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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. -
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. -
Mineralization and Sustainable Development in the West African Craton: from field Observations to Modelling
Downloaded from http://sp.lyellcollection.org/ by guest on September 25, 2021 Mineralization and sustainable development in the West African Craton: from field observations to modelling Tahar Aïfa Université de Rennes, CNRS, Géosciences Rennes–UMR 6118, Bât. 15, Campus de Beaulieu, 35042 Rennes, France 0000-0002-1573-7668 [email protected] Abstract: This Special Publication combines results obtained by interdisciplinary groups from numerous aca- demic institutions working on Paleoproterozoic formations to decipher the origins of the main mineralization resources in the West African Craton (WAC) and their impacts on African economic development. Structural, geophysical, sedimentological, stratigraphical, geochemical, petrophysical and mineralogical analyses have been used to highlight the complexities involved in mineralization emplacement and its origin and evolution within the WAC. Fourteen articles, mainly of basic research carried out in the WAC and surrounding areas, contribute to new knowledge in mineral research with updated references. They show that the geodynamic evo- lution of the WAC is complex from one area to another: it involves subduction, collision and obduction during several deformation phases ranging from Birimian (2.3–2.0 Ga) to Pan-African (650–450 Ma) events. Miner- alization is mainly controlled by tectonics within shear zones, orogenic belts, basins and faulting systems occur- ring in the various corridors. Mineralized fluid circulation is stressed and injected into appropriate formations and precipitate several types of well-documented ore deposits: porphyry, metal-bearing, volcanogenic massive sulfide, sedimentary exhalative and lateritic. Various modelling techniques, when integrated, help in under- standing the mechanisms of mineralization emplacement, some of which are still a matter of debate. -
Lower Crust Exhumation During Paleoproterozoic (Eburnean) Orogeny
Precambrian Research 274 (2016) 82–109 Contents lists available at ScienceDirect Precambrian Research jo urnal homepage: www.elsevier.com/locate/precamres Lower crust exhumation during Paleoproterozoic (Eburnean) orogeny, NW Ghana, West African Craton: Interplay of coeval contractional deformation and extensional gravitational collapse a,∗ b c a,e d Sylvain Block , Mark Jessell , Laurent Aillères , Lenka Baratoux , Olivier Bruguier , f d d g Armin Zeh , Delphine Bosch , Renaud Caby , Emmanuel Mensah a Géosciences Environnement Toulouse, Observatoire Midi Pyrénées, 14 ave E. Belin, 31400 Toulouse, France b Center for Exploration Targeting, The University of Western Australia, 35 Stirling Highway, Crawley, Perth 6009, WA, Australia c Monash University, School of Geosciences, Wellington Road, Clayton 3800, VIC, Australia d Géosciences Montpellier, Université Montpellier 2-CNRS, cc 066, Place Eugène Bataillon, 34095 Montpellier Cedex 5, France e IFAN, Cheikh Anta Diop, Dakar, Senegal f Institut für Geowissenschaften, Altenhöfer Allee 1, D-60438 Frankfurt am Main, Germany g Geological Survey Department of Ghana, Accra, Ghana a r t i c l e i n f o a b s t r a c t Article history: We present new litho-structural and metamorphic maps of the Paleoproterozoic (2.25–2.00 Ga) West Received 1 December 2014 African Craton in northern Ghana, based on the interpretation of field observations and airborne geophys- Received in revised form 31 August 2015 ical datasets. The study reveals contrasting metamorphic domains consisting of high-grade gneisses and Accepted 17 October 2015 low-grade volcano–sedimentary belts, separated by shear zones and assembled during the Paleoprotero- Available online 29 October 2015 zoic Eburnean orogeny (2.15–2.07 Ga). -
Congo River Sand and the Equatorial Quartz Factory
Earth-Science Reviews 197 (2019) 102918 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Congo River sand and the equatorial quartz factory T ⁎ Eduardo Garzantia, , Pieter Vermeeschb, Giovanni Vezzolia, Sergio Andòa, Eleonora Bottia, Mara Limontaa, Pedro Dinisc, Annette Hahnd, Daniel Baudete, Johan De Gravef, Nicole Kitambala Yayag a Laboratory for Provenance Studies, Department of Earth and Environmental Sciences, University of Milano-Bicocca, 20126 Milano, Italy b London Geochronology Centre, Department of Earth Sciences, University College London, London, WC1E 6BT, UK c Department of Earth Sciences, MARE – Marine and Environmental Sciences Centre, University of Coimbra, Portugal d MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany e Geodynamics & Mineral Resources, Royal Museum for Central Africa (RMCA), Leuvensesteenweg 13, 3080 Tervuren, Belgium f Department of Geology and Soil Science (WE13), MINPET, Ghent University, Krijgslaan 281/S8, WE13, B-9000 Gent, Belgium g CRGM Centre de Recherches Géologiques et Minières, 44, Av. de la Démocratie, Kinshasa-Gombe, Democratic Republic of Congo ARTICLE INFO ABSTRACT Keywords: A never solved problem in sedimentary petrology is the origin of sandstone consisting exclusively of quartz and Provenance analysis most durable heavy minerals. The Congo River offers an excellent test case to investigate under which tectonic, Equatorial weathering geomorphological, climatic, and geochemical conditions pure quartzose sand is generated today. In both upper U-Pb zircon geochronology and lowermost parts of the catchment, tributaries contain significant amounts of feldspars, rock fragments, or Zircon weatherability moderately stable heavy minerals pointing at the central basin as the main location of the “quartz factory”. -
Geographical and Subject Index
Index Geographical and Subject Index J\[`d\ekXip 9Xjj`ej E @ek\i`fiYXj`e N < :fdgfj`k\Xe[Zfdgc\oYXj`ej I`]kYXj`e J ;fnenXigYXj`e DXi^`eXcjX^figlcc$XgXikYXj`ej D\[`XeXe[jlY[lZk`feYXj`ej ;\ckX DXafi]iXZkli\qfe\j Geographical Index A B Abd-Al-Kuri (Socotra) 224 Bab el Mandeb (Sudan) 241 Aberdares (Kenya) 136 Babadougou (Ivory Coast) 130 Abidjan (Ivory Coast) 128 Babassa (Central African Republic) 68 Abkorum-Azelik (Niger) 192 Baddredin (Egypt) 96 Abu Ras Plateau (Egypt) 94 Bahariya Oasis (Egypt) 95, 96 Abu Tartur (Egypt) 94, 96 Bakouma (Central African Republic) 68 Abu Zawal (Egypt) 94 Bamako (Mali) 165 Abuja (Nigeria) 196 Bandiagara (Mali) 165 Accra (Ghana) 119 Bangui (Central African Republic) 68 Acholi region (Uganda) 265 Bangweulu Swamp (Zambia) 270 Adrar des Iforas (Algeria) 32, 34 Banjul (Gambia) 114 Addis Ababa (Ethiopia) 106 Baragoi (Kenya) 134 Ader-Doutchi (Niger) 193 Barberton Mountains (South Africa) 230 Adola (Ethiopia) 108 Basila (Benin) 44 Adrar (Mauritania) 169 Bation Peak (Kenya) 135 Adrar des Iforas Mountains (Mali) 162 Batoka Gorge (Zambia) 270 Adua-Axum (Ethiopia) 106 Bayuda Desert (Sudan) 238, 240 Afast (Niger) 192 Beghemder (Ethiopia) 106 Agadez (Niger) 192, 193 Benghazi (Libya) 150 Agadir (Morocco) 176 Bengo (Angola) 41 Agbaja Plateau (Nigeria) 196 Benty (Guinea) 124 Ahnet (Algeria) 34 Benue Valley (Nigeria) 196 AÏr Massif 190, 193 Biankouma (Ivory Coast) 130 Akagera (Rwanda) 206 Bidzar (Cameroon) 60 Akoufa (Niger) 192 Bie (Angola) 41 Alexandra Peak (Uganda) 264 Big Hole (South Africa) 234, 235 Algerian Atlas (Algeria) -
Uranium Deposits in Africa: Geology and Exploration
Uranium Deposits in Africa: Geology and Exploration PROCEEDINGS OF A REGIONAL ADVISORY GROUP MEETING LUSAKA, 14-18 NOVEMBER 1977 tm INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1979 The cover picture shows the uranium deposits and major occurrences in Africa. URANIUM DEPOSITS IN AFRICA: GEOLOGY AND EXPLORATION The following States are Members of the International Atomic Energy Agency: AFGHANISTAN HOLY SEE PHILIPPINES ALBANIA HUNGARY POLAND ALGERIA ICELAND PORTUGAL ARGENTINA INDIA QATAR AUSTRALIA INDONESIA ROMANIA AUSTRIA IRAN SAUDI ARABIA BANGLADESH IRAQ SENEGAL BELGIUM IRELAND SIERRA LEONE BOLIVIA ISRAEL SINGAPORE BRAZIL ITALY SOUTH AFRICA BULGARIA IVORY COAST SPAIN BURMA JAMAICA SRI LANKA BYELORUSSIAN SOVIET JAPAN SUDAN SOCIALIST REPUBLIC JORDAN SWEDEN CANADA KENYA SWITZERLAND CHILE KOREA, REPUBLIC OF SYRIAN ARAB REPUBLIC COLOMBIA KUWAIT THAILAND COSTA RICA LEBANON TUNISIA CUBA LIBERIA TURKEY CYPRUS LIBYAN ARAB JAMAHIRIYA UGANDA CZECHOSLOVAKIA LIECHTENSTEIN UKRAINIAN SOVIET SOCIALIST DEMOCRATIC KAMPUCHEA LUXEMBOURG REPUBLIC DEMOCRATIC PEOPLE'S MADAGASCAR UNION OF SOVIET SOCIALIST REPUBLIC OF KOREA MALAYSIA REPUBLICS DENMARK MALI UNITED ARAB EMIRATES DOMINICAN REPUBLIC MAURITIUS UNITED KINGDOM OF GREAT ECUADOR MEXICO BRITAIN AND NORTHERN EGYPT MONACO IRELAND EL SALVADOR MONGOLIA UNITED REPUBLIC OF ETHIOPIA MOROCCO CAMEROON FINLAND NETHERLANDS UNITED REPUBLIC OF FRANCE NEW ZEALAND TANZANIA GABON NICARAGUA UNITED STATES OF AMERICA GERMAN DEMOCRATIC REPUBLIC NIGER URUGUAY GERMANY, FEDERAL REPUBLIC OF NIGERIA VENEZUELA GHANA NORWAY VIET NAM GREECE PAKISTAN YUGOSLAVIA GUATEMALA PANAMA ZAIRE HAITI PARAGUAY ZAMBIA PERU The Agency's Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957. The Headquarters of the Agency are situated in Vienna. -
2Nd Colloquium of the International Geoscience Program IGCP638
2nd Colloquium of the International Geoscience Program IGCP638 Geodynamics and mineralizations of paleoproterozoic formations for a sustainable development Casablanca, 07th-12th November 2017 Parrainé par l’UNESCO Organisé par L'Université Hassan II de Casablanca Faculté des Sciences Aïn Chock IGCP638 Leaders: Tahar AÏFA / Rennes 1 University (France) Omar SADDIQI / Hassan II Casablanca University (Morocco) Moussa DABO/ Cheikh Anta Diop University, Dakar (Senegal) http://igcp638.univ-rennes1.fr ORGANIZING COMMITTEE Omar Saddiqi (FSAC UH2C Casablanca): Chairman Lahssen Baidder (FSAC UH2C Casablanca) EL Hassan El Arabi (FSAC UH2C Casablanca) Aboubaker Farah (FSAC UH2C Casablanca) Faouziya Haissen ( FSBM UH2C Casablanca) Atika Hilali (FSAC UH2C Casablanca) Abdelhadi Kaoukaya (FSAC UH2C Casablanca) Mehdi Mansour (FSAC UH2C Casablanca) Mostafa Oukassou (FSBM UH2C Casablanca) Hassan Rhinane (FSAC UH2C Casablanca) SCIENTIFIC COMMITTEE Tahar Aïfa (Univ. Rennes 1, France) Alain Kouamelan (Univ. Abidjan, Ivory Coast) Mohammed Aissa (UMS Meknès, Morocco) Théophile Lasm (Univ. Abidjan, Ivory Coast) Laurent Ameglio (GyroLAG Potchefstroom, South Africa/ Jean-Pierre Lefort (Univ. Rennes 1, France) Perth, Australia) Addi Azza (Conseiller du Ministre de l’Energie, des Mines Ulf Linnemann (Unv. Dresden, Germany) et du Développement Durable, Rabat, Morocco) David Baratoux (IRD/UPS/IFAN, France) Khalidou Lo (Univ. Nouakchott, Mauritania) Lahssen Baidder (UH2C Casablanca, Morocco) Martin Lompo (Univ. Ouagadougou, Burkina Faso) Lenka Baratoux (IRD/IFAN, France) Lhou Maacha (Managem Casablanca, Morocco) Jocelyn Barbarand (UPS Orsay, France) Younes Maamar (Managem Casablanca, Morocco) Fernando Bea (Univ. of Granada, Spain) Henrique Masquelin (Univ. Montevideo, Uruguay) Mouloud Benbrahim (Univ. of Oran, Algeria) Sharad Master (Univ. Johannesburg, South Africa) Mohammed Bouabdellah (UMP Oujda, Morocco) Nacer Merabet (CRAAG Algiers, Algeria) Jean-Louis Boudinier (Univ. -
Quantifying Spatial Association Between Mineral Deposits And
Quantifying spatial association between mineral deposits and geology across three African crustal segments of different age, with implication for secular change in mineralization during Earth history. Tshifbiwa Mabidi Town Cape of Thesis submitted in fulfilment of the requirements for the degree of Master of Science University Department of Geological Sciences University of Cape Town February, 2006 AE::ON AFRICA EARTH OOSERVATORY NETWORK EARTH STEWARDSH P THROUGH SCIENCE The copyright of this thesis vests in the author. No quotation from it or information derived from it is to be published without full acknowledgement of the source. The thesis is to be used for private study or non- commercial research purposes only. Published by the University of Cape Town (UCT) in terms of the non-exclusive license granted to UCT by the author. University of Cape Town Declaration • I know that plagiarism is wrong. Plagiarism is to use another's work and to pretend that it is one's own. • Each significant contribution to, and quotation in, this thesis from the work, or works, of other people has been attributed, and has been cited and referenced. • This thesis is my own work. ■ I have not allowed, and will not allow, anyone to copy my work with the intention of passing it offas his/her own work. Abstract Variations in enrichment of mineralization, expressed in ore deposits, in the continental crust may be one way to test for secular changes in crustal genesis. This study collates and analyses fundamental information about mineral deposits with which to 'fingerprint' the metal endowment of African crust of different age. -
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. -
Neoproterozic Ages for Supposed Eburnean Basement of the Bou Azzer Inlier, Anti-Atlas Mountains R.S
Precambrian Research 147 (2006) 65–78 A newly discovered orogenic event in Morocco: Neoproterozic ages for supposed Eburnean basement of the Bou Azzer inlier, Anti-Atlas Mountains R.S. D’Lemos a, J.D. Inglis b, S.D. Samson b,∗ a Deers Cottage, Somerton, UK OX25 6NP, USA b Department of Earth Sciences, Syracuse University, Syracuse, NY 13244, USA Received 25 August 2005; received in revised form 7 February 2006; accepted 9 February 2006 Abstract The Bou Azzer inlier within the Anti-Atlas orogenic belt of Morocco exposes a dismembered ophiolite, long considered to mark a Late Neoproterozoic suture between the West African Craton (WAC) in the south, and Neoproterozoic arcs to the north. Southern parts of the Bou Azzer inlier include meta-igneous units, paragneiss, schist and muscovite-bearing granite that have until now been regarded as the c. 2 Ga Eburnean WAC basement onto which the ophiolite was obducted. An example of supposed Paleoproterozoic basement occurs at Tazigzaout. The main units within this complex are metagabbro, augen granite gneiss, finely banded granite gneiss and variably sheared syn-tectonic leucogranite, all of which are intercalated within a complex sub-vertical, upper greenschist facies, ductile dextral shear zone. The meta-igneous rocks are crosscut by a sheeted muscovite-biotite granite pluton. Three concordant U–Pb analyses of zircon from an augen granite gneiss provide a date of 753 +1/−2 Ma. Zircon from a nearby metagabbro provide an indistinguishable date of 752.2 ± 2.4 Ma. Both dates are considered best estimates of the crystallization ages of their igneous protoliths. -
Eburnean Deformation Pattern of Burkina Faso and the Tectonic Significance of Shear Zones in the West African Craton
BSGF - Earth Sciences Bulletin 2020, 191, 2 © D. Chardon et al., Published by EDP Sciences 2020 https://doi.org/10.1051/bsgf/2020001 Available online at: www.bsgf.fr Eburnean deformation pattern of Burkina Faso and the tectonic significance of shear zones in the West African craton Dominique Chardon1,2,3,*, Ousmane Bamba1 and Kalidou Traoré1,2,4 1 Département des Sciences de la Terre, Université Joseph Ki-Zerbo, Ouagadougou, Burkina Faso 2 IRD, Ouagadougou, Burkina Faso 3 GET, Université de Toulouse, IRD, CNRS, UPS, CNES, Toulouse, France 4 Laboratoire de cartographie, DER de Géologie, FST, Université des Sciences, des Techniques et des Technologies de Bamako, Bamako, Mali Received: 11 March 2019 / Accepted: 24 December 2019 Abstract – Shear zones of the Paleoproterozoic Eburnean accretionary Orogen (West African craton) are investigated by means of large-scale structural mapping. Regional scale (10-100 km) mapping was based on the aeromagnetic survey of Burkina Faso and craton-scale (1000 km) mapping on a compilation of fabric data. At both scales, shear zones are arranged as an anastomosed transpressional network that accommodated distributed shortening and lateral flow of the orogenic lithosphere between the converging Kénéma-Man and Congo Archean provinces. Structural interference patterns at both scales were due to three-dimensional partitioning of progressive transpressional deformation and interactions among shear zones that absorbed heterogeneities in the regional flow patterns while maintaining the connectivity of the shear zone network. Such orogen-scale kinematic patterns call for caution in using the deformation phase approach without considering the “bigger structural picture” and interpreting displacement history of individual shear zones in terms of plate kinematics.