics at the University of Erlangen-Nürnberg in Germany. Ludger Kühnhardt is Director at the Center for European Integration Studies (ZEI) and Professor of Political Science at Bonn University, Germany. Matthias Lücke is Senior Researcher at the Kiel Institute for the World Economy (IfW) and Adjunct Professor at Kiel University, Germany. Olawale I. Maiyegun is Director of the Department of Social Affairs of the African Union Commis- sion in Addis Ababa, Ethopia. Abdarahmane Ngaïde is Associate Researcher at the Pan-African Institute for Strategies (UCAD) in Dakar, Senegal, and teaches at University Cheikh Anta Diop of Dakar. Rike Sohn is Junior Fellow at ZEI and Project Coordinator for the WAI-ZEI cooperation project. Joseph Kofi Teye is Senior Lecturer at the Department of Geography and Resource Develop- ment, and Senior Research Fellow at the Centre for Migration Studies, University of Ghana. Djénéba Traoré is Managing Director at the West Africa Institute (WAI) in Praia, Cape Verde.