Mineralogy of Dust Emissions from the Bodele Depression

Total Page:16

File Type:pdf, Size:1020Kb

Mineralogy of Dust Emissions from the Bodele Depression MINERALOGY OF DUST EMISSIONS FROM THE BODELE DEPRESSION By ROSEMARY ASSUNTA MILLHAM Bachelor of Science State University of New York at New Paltz New Paltz, NY 1983 Master of Science in Education State University of New York at New Paltz New Paltz, NY 1987 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY July, 2007 MINERALOGY OF DUST EMISSIONS FROM THE BODELE DEPRESSION Dissertation Approved: Steven Marks ________________________________________________ Dissertation Adviser Caroline Beller ________________________________________________ Steve Stadler ________________________________________________ Jack Vitek ________________________________________________ A. Gordon Emslie ________________________________________________ Dean of Graduate College ii ACKNOWLEDGEMENTS This dissertation is dedicated to the memory of Yoram Kaufman, a dedicated scientist, and good friend. Thank you for believing in me. It is with sincere thoughts and attitudes that I acknowledge the roles that Yoram Kaufman, Ilan Koren, and Vanderlei Martins have played in the development of my dissertation topic that was based on a need in the scientific community as essential to understanding climate, climate change, and climate modeling as the weather is to understanding climate. Through their dogged belief in my abilities, patience in the explanation of the difficult to explain, and the trust they placed on me in my own abilities as a geologist, Yoram, Ilan, and Vanderlei pushed the envelope of my resolve and dedication to complete the task. To Steve Marks and Jack Vitek, to whom I owe the deepest gratitude for their unfailing support, advice, and direction, I say thank you for your valued trust in my work ethics, dedication, and abilities. To my family, especially to my adult children, Jennifer and Matthew, I am amazed and truly blessed to know how much faith you have in me to accomplish something I thought was unreachable. To my husband, Bobby Boy, thanks for all of the meals and doggie walks that allowed me to work uninterrupted for days at a time when I needed the time to follow through on an idea, concept, or theory. You are truly one-of-a- kind. iii TABLE OF CONTENTS Chapter Page I. INTRODUCTION .....................................................................................1 Statement of the Problem .....................................................................4 Purpose of the Study.............................................................................5 Significance of the Study......................................................................5 Research Questions ..............................................................................6 Definition of Terms..............................................................................7 Scope of Study ...................................................................................28 Limitations.........................................................................................28 Assumptions.......................................................................................29 II. REVIEW OF LITERATURE...................................................................31 Introduction........................................................................................31 Aerosols in General............................................................................44 Primary and Secondary Sources of Aerosols.......................................48 Aerosol Light Scattering Efficiency....................................................55 Aerosols and Cloud Formation ...........................................................66 Atmospheric Mineral Dust .................................................................72 Geological and Geomorphological Considerations .............................75 The Bodele ........................................................................................84 Summary............................................................................................88 III. METHODOLOGY...................................................................................90 Procedures and Instrumentation..........................................................90 Data Collection ..................................................................................92 Data Analysis.....................................................................................94 IV. FINDINGS AND ANALYSIS OF DATA................................................96 Analysis of SEM Bulk Data................................................................98 Analysis of SEM Aerosol Data.........................................................102 Analysis of XRD Bulk Data .............................................................104 Analysis of XRD XRF Data .............................................................107 iviv Chapter Page Analysis of Geological Maps............................................................112 Research Questions and Hypothesis .................................................112 V. SUMMARY, CONCLUSIONS, AND RECOMMENDATIONS ...........116 Summary..........................................................................................116 Conclusions......................................................................................117 Recommendations ............................................................................118 BIBLIOGRAPHY ...................................................................................................120 APPENDIXES ........................................................................................................138 APPENDIX A - MAPS OF AFRICA, CHAD, AND BODELE.......139 APPENDIX B - SATELLITE IMAGES OF THE BODELE...........142 APPENDIX C - SEM DATA FOR BULK SAMPLES....................146 APPENDIX D - SEM IMAGES FOR BULK SAMPLES................195 ` APPENDIX E - SEM DATA FOR AEROSOL SAMPLES ............219 APPENDIX F SEM IMAGES FOR AEROSOL SAMPLES ........235 APPENDIX G - XRD DATA FOR BULK SAMPLE......................242 APPENDIX H - TECHNOLOGY FOR XRD XRF .........................245 v LIST OF TABLES Table Page 1. Annual Source Strength............................................................................47 2. Primary Particle Emissions.......................................................................49 3. Aerosol Sulfates Precursors......................................................................69 4. Atomic % and Weight % Bulk Sample Analyses......................................99 5. Elemental Weight % Analyses for Crustal Materials ..............................100 6. Actual SEM Bulk Data Chemical Analyses............................................101 7. Elemental Table of Clay Mineral Elements for Crustal Material on Earth..................................................................102 8. Atomic % and Weight % Aerosol Sample Analyses ...............................103 9. Actual SEM Aerosol Data Chemical Analyses .......................................104 10. Bodele Semi-Quantitative Mineral Analysis...........................................104 vi LIST OF FIGURES Figure Page 1, Bodele Depression, Chad in Africa...........................................................3 2. Saltation of Sediments ..............................................................................31 3. Particle Size Classification........................................................................32 4. Yardang Linear Features...........................................................................34 5. Dune Types ..............................................................................................34 6. Bodele Depression, Chad..........................................................................37 7. Particle Size Suspension and Wind Velocity.............................................38 8. Trade Wind Patterns of North Africa ........................................................39 9. Harmattan Wind Diagram.........................................................................40 10. Model Simulated Column Averages of Cloud Fraction with T> 253° K.........................................................................................43 11. Annual Average Aerosol Source Strength.................................................51 12. Observed and Model-predicted Annual Average Sulphate Concentrations..........................................................................................53 13. Observed and Model-predicted Annual Average Concentrations of Sea-salt.................................................................................................53 14. Simulated Surface Mass Concentrations of Dust Particles.........................54 15. Extinction Efficiency and Single Scattering Albedo..................................57 16. Aerosol Optical Depth ..............................................................................58 17. Variations of Single Scattering Albedo .....................................................60 vii Figure Page 18. Monthly Averages of Simulated First Direct Forcings...............................62 19. Observed and Simulated Concentrations of Black Carbon.........................63 20. Observed and Simulated Organic Carbon..................................................63 21. Sulphate Aerosols.....................................................................................71 22. Gondwana ................................................................................................76
Recommended publications
  • Pan-African Orogeny 1
    Encyclopedia 0f Geology (2004), vol. 1, Elsevier, Amsterdam AFRICA/Pan-African Orogeny 1 Contents Pan-African Orogeny North African Phanerozoic Rift Valley Within the Pan-African domains, two broad types of Pan-African Orogeny orogenic or mobile belts can be distinguished. One type consists predominantly of Neoproterozoic supracrustal and magmatic assemblages, many of juvenile (mantle- A Kröner, Universität Mainz, Mainz, Germany R J Stern, University of Texas-Dallas, Richardson derived) origin, with structural and metamorphic his- TX, USA tories that are similar to those in Phanerozoic collision and accretion belts. These belts expose upper to middle O 2005, Elsevier Ltd. All Rights Reserved. crustal levels and contain diagnostic features such as ophiolites, subduction- or collision-related granitoids, lntroduction island-arc or passive continental margin assemblages as well as exotic terranes that permit reconstruction of The term 'Pan-African' was coined by WQ Kennedy in their evolution in Phanerozoic-style plate tectonic scen- 1964 on the basis of an assessment of available Rb-Sr arios. Such belts include the Arabian-Nubian shield of and K-Ar ages in Africa. The Pan-African was inter- Arabia and north-east Africa (Figure 2), the Damara- preted as a tectono-thermal event, some 500 Ma ago, Kaoko-Gariep Belt and Lufilian Arc of south-central during which a number of mobile belts formed, sur- and south-western Africa, the West Congo Belt of rounding older cratons. The concept was then extended Angola and Congo Republic, the Trans-Sahara Belt of to the Gondwana continents (Figure 1) although West Africa, and the Rokelide and Mauretanian belts regional names were proposed such as Brasiliano along the western Part of the West African Craton for South America, Adelaidean for Australia, and (Figure 1).
    [Show full text]
  • Neoproterozoic Crustal Evolution in Southern Chad: Pan-African Ocean Basin Closing, Arc Accretion and Late- to Post-Orogenic Granitic Intrusion
    Neoproterozoic crustal evolution in Southern Chad: Pan-African ocean basin closing, arc accretion and late- to post-orogenic granitic intrusion. André Pouclet, Max Vidal, J.C. Doumnang, Jean-Paul Vicat, Rigobert Tchameni To cite this version: André Pouclet, Max Vidal, J.C. Doumnang, Jean-Paul Vicat, Rigobert Tchameni. Neoproterozoic crustal evolution in Southern Chad: Pan-African ocean basin closing, arc accretion and late- to post-orogenic granitic intrusion.. Journal of African Earth Sciences, Elsevier, 2006, 44, pp.543-560. 10.1016/j.jafrearsci.2005.11.019. hal-00073651 HAL Id: hal-00073651 https://hal-insu.archives-ouvertes.fr/hal-00073651 Submitted on 30 May 2006 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Neoproterozoic crustal evolution in Southern Chad: Pan- African ocean basin closing, arc accretion and late- to post-orogenic granitic intrusion A. Poucleta, M. Vidala, J.-C. Doumnangb, J.-P. Vicata and R. Tchamenic aInstitut des Sciences de la Terre d’Orléans, UMR 6113, Université, B.P. 6759, 45067 Orléans Cedex 2, France bLaboratoire de Géologie, Faculté des Sciences, Université, B.P. 1027, N’Djamena, Tchad cDépartement des Sciences de la Terre, Faculté des Sciences, Université, B.P.
    [Show full text]
  • A Detrital Record of the Nile River and Its Catchment
    Downloaded from http://jgs.lyellcollection.org/ by guest on September 26, 2021 Research article Journal of the Geological Society Published online December 7, 2016 https://doi.org/10.1144/jgs2016-075 | Vol. 174 | 2017 | pp. 301–317 A detrital record of the Nile River and its catchment Laura Fielding1, Yani Najman1*, Ian Millar2, Peter Butterworth3, Sergio Ando4, Marta Padoan4, Dan Barfod5 & Ben Kneller6 1 Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK 2 NIGL, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 3 BP Egypt, 14 Road 252, Al Maadi, Cairo, Egypt 4 DISAT, University of Milano-Bicocca, Piazza della Scienza, 4 20126 Milano, Italy 5 SUERC, Rankine Ave, Scottish Enterprise Technology Park, East Kilbride, G75 0QF, UK 6 University of Aberdeen, Aberdeen AB24 3FX, UK *Correspondence: [email protected] Abstract: This research uses analyses from Nile catchment rivers, wadis, dunes and bedrocks to constrain the geological history of NE Africa and document influences on the composition of sediment reaching the Nile delta. Our data show evolution of the North African crust, highlighting phases in the development of the Arabian–Nubian Shield and amalgamation of Gondwana in Neoproterozoic times. The Saharan Metacraton and Congo Craton in Uganda have a common history of crustal growth, with new crust formation at 3.0 – 3.5 Ga, and crustal melting at c. 2.7 Ga. The Hammamat Formation of the Arabian– Nubian Shield is locally derived and has a maximum depositional age of 635 Ma. By contrast, Phanerozoic sedimentary rocks are derived from more distant sources. The fine-grained (mud) bulk signature of the modern Nile is dominated by input from the Ethiopian Highlands, transported by the Blue Nile and Atbara rivers.
    [Show full text]
  • Detrital Zircon Analysis of the Taza-Guercif Basin and The
    University of South Carolina Scholar Commons Theses and Dissertations 5-8-2015 Detrital Zircon Analysis of the Taza-Guercif Basin and the Adjacent Rif and Middle Atlas Mountains of Morocco and X-Ray Fluorescence Chemofacies Analysis of the Maness Shale of East Texas Jonathan Richard Pratt University of South Carolina - Columbia Follow this and additional works at: https://scholarcommons.sc.edu/etd Part of the Geology Commons Recommended Citation Pratt, J. R.(2015). Detrital Zircon Analysis of the Taza-Guercif Basin and the Adjacent Rif and Middle Atlas Mountains of Morocco and X- Ray Fluorescence Chemofacies Analysis of the Maness Shale of East Texas. (Doctoral dissertation). Retrieved from https://scholarcommons.sc.edu/etd/3071 This Open Access Dissertation is brought to you by Scholar Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. DETRITAL ZIRCON ANALYSIS OF THE TAZA-GUERCIF BASIN AND THE ADJACENT RIF AND MIDDLE ATLAS MOUNTAINS OF MOROCCO AND X-RAY FLUORESCENCE CHEMOFACIES ANALYSIS OF THE MANESS SHALE OF EAST TEXAS by Jonathan Richard Pratt Bachelor of Science The Ohio State University, 2008 Submitted in Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy in Geological Sciences College of Arts and Sciences University of South Carolina 2015 Accepted by: David L. Barbeau, Jr., Major Professor Andrew Leier, Committee Member Michael Bizimis, Committee Member Howie Scher, Committee Member Harry Rowe, Committee Member Lacy Ford, Vice Provost and Dean of Graduate Studies © Copyright by Jonathan Richard Pratt, 2015 All Rights Reserved.
    [Show full text]
  • The Saharides and Continental Growth During the Final Assembly of Gondwana-Land
    Reconstructing orogens without biostratigraphy: The Saharides and continental growth during the final assembly of Gondwana-Land A. M. Celâl S¸ engöra,b,1, Nalan Lomc, Cengiz Zabcıb, Gürsel Sunalb, and Tayfun Önerd aIstanbul_ Teknik Üniversitesi (ITÜ)_ Avrasya Yerbilimleri Enstitüsü, Ayazaga˘ 34469 Istanbul,_ Turkey; bITÜ_ Maden Fakültesi, Jeoloji Bölümü, Ayazaga˘ 34469 Istanbul,_ Turkey; cDepartement Aardwetenschappen, Universiteit Utrecht, 3584 CB Utrecht, The Netherlands; and dSoyak Göztepe Sitesi, Üsküdar 34700 Istanbul,_ Turkey Contributed by A. M. Celâl S¸ engör, October 3, 2020 (sent for review July 17, 2020; reviewed by Jonas Kley and Leigh H. Royden) A hitherto unknown Neoproterozoic orogenic system, the Sahar- identical to those now operating (the snowball earth and the ab- ides, is described in North Africa. It formed during the 900–500-Ma sence of land flora were the main deviating factors), yet the interval. The Saharides involved large subduction accretion com- dominantly biostratigraphy-based methods used to untangle oro- plexes occupying almost the entire Arabian Shield and much of genic evolution during the Phanerozoic are not applicable Egypt and parts of the small Precambrian inliers in the Sahara in- to them. cluding the Ahaggar mountains. These complexes consist of, at least by half, juvenile material forming some 5 million km2 new Method of Reconstructing Complex Orogenic Evolution in continental crust. Contrary to conventional wisdom in the areas the Neoproterozoic without Biostratigraphy: Example of the they occupy,
    [Show full text]
  • Metacraton: Nature, Genesis and Behavior
    Gondwana Research 23 (2013) 220–237 Contents lists available at SciVerse ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr GR Focus Review Metacraton: Nature, genesis and behavior Jean-Paul Liégeois a,⁎, Mohamed G. Abdelsalam b, Nasser Ennih c, Aziouz Ouabadi d a Isotope Geology, Royal Museum for Central Africa, B-3080 Tervuren, Belgium b Missouri University of Science and Technology, Dept Geological Sciences & Engineering, 1400 N. Bishop, Rolla, MO 65401, USA c Équipe de Géodynamique, Géo-éducation et Patrimoine Géologique, Dept Géologie, Faculté des Sciences, Université Chouaïb Doukkali, BP. 20, 24000 El Jadida, Morocco d Laboratoire LGGIP/USTHB, Faculté des Sciences de la Terre, de la Géographie et de l'Aménagement du Territoire, BP 32, El Alia Bab Ezzouar 16 111 Algiers, Algeria article info abstract Article history: In this paper, we show with examples that cratons involved in intercontinental collisions in a lower plate Received 3 November 2011 position are often affected by orogenic events, leading to the transformation of their margins. In some Received in revised form 14 February 2012 cases, craton interiors can also be shaped by intense collisional processes, leading to the generation of intra- Accepted 26 February 2012 cratonic orogenic belts. We propose to call these events “metacratonization” and the resulting lithospheric Available online 3 March 2012 tract “metacraton”. Metacratons can appear similar to typical orogenic belts (i.e. active margin transformed by collisional processes) but are actually
    [Show full text]
  • Cenozoic Mountain Building of Western Europe Controlled By
    A North Atlantic Ocean Baltica Shield 60˚ Oslo Neogene-Quaternary Rift VG MFG Tornquist Zone Paleogene Rockall WCG Through 50˚ North Mesozoic Sea EURASIA Trans-European Suture Zone (TESZ) Paleozoic/ Precambrian basement Major Alpine Western EGU21-12348-GD1.6 normal and reverse Approaches HZ faults Basin AR RM Paleozoic and Mesozoic Bohemian Ca rp faults (with reactivation) Massif a th Bay of Biscay RG i an s Cenozoic magmatism MC Alps Pannonian N.Dobrogea Basin Pyrenees Apennines Dinarides Adriatic Sea Moesia Gulf of Lion Iberian Ranges Liguro- IBERIA provençal Basin Hellenides Tyrrhenian Betics Sea Cenozoic mountain building of WesternAlgerian Alboran Sea Basin Rif m i s Tell C r Aegean a p Meseta Mid. Atlas l n Sea Pelagian a b ri a Saharan Atlas Sea Europe controlled by continentalHigh Atlas lithosphere Ionian Sea M Anti-Atlas e diterra nnean ridge evolution Tindouf Basin AFRICA Cyrenaica Reguibat Shield Precambrian Laurentian nt B o r basement (Scotland) f don le ian a Frédéric Mouthereau & Paul Angrand Grampian arc and allochtonous LAURENTIA Caledonian front C 60°N units of Caledonian (Scandian) orogen BALTICA GET-Univ. Toulouse - France Sveconorwegian Fig. 7 Caledonian front Iapetus Variscan front with its Thor suture reconstructed position AVALONIA o"shore Alpine main faults (Alps, Variscan front Betics , Rif) ARMORICA Tornquist Rheic Moroccan Hot Line 50°N Late Variscan shear zones GSB s ne ra CAMP dykes and lava !ows er NPSZ T A N A W EVSZ D ADRIA N O -G ri e p “Moroccan Hot Line” Mouthereau et al., 2021 “Cenozoic mountain Variscan front building and topographic evolution in Western Europe: impact of billion years lithosphere evolution GONDWANA and plate tectonics” submitted 0° 10° Orogenic evolution reflects mantle convection or inherited lithosphere properties ? whole-mantle drivers frica/G 80 Ma A ondw ana M W.
    [Show full text]
  • Paper Number: 4082 Geology and Geoheritage in the Sahara and Sahel Master, S.1
    Paper Number: 4082 Geology and geoheritage in the Sahara and Sahel Master, S.1 1School of Geosciences, University of Witwatersrand, Johannesburg, South Africa. [email protected] ___________________________________________________________________________ The Sahara is the largest desert in the world. It is made up of sand seas (ergs), gravel plains (regs) and mountains, including volcanoes. The Saharan region comprises a Precambrian crystalline basement, overlain by Phanerozoic platforms. The Precambrian basement consists of the Archaean to Palaeoproterozoic West African Craton and East Saharan Metacraton, and numerous Pan African (late Neoproterozoic to early Palaeozoic) mobile belts (the Rokelides, Mauritanides, Anti-Atlas, Ougarta, Adrar des Iforas, Hoggar, Aïr, Gourma, Dahomeyides, Oubanguides, and Nubian Shield). Following the Pan-African-Brasiliano tectono-thermal events, which took place during the formation of the Gondwana supercontinent, there was uplift and erosion, and a major Cambro-Ordovician sand sheet was deposited as a post-orogenic molasse, in a wide variety of continental environments, in an area extending from Morocco to Arabia. This was followed by an epicontinental margin in the north of Gondwana, along which marine transgressions over much of the Phanerozoic led to the deposition of major platform cover sequences ranging in age from Silurian to Neogene [1]. Since the Oligocene (~30 Ma), the African Plate has been stationary with respect to the underlying mantle, resulting in continent-wide basin and swell topography, which reflects an underlying shallow-mantle system of convection cells [2]. Broad uplifts have formed over regions of rising convection cells, and in these regions the Phanerozoic cover has been stripped by erosion, exposing the Precambrian basement.
    [Show full text]
  • New Insights Into the Crust and Lithospheric Mantle Structure of Africa from Elevation, Geoid, and Thermal Analysis
    New insights into the crust and lithospheric mantle structure of Africa from elevation, geoid, and thermal analysis Jan Globig(1), Manel Fernàndez(1), Montserrat Torne(1), Jaume Vergés(1), Alexandra Robert(2) and Claudio Faccenna(3) (1) Institute of Earth Sciences Jaume Almera, ICTJA-CSIC, Group of Dynamics of the Lithosphere (G.D.L.), Barcelona, Spain (2) Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, France (3) University Roma TRE, Dept. of Geological Sciences, Italy Key points: 1) We present 10 min resolution crust and lithosphere maps of Africa constrained by a compilation of seismic Moho data and tomography models. 2) Our maps cover large areas of Africa where no data are available showing 76% fit with seismic data after excluding the Afar plume region. 3) Misfits with seismic data in the Afar region are discussed in terms of residual topography related to sublithospheric processes. Abstract 1. Introduction 2. Tectonic Background 3. Data 4. Method and model parameters 5. Results This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1002/2016JB012972 © 2016 American Geophysical Union. All rights reserved. 6. Discussion 7. Conclusion Appendix References Acknowledgments Abstract We present new crust and lithosphere thickness maps of the African mainland based on integrated modeling of elevation and geoid data and thermal analysis. The approach assumes local isostasy, thermal steady-state, and linear density increase with depth in the crust and temperature-dependent density in the lithospheric mantle.
    [Show full text]
  • Seismic Tomography, Mantle Petrology, and Tectonic Evolution
    The lithospheric architecture of Africa: Seismic tomography, mantle petrology, and tectonic evolution G.C. Begg Minerals Targeting International, 26/17 Prowse Street, West Perth, Western Australia 6005, Australia, and GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia W.L. Griffi n L.M. Natapov Suzanne Y. O’Reilly GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia S.P. Grand Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA C.J. O’Neill GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, New South Wales 109, Australia J.M.A. Hronsky Western Mining Services (Australia), 26/17 Prowse Street, West Perth, Western Australia 6005, Australia Y. Poudjom Djomani GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia, and Geological Survey of New South Wales, Maitland, New South Wales 2320, Australia C.J. Swain Western Australian Centre for Geodesy, Curtin University of Technology, Perth, Western Australia 6845, Australia T. Deen GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, New South Wales 2109, Australia, and British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK P. Bowden Department of Geology-Petrology-Geochemistry, Université Jean-Monnet, 42023 Saint-Étienne, France ABSTRACT ancient highly depleted subcontinental litho- refertilization has reduced the lateral and spheric mantle (SCLM), zones of younger or vertical extent of strongly depleted SCLM. We present a new analysis of the litho- strongly modifi ed SCLM and zones of active Some cratonic roots extend ≥300 km into the spheric architecture of Africa, and its evolu- mantle upwelling, and to relate these to the Atlantic Ocean, suggesting that the upper tion from ca.
    [Show full text]
  • The Significance of the Transbrasiliano-Kandi Tectonic
    DOI: 10.5327/Z2317-48892013000300012 INVITED REVIEW The significance of the Transbrasiliano-Kandi tectonic corridor for the amalgamation of West Gondwana A significação do corredor tectônico Transbrasiliano-Kandi para a amalgamação do Gondwana Ocidental Umberto Giuseppe Cordani1*, Marcio Martins Pimentel2, Carlos Eduardo Ganade de Araújo3, Reinhardt Adolfo Fuck2 ABSTRACT: The assembly of West Gondwana was completed by the RESUMO: O supercontinente Gondwana Ocidental completou-se no end of the Precambrian, when the Amazonian, West African, São Fran- final do Pré-Cambriano, quando os crátons Amazônico, São Francis- cisco-Congo, Kalahari and Rio de la Plata cratons, as well as the Saharan co-Congo, Kalahari e Rio de La Plata, o metacraton do Sahara e os metacraton and the Parnaíba, Paranapanema and Luiz Alves cratonic fragmentos cratônicos do Paranapanema, Parnaíba e Luiz Alves foram fragments were united by means of the Brasiliano-Pan African orogeny, amalgamados pelos eventos da Orogenia Brasiliana-Pan-Africana, pro- a geotectonic process that was active from the late Neoproterozoic to the cesso geotectônico ativo entre o Neoproterozoico e o início do Paleozoico, early Paleozoic, related to the closure of a large oceanic domain, the Goi- relacionado com o fechamento de um grande domínio oceânico, o Ocea- ás-Pharusian Ocean. Several accretionary complexes and possible micro- no Goiás-Farusiano. Neste processo, diversos complexos acrecionários continents were trapped within the Brasiliano-Pan African mobile belts, e possíveis microcontinentes foram aprisionados nos cinturões móveis and they have been accommodated within a few hundred kilometers brasilianos-pan-africanos e foram acomodados no interior do corredor of the Transbrasiliano-Kandi tectonic corridor.
    [Show full text]
  • Structural Geology of Abu Sari Auriferous Veins in Northern Sudan: an Example for Shear-Hosted Mesothermal Gold Mineralization in Greenstone Belts
    STRUCTURAL GEOLOGY OF ABU SARI AURIFEROUS VEINS IN NORTHERN SUDAN: AN EXAMPLE FOR SHEAR-HOSTED MESOTHERMAL GOLD MINERALIZATION IN GREENSTONE BELTS A THESIS SUBMITTED TO THE GRADUATE SCHOOL OF NATURAL AND APPLIED SCIENCES OF MIDDLE EAST TECHNICAL UNIVERSITY BY ERDEM ATALAR IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN GEOLOGICAL ENGINEERING SEPTEMBER 2019 Approval of the thesis: STRUCTURAL GEOLOGY OF ABU SARI AURIFEROUS VEINS IN NORTHERN SUDAN: AN EXAMPLE FOR SHEAR-HOSTED MESOTHERMAL GOLD MINERALIZATION IN GREENSTONE BELTS submitted by ERDEM ATALAR in partial fulfillment of the requirements for the degree of Master of Science in Geological Engineering Department, Middle East Technical University by, Prof. Dr. Halil Kalıpçılar Dean, Graduate School of Natural and Applied Sciences Prof. Dr. Erdin Bozkurt Head of Department, Geological Engineering Prof. Dr. Erdin Bozkurt Supervisor, Geological Engineering, METU Examining Committee Members: Prof. Dr. Gürol Seyitoğlu Geological Engineering Dept., Ankara University Prof. Dr. Erdin Bozkurt Geological Engineering, METU Assoc. Prof. Dr. Erman Özsayın Geological Engineering Dept., Hacettepe University Assist. Prof. Dr. Ulaş Avşar Geological Engineering Dept., METU Assist. Prof. Dr. Selman Aydoğan Geological Engineering Dept., Balıkesir University Date: 12.09.2019 I hereby declare that all information in this document has been obtained and presented in accordance with academic rules and ethical conduct. I also declare that, as required by these rules and conduct, I have fully cited and referenced all material and results that are not original to this work. Name, Surname: Erdem Atalar Signature: iv ABSTRACT STRUCTURAL GEOLOGY OF ABU SARI AURIFEROUS VEINS IN NORTHERN SUDAN: AN EXAMPLE FOR SHEAR-HOSTED MESOTHERMAL GOLD MINERALIZATION IN GREENSTONE BELTS Atalar, Erdem Master of Science, Geological Engineering Supervisor: Prof.
    [Show full text]