The Geology and Gold Mineralization of the Belhoura Region, Northern Burkina Faso, West Africa, and Their Implications for the Birimian of West Africa

Total Page:16

File Type:pdf, Size:1020Kb

The Geology and Gold Mineralization of the Belhoura Region, Northern Burkina Faso, West Africa, and Their Implications for the Birimian of West Africa The Geology and gold mineralization of the Belhoura Region, Northern Burkina Faso, West Africa, and their implications for the Birimian of West Africa Item Type text; Thesis-Reproduction (electronic) Authors Schaeneman, Lewis George Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 05/10/2021 09:17:45 Link to Item http://hdl.handle.net/10150/558232 The Geology and Gold Mineralization of the Belhoura Region, Northern Burkina Faso, West Africa, and Their Implications for the Birimian of West Africa by Lewis George Schaeneman HI Copyright © Lewis George Schaeneman m 1994 A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 9 4 2 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under the rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the copyright holder. SIGNED: APPROVAL BY THESIS DIRECTOR This thesis has been approved on the date shown below: ) 9 ? ^ ~ John M. Guilbert Date ofesspr of Geology 3 ACKNOWLEDGMENTS This study was funded in large part by BHP Minerals. Ideas presented here are by products of a visit to Burkina Faso with Demetrius Pohl of BHP Minerals in July of 1990. These ideas, however, were developed solely by the author and are his responsibility alone. Jim Bratt, Chris Ford, and Demetrius Pohl were instrumental in obtaining funding for the field portion of the study and the chemical analyses, and Demetrius' instruction in the ’how to' of operating in Burkina was invaluable. Doug Ellesworth and Bill Fox of BHP Minerals' Minerals Laboratory provided valuable assistance in analyzing the geochemical samples and added much to the interpretation of the geochemical data through our numerous discussions. John Foley, a temporary employee at the Minerals Lab, also contributed to these discussions. Puru Shresta generously donated instruction and time on the SEM, arranged for the preparation of polished grain mounts, and spent time discussing the data. This study would not have existed, and could not have been completed, without the help of these individuals. Sincere thanks are extended to the people of the Bureau Des Mines et de la Geologic du Burkina (BUMIGEB) for their assistance during the field portion of this study. Mr. Kabore, the Director General of BUMIGEB, graciously allowed the use of their facilities at Belhoura and Ouagadougou, as well as access to BUMIGEB bulk samples and drill cores at Belhoura. Mr. Kabore's assistance was instrumental in dealing with the military authorities during my stay in Burkina and undoubtedly made travel much easier than it would have been otherwise. Credit and thanks also go to Joseph Sawadogo, Francois Pale, and Jean Frederic Somdah for their open discussion of their work at Belhoura and for their help in making travel and living arrangements at Belhoura. Understanding of weathering processes and their effects in West Africa was greatly aided by discussions with George Grandin and Fabrice Colin during a two day field trip of the Belhoura area during the early stages of the field work. Many thanks are extended to Joe Wooden at the Branch of Isotope Geology, and Randy Koski at the Branch of Marine Geology of the United States Geological Survey in Menlo Park California. Use of their facilities and our many fruitful discussions were crucial to the development of the ideas presented here. Their encouragement throughout the later part of the study is in part responsible for its completion. , I would like to thank the members of my committee, John Guilbert, Joaquin Ruiz, and Spence Titley for sticking with me after the many problems and errors that made this project seem unfeasible early on and interminable later. Most of all I thank my wife, Robin, and the rest of my family for helping me through one of the most difficult periods of my life. Because of them, I am able to walk away from the experience a better person, with a healthier perspective on life and a deeper sense of what is really important in it. 4 DEDICATION This thesis is dedicated to the memory of my grandmothers Mary Schaeneman and Margaret Snider whose intelligence, kindness, tenacity of spirit, and zest for life left an indelible impression on me in my youth. They are deeply missed. 5 TABLE OF CONTENTS L IST OF FIG U R E S..................................................................................................................8 LIST OF TABLES .................................................................................................................15 LIST OF PLATES...................................... 16 A B ST R A C T ......................................................................................................... 1 7 IN T R O D U C T IO N ....................................................................................... .........................18 Purpose of Study.................................................................................... 18 L o c a tio n ............................................................................................................................... 2 0 G eography and C lim ate.............................................................................................. 2 1 C ulture...................................................................................................................................2 2 P R O T E R O Z O IC T E C T O N IC S..................................................................................... 2 3 GEOLOGY OF WEST AFRICA ...................................................................................2 5 K enem a-M an G ranite-G reenstone D om ain........................................................2 5 B aou li-M ossi D om ain .................................................................................. 2 9 E ffects of W eathering............................................................................... 42 METHODS OF STUDY ............................................ 4 5 F ield W ork ........................................................................................... 4 5 Lithologies..................... 4 6 Structural Geology.................................................................................................. 8 2 M icro sco p y ......................................................................................................................... 8 6 Heavy Mineral Separates..................................................................................... 8 6 Scanning Electron Microscopy............................................... 1 0 8 6 TABLE OF CONTENTS-Continued Geochemistry ................................................................. 1 2 8 Sampling Methods.................................................................................... 1 2 8 Analytical Methods................................................................... 129; Analytical Results...................................... 1 3 2 D IS C U S S IO N .................................................................!........... .......................................... 1 3 4 Interpretation off Field Evidence........... ..............................................................1 3 4 Lithologic Interpretation....................................................................................1 3 4 Structural and Tectonic Interpretation.......................................................1 4 3 Interpretation of Heavy Mineral Suites..................................................... 1 7 3 In terp retation off G eochem istry...................................................... 1 7 5 Geochemical Evidence for a Sedimentary Influence on the Gold Content of the Quartz Bodies.............................................. 1 7 5 Geochemical Evidence for a Magmatic/Hydrothermal Influence on the Gold Content of the Quartz Bodies.........................1 9 7 Geochemical Evidence for a Supergene Influence on the Gold Content of the Quartz Bodies.............................................................. 1 9 9 C O N C L U S IO N S ................................................................................................................. 2 0 8 A PPE N D IX A: G eochem ical D ata........................................................................... 2 1 5 APPENDIX B: Gold Grain Chemistry From Semi-Quantitative Energy Dispersive X-ray Analysis........................................2 1 9 APPENDIX C: Geochemical Comparison off Heavy Mineral-Borne Trace Elements and Hydrothermal/Magmatic Trace E le m e n ts.............................................................................................. 2 2 1 APPENDIX D: Geochemical Comparison off Trace Elements and the Sum off Fe and Mn Oxides and Hydroxides............. 2 2 8 APPENDIX E: Geochemical Comparison
Recommended publications
  • Roxgold Inc. Annual Information Form for the Fiscal Year Ended December
    ROXGOLD INC. ANNUAL INFORMATION FORM FOR THE FISCAL YEAR ENDED DECEMBER 31, 2019 Dated March 16, 2020 TABLE OF CONTENTS GENERAL MATTERS ..................................................................................................................... 2 STATEMENT REGARDING FORWARD LOOKING STATEMENTS ........................................ 3 CORPORATE STRUCTURE ........................................................................................................... 6 GENERAL DEVELOPMENT OF THE BUSINESS ........................................................................ 7 DESCRIPTION OF THE BUSINESS ............................................................................................. 10 MINERAL RESERVE AND RESOURCE ESTIMATES .............................................................. 15 MINERAL PROPERTIES ............................................................................................................... 17 RISK FACTORS ............................................................................................................................. 30 DIVIDENDS .................................................................................................................................... 47 DESCRIPTION OF CAPITAL STRUCTURE ............................................................................... 47 MARKET FOR SECURITIES ........................................................................................................ 47 DIRECTORS AND OFFICERS .....................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Gold in Mali
    Acta Montanistica Slovaca Ročník 4 (1999), 4, 311-318 Gold in Mali 1 Imrich Kušnír Zlato v Mali Článok sa, okrem stručného úvodu do geológie regiónu, zaoberá popisom hlavných zlatých ložísk Mali, kde sa t.č. ťaží viac ako 20 t zlata ročne. Súčasné objavy zlata v tejto Západoafrickej krajine sú totiž príkladom, ako orientácia geologického prieskumu územia s dobrým potenciálom pre určitú nerastnú surovinu a použitie vhodnej metódy môže viesť k úspechu. Zlato sa v Mali ťaží už od nepamäti, ale ekonomicky významné ložiská (s prepočítanými zásobami 50 až 240 ton Au), sú objavované len v poslednom období. Presnejšie odvtedy, odkedy sa prieskum sústredil na zóny proterozoických epimetamorfovaých vulkano-sedimentárnych hornín (tzv. Birrimian greenstone belts) Západoafrického kratónu, s použitím geochémie, ako jednej z hlavných prieskumných metód. Keď si prieskumári uvedomili, že "Birrimian" môže mať rovnaký potenciál na zlato ako archaické "greenstones", ktoré sú hlavným zdrojom zlata na svete a že geochémia môže byt účinnou metódou pre prieskum krajiny s plochým povrchom, bez východov hornín, ktorá je charakteristická pre väčšinu územia Mali (a celej Západnej a Strednej Afriky). Key words: Mali, West Africa, West African craton, Tuareg shield, Proterozoic, Birrimian, Pan-african orogeny, precambrian greenstones, gold, lode gold, auriferous tourmalinites. Introduction Gold mining in Mali has a long history. In 1433, its renowned emperor Kanku Mussa brought 8 tons of gold on his pilgrimage to Mecca. Local population has exploited gold since immemorial times. Nowadays, several thousands of "artisan" miners exploit numerous sites and their production is estimated at more than 2 tons of gold per year. Industrial mining began in the 1970's (Kalana mine), following a large exploration programme by SONAREM with the soviet assistance (Golder et al., 1965; Boltroukevitch, 1973).
    [Show full text]
  • Bougouni-Kékoro Basin, Leo-Man Shield)
    Open Journal of Geology, 2021, 11, 105-141 https://www.scirp.org/journal/ojg ISSN Online: 2161-7589 ISSN Print: 2161-7570 Petro-Structural Study of the Paleoproterozoic Formations of the Faboula Gold Deposit (Bougouni-Kékoro Basin, Leo-Man Shield) Ousmane Wane1*, Amadou Baby Ouologuem1, Ismaïla N’diaye2, Ousmane Dao2, Mamadou Yossi3 1Laboratoire de Minéralogie et de Pétrologie, Faculté des Sciences et Techniques, Université des Sciences, des Techniques et des Technologies de Bamako, BP E 3206, Colline de Badalabougou, Bamako, Mali 2Faculté des Sciences et Techniques, Université des Sciences, des Techniques et des Technologies de Bamako, BP E 3206, Colline de Badalabougou, Bamako, Mali 3Sagax Afrique S.A Geophysical Surveys and Consulting, Ouagadougou, Burkina Faso How to cite this paper: Wane, O., Ouolo- Abstract guem, A.B., N’diaye, I., Dao, O. and Yossi, M. (2021) Petro-Structural Study of the Recent petro-structural investigations on the Faboula gold deposit located in Paleoproterozoic Formations of the Fabou- the Bougouni-Kékoro basin, in southern Mali, north-west of the Leo-Man la Gold Deposit (Bougouni-Kékoro Basin, Shield, have provided new data on the nature and spatial organization of the Leo-Man Shield). Open Journal of Geology, 11, 105-141. lithostratigraphic units as well as their deformation style. The deposit is cov- https://doi.org/10.4236/ojg.2021.114007 ered by a thick lateritic layer and is hosted by a metavolcano-sedimentary se- quence of Paleoproterozoic age intersected by intrusive bodies and filled Received: March 10, 2021 fractures of various shapes and types. The lithostratigraphic units consist of Accepted: April 23, 2021 Published: April 26, 2021 metagreywackes, metasiltstones, meta-argillites, slates and schists.
    [Show full text]
  • Technical Report for the First Disclosure of a Mineral Reserve Estimate for a Material Property
    Technical Report for the First Disclosure of a Mineral Reserve Estimate for a Material Property Wassa Mine, South West Ghana prepared for Golden Star Resources Ltd. Denver, Colorado submitted by David Alexander C.Eng Bogoso Gold Limited Bogoso, Ghana 1st August 2003 Report No. 010803/DA TABLE OF CONTENTS 1 Summary .............................................................................................................................................1 2 Introduction and Terms of Reference.............................................................................................3 3 Disclaimer............................................................................................................................................4 4 Property Description and Location.................................................................................................4 5 Accessibility, Climate, Local Resources, Infrastructure and Physiography ............................6 6 History .................................................................................................................................................6 7 Geological Setting...............................................................................................................................7 7.1 Deposit Type................................................................................................................................12 7.2 Stratigraphy.................................................................................................................................12
    [Show full text]
  • The Potential for Diamonds in Liberia
    ANDS, MIN L ES F O & Y GICAL SU E R LO RV N O E T E Y E S G I R G N I Y M R E IA P R UB E LIC OF LIB The potential for diamonds in Liberia liberia diamond cover.indd 1 21/01/2016 09:33:29 Liberia — an under-explored West African diamond region: ▪▪ More than 160 known occurrences of kimberlite, with many part of a single province that includes diamondiferous kimberlites in neighbouring Sierra Leone and Guinea. ▪▪ A long history of alluvial diamond production in western and central Liberia. ▪▪ Potential for new alluvial and bedrock diamond discoveries in under-explored Archean terrane. Diamonds in West Africa Diamonds in West Africa are produced from (>300 kilometres), Archean crust with low both primary (bedrock) kimberlite sources and geothermal heat flow (c. 40 mW/m2), representing secondary (alluvial) placers in Ghana, Guinea, a favourable tectonic environment for economic Sierra Leone, Togo and Liberia. West African kimberlites (Kjarsgaard, 2007). It is host to diamonds account for approximately one per cent numerous kimberlite pipes and dykes, some of of the global production of diamonds (BGS, 2015). which are known to be diamondiferous. Published information about West African kimberlites is The Man Shield, that underlies a large part of generally sparse, with those in Sierra Leone being central and western Liberia, is an area of thick the most studied. West African kimberlites can be ¨ 13°W 12°W 11°W 10°W ¨ 9°W 8°W 7°W ¨ ¨ ¨ ¨ ¨ ¨ !¨ ¨ ¨ ! ¨ N Banankoro N ¨ ¨ Bouro 9° ¨ 9° ± Baoulé ¨ ¨ ! ¨ Koidu ! ¨ ! ! ! Mandala Droujba ! X! X
    [Show full text]
  • The Potential for Gold in Liberia
    ANDS, MIN L ES F O & Y GICAL SU E R LO RV N O E T E Y E S G I R G N I Y M R E IA P R UB E LIC OF LIB The potential for gold in Liberia liberia cover.indd 1 21/01/2016 09:28:22 Liberia — a major under-explored West African gold terrane: ▪▪ Recent exploration success and new mine development have led to a considerable increase in activity. ▪▪ 90 per cent of Liberia is underlain by the Archean and Birimian, two of the most productive gold-bearing terranes globally. ▪▪ These rocks host multi-million ounce gold deposits in neighbouring countries. ▪▪ Liberia has not been systematically explored using modern techniques and deposit models, so the potential for new discoveries is great. The geology of Liberia Liberia is located within the Man Shield, part of maps for the entire country, supported by field the West African Craton, which comprises two checking, allowed the bedrock geology and main major areas of Archean and Paleoproterozoic tectonic divisions of Liberia to be defined. rocks. Liberia was mapped during the 1970s in a joint programme between the Liberia Geological Liberian age (2.5–3.0 Ga) Archean basement, Survey (LGS) and the United States Geological extending across central and western Liberia, is Survey (USGS). Aeromagnetic and aeroradiometric characterised by a granite-greenstone association 12°W 11°W 10°W 9°W8°W 7°W Voinjama Be drock gold occurrences " ge 1New Liberty " Foya ± Mano River Ran 2Weaju zi GUINEA -Wologizi Range gi 3Ndablama SIERRA LEONE Wolo 4Innis N °N 5 Leopard Rock Masawo-Zolowo 8° 6Gondoja -Zorzor " Zorzor 7Mandingo Hill Bopolu-Wuesua A F -Tawalata O mba Range 8Mt Coffee L Ni 9 Lucky Hill YAMBESEIKpo Bea Mountain Mountains 10 Gayama 10 " Sanniquellie 11 Kle Kle " Karnplay 6 12 " 12 Toto Mountain Range 2 3 9 Ganta 13 Tortor Mountain 5 13 N8 " 14 River Cess N 7° Gbarnga " 1 Sacleapea 7° 15 Kokoya " Tubmanburg St.
    [Show full text]
  • 2015 Nordgold Mineral Resources and Ore Reserves Overview
    2015 Nordgold Mineral Resources 6 and Ore Reserves 201 Overview May CONTENTS TABLES ........................................................................................................................................ 5 FIGURES ....................................................................................................................................... 6 1 INTRODUCTION ................................................................................................................... 9 2 GROUP MINERAL RESOURCES AND ORE RESERVES ............................................................. 13 2.1 Overview of Group Mineral Resources and Ore Reserves ....................................................... 13 2.2 Assessment and Reporting Criteria .......................................................................................... 21 2.3 Development and Exploration Projects ................................................................................... 23 3 OPERATING MINES - BURKINA FASO ................................................................................... 24 3.1 Regional Geology ..................................................................................................................... 24 3.2 Bissa ......................................................................................................................................... 25 3.2.1 Location and Access ...................................................................................................... 25 3.2.2 Project Ownership and License
    [Show full text]
  • Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana
    Prepared in cooperation with the Geological Survey Department, Minerals Commission, and Precious Minerals Marketing Company of Ghana under the auspices of the U.S. Department of State Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana Scientific Investigations Report 2010–5045 U.S. Department of the Interior U.S. Geological Survey Cover. The Bonsa River flowing west-northwest from the village of Bonsa, March 2009. Alluvial Diamond Resource Potential and Production Capacity Assessment of Ghana By Peter G. Chirico, Katherine C. Malpeli, Solomon Anum, and Emily C. Phillips Large alluvial diamond mining site at alluvial flat in Wenchi, March 2009 Prepared in cooperation with the Geological Survey Department, Minerals Commission, and Precious Minerals Marketing Company of Ghana under the auspices of the U.S. Department of State Scientific Investigations Report 2010–5045 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report.
    [Show full text]
  • West African Goldfields
    155 West African Goldfields M. Robertson1 and L. Peters2 The MSA Group, 20B Rothesay Avenue, Craighall Park, 2196, South Africa E-mail: [email protected]; [email protected] DOI: 10.18814/epiiugs/2016/v39i2/95773 The West African region has long been known for Introduction its gold endowment and gold production. Apart from The gold potential of West Africa has long been known, with the last 20 to 30 years, this production was largely informal artisanal mining having taken place for centuries. However, derived from informal artisanal workings covering modern systematic exploration and commercial scale mining have large areas of West Africa. For a period of over a only come into their own relatively recently. Ghana has long been the thousand years until 1500 AD, West Africa was the second largest gold producer on the African continent after South world’s most important supplier of gold, much of Africa, having produced 2.85 million troy ounces (Moz) in 2013. The increasing importance of West Africa as a gold producing region which formed part of the trans-Sahara trade with is reflected in Mali and Burkina Faso which have become the third the Arab world, whose monetary system was based on and fifth largest African producers respectively, the former having gold. Artisanal gold mining is still widespread across yielded 1.42 Moz and the latter 0.77 Moz in 2013. West Africa and a significant number of modern gold The majority of gold deposits on the West African Craton are hosted in Palaeoproterozoic rocks of the Birimian Supergroup, and mines in the region were founded on artisanal mining are temporally and spatially related to structures formed during the sites.
    [Show full text]
  • The Potential for Iron Ore in Liberia
    ANDS, MIN L ES F O & Y GICAL SU E R LO RV N O E T E Y E S G I R G N I Y M R E IA P R UB E LIC OF LIB The potential for iron ore in Liberia liberia ironore cover.indd 1 21/01/2016 09:37:17 Liberia – an under-explored West African iron ore region: ▪▪ A major historic iron ore producer — Africa’s leading producer in the 1970s. ▪▪ Approximately 65 per cent of Liberia is underlain by Archean rocks, the world’s main source of iron ore today. ▪▪ West Africa has world-class iron ore resources and is an expanding producer of global importance. ▪▪ Digital geological and aeromagnetic data available for the whole of Liberia. ▪▪ Significant potential for new discoveries in large, poorly known and under-explored areas. Iron ore in West Africa West Africa has numerous deposits and major important and widespread deposits are ‘banded resources of iron ore. Currently it accounts for iron formations’ (BIFs), most of which belong to a 15 per cent of African production with most mines Lower Proterozoic supracrustal sequence that rests located in supracrustal rocks in Sierra Leone, unconformably on crystalline Archean basement Guinea and Liberia (BGS, 2015). Various types of of the Man Shield, the southern part of the West iron ore deposit have been recognised. The most African craton that underlies much of the region. 13°W 12°W 11°W 10°W 9°W 8°W ! Wologizi Simandou Voinjama " ± " Foya ange e nge SIERRA LEONE ! i R GUINEA Rang N a N 8° Kpo Ra Wologiz 8° Nimb " Zorzor Western Range Mano to Cluster Western River Kpo To " ! @ Yekepa" Range Project Bea @ Sanniquellie
    [Show full text]