Facies Analysis and Paleontology of Carbonate Sedimentary Rock In

Total Page:16

File Type:pdf, Size:1020Kb

Facies Analysis and Paleontology of Carbonate Sedimentary Rock In ADDIS ABABA UNIVERSITY SCHOOL OF EARTH SCIENCE POST GRADUATE PROGRAM IN STRATIGRAPHY AND SEDIMENTOLOGY FACIES ANALYSIS AND PALEONTOLOGY OF CARBONATE SEDIMENTARY ROCKS IN HAGERE-SELAM, MESSOBO AND WUKRO STRATIGRAPHIC SECTIONS; NORTHERN ETHIOPIA, TIGRAI: IMPLICATION FOR DEPOSITIONAL ENVIRONMENT RECONSTRUCTION AND AGE DETERMINATION. BY WEREDE GIRMAY TESFASILASIA A Thesis Submitted to the School of Earth Science, Addis Ababa University in partial fulfillment of the requirement for the Degree Master of Science (Stratigraphy and Sedimentology Program). May 2018, Addis Ababa, Ethiopia ADDIS ABABA UNIVERSITY SCHOOL OF EARTH SCIENCE POST GRADUATE PROGRAM IN STRATIGRAPHY AND SEDIMENTOLOGY FACIES ANALYSIS AND PALEONTOLOGY OF CARBONATE SEDIMENTARY ROCK IN HAGERE-SELAM, MESSOBO AND WUKRO STRATIGRAPHIC SECTIONS; NORTHERN ETHIOPIA, TIGRAI: IMPLICATION FOR DEPOSTIONAL ENVIRONMENT RECONSTRUCTION AND AGE DETERMINATION. BY WEREDE GIRMAY TESFASILASIA ADVISOR: BALEMWAL ATNAFU (PhD) A Thesis Submitted to the School of Earth Science, Addis Ababa University in partial fulfillment of the requirement for the Degree Master of Science (Stratigraphy and Sedimentology Program). May, 2018 Addis Ababa, Ethiopia ADDIS ABABA UNIVERSITY SCHOOL OF GRADUATE STUDIES SCHOOL OF EARTH SCIENCE FACIES ANALYSIS AND PALEONTOLOGY OF CARBONATE SEDIMENTARY ROCK IN HAGERE-SELAM, MESSOBO AND WUKRO STRATIGRAPHIC SECTIONS; NORTHERN ETHIOPIA, TIGRAI: IMPLICATION FOR DEPOSTIONAL ENVIRONMENT RECONSTRUCTION AND AGE DETERMINATION. BY WEREDE GIRMAY TESFASILASIA APPROVED BY EXAMINATION BOARD AND DEPARTMENT CHAIRMAN Name Signature Date Dr. Balemwal Atnafu ________________ ________________ Head, School of Earth Science Dr. Balemwal Atnafu _________________ ________________ Advisor Dr.Mulugeta Fissha _________________ ________________ Examiner1 Dr.Gilamichael _________________ _________________ Examiner 2 May, 2018 Addis Ababa, Ethiopia DECLARATION OF ORIGINALITY I hereby declare that the thesis entitled “Facies Analysis and Paleontology of carbonate sedimentary rock in Hagere-Selam, Messobo and Wukro stratigraphic sections, Northern Ethiopia: Implication for Depositional Environment Reconstruction and Age Determination” has been carried out by me under the supervision of Dr. Balemwal Atnafu, School of Earth Science, Addis Ababa University, Addis Ababa, Ethiopia during the year 2017-18 as part of Masters of Science program in Stratigraphy and Sedimentology. I Furthermore, declare that this thesis is my original master degree work and has not been submitted to any university or institution in the past for the award of any degree or diploma at any other university. All sources and materials used for this thesis work have been well referenced and duly acknowledged. Werede Girmay Tesfasilasia _____________ _______________ Signature Date This is to certify that the above declaration made by the candidate is correct to the best of my knowledge. Dr. Balemwal Atnafu (Advisor) _____________ _______________ Signature Date ABSTRACT There is carbonate unit deposited in the Mekelle Outlier during the Upper Jurassic Period as a result of flooding of the area by Paleotethys Ocean toward the southeast direction. The Mekelle Outlier is situated in the northern most part of Northwestern Plateau (NWP) and the study carbonate successions are aligned along the western (Hagere-Selam), southeastern (Messsobo) and northeastern (Wukro section) margin of the Mekelle Outlier. This study focused on detailed investigation of facies analysis and paleontology of the Upper Jurassic carbonate units in order to obtain a detailed picture of depositional environment, age determination and correlation. Three main methods were implemented in order to accomplish the stated research problem and objective of the present study. These are pre-fieldwork, a detailed main fieldwork and laboratory analysis (petrographic analysis, micro and macro fossil description and systematics and microfacies analysis). A total of 65 rocks and 26 productive dry marl sediment samples are collected from the study sections and examined under petrographic microscope. Lithostratigraphically, the carbonate succession has a total thickness about 400m, which is characterized by thin-thick bedded limestone, mudstone, fossiliferous, coquinoidal, oolitic and sandy limestone with different skeletal components and different sedimentary structures. Based on a detailed field investigation, paleontological and petrographical information, 19 microfacies type are recognized. These are grouped into four microfacies association including tidal flat (MFT1-3), lagoon (MFL1-2), shoal (MFS1-6) and open marine environment (MFO1-8). Therefore, the depositional system of the carbonate succession represents a homoclinal ramp setting because of thier wide lateral and vertical distribution of facies. Additionally, the carbonate units of the study area are affected by different diagenetic features including compaction, cementation, dissolusion, micrtization, dolomitization, neomorphism, and silicification. The carbonate rock units are correlated within different measured sections in the Mekelle Outlier and regionally correlated with the Antalo Limestone of Blue Nile, the Urandab Formation of Ogaden, the Antalo Limestone of Eretria and other Arabian platforms based on biostratigraphy and lithostratigraphy. Keywords: Stratigraphy, Microfacies analysis, Age, Paleontology, Depositional environment, diagenesis, Mekelle Outlier. Thesis for MSc on Stratigraphy and Sedimentology By Werede i ACKNOWLEDGMENT Firstly I would like to give my sincere gratitude to Aksum University and Addis Ababa University, School of Earth Sciences for providing an opportunity to study my master degree and funding the research project. My second deepest gratitude goes to my advisor and instructor Dr. Balemwal Atnafu for his follow up, constructive comment, valuable suggestion, encouragement and tireless support. Dr. Balemwal Atnafu is the person to give my respect and acknowledgement for having valuable technical discussion with him and guidance; it is really meant a lot to me. Next I want to express my deepest sincere thanks to Ethiopian Geological Survey laboratory team for facilitating things in order to reach the thin section analysis result on time. During the research field work I got a lot of support from my friends and my colleagues Trhas Hadush and during the laboratory description and analysis, I got a lot of support from my instructor Addis Hailu. Therefore, I ran out of words to express my great appreciation and gratitude for your critical support from the beginning to the end of this thesis work. My acknowledgement goes to my family for giving me courage and unforgettable support when I am in the project work. The last but not the least my gratitude goes to government officials and local peoples of Hagere-Selam, Wukro and Mekelle for allowing and helping me during the field work. Thesis for MSc on Stratigraphy and Sedimentology By Werede ii TABLE OF CONTENTS ABSTRACT ........................................................................................................................................... i ACKNOWLEDGMENT ...................................................................................................................... ii TABLE OF CONTENTS ...................................................................................................................... iii LIST OF APPENDIXES ...................................................................................................................... vii CHAPTER ONE ....................................................................................................................................1 1. INTRODUCTION .............................................................................................................................1 1.1. Background and Justification ...................................................................................... 1 1.2. General setting of the study area ................................................................................. 2 1.2.1. Location of the study area .....................................................................................................2 1.2.2. Accessibility of the study area ...............................................................................................3 1.2.3. Physiography of the study area ..............................................................................................5 1.2.4. Drainage pattern of the study area .........................................................................................5 1.2.5. Climate and vegetation of the study area ...............................................................................5 1.2.6. Population and settlement ......................................................................................................7 1.3. Review of previous works of the carbonate succession .............................................. 7 1.4. Statement of the research problem .............................................................................. 8 1.5. Objectives of the research............................................................................................. 8 1.5.1 General objectives ..................................................................................................................8 1.5.2. Specific objectives .................................................................................................................8 1.8. Limitation of the study
Recommended publications
  • Provenance of Sandstones in Ethiopia During
    1 Provenance of sandstones in Ethiopia during Late 2 Ordovician and Carboniferous–Permian Gondwana 3 glaciations: petrography and geochemistry of the Enticho 4 Sandstone and the Edaga Arbi Glacials 5 6 Anna Lewina,*, Guido Meinholdb,c, Matthias Hinderera, Enkurie L. Dawitd, 7 Robert Busserte 8 9 aInstitut für Angewandte Geowissenschaften, Fachgebiet Angewandte 10 Sedimentologie, Technische Universität Darmstadt, Schnittspahnstraße 9, 11 64287 Darmstadt, Germany 12 bAbteilung Sedimentologie / Umweltgeologie, Geowissenschaftliches 13 Zentrum Göttingen, Universität Göttingen, Goldschmidtstraße 3, 37077 14 Göttingen, Germany 15 cSchool of Geography, Geology and the Environment, Keele University, 16 Keele, Staffordshire, ST5 5BG, UK 17 dDepartment of Geology, University of Gondar, P.O. Box 196, Gondar, 18 Ethiopia 19 eInstitut für Angewandte Geowissenschaften, Fachgebiet 20 Explorationsgeologie, Technische Universität Berlin, Ackerstraße 76, 13355 21 Berlin, Germany 22 23 *corresponding author. Tel. +49 6151 1620634 24 E-mail address: [email protected] (A. Lewin). 25 26 27 Abstract 28 29 We compare Ethiopian glaciogenic sandstone of the Late Ordovician 30 and Carboniferous–Permian Gondwana glaciations petrographically 31 and geochemically to provide insight into provenance, transport, and 32 weathering characteristics. Although several studies deal with the 33 glacial deposits in northern Africa and Arabia, the distribution of ice 34 sheets and continent-wide glacier dynamics during the two 35 glaciations remain unclear. Provenance data on Ethiopian Palaeozoic 36 sedimentary rocks are scarce. The sandstones of the Late Ordovician 37 glaciation are highly mature with an average quartz content of 95% 1 38 and an average chemical index of alteration of 85, pointing to intense 39 weathering and reworking prior to deposition.
    [Show full text]
  • Hewn Churches and Its Surroundings, Tigray Region, Northern Ethiopia
    Research Article http://dx.doi.org/10.4314/mejs.v9i2.4 Geological and Geomechanical Properties of Abraha-Atsibha and Wukro rock- hewn churches and its surroundings, Tigray Region, Northern Ethiopia Asmelash Abay*, Gebreslassie Mebrahtu and Bheemalingeswara Konka School of Earth Sciences, Mekelle University, P.O.Box:231, Mekelle, Ethiopia (*[email protected]). ABSTRACT Globally well-known ancient rock-hewn churches are present in Ethiopia in general and particularly in the central and eastern parts of Tigray regional state. They are important sites of heritage and tourism. Most of them are facing destabilization problem in different degree due to natural and anthropogenic factors. Among the affected, two churches hewn into sandstone located near Abreha-Atsibaha and Wukro (Kirkos/Cherkos church) in Tigray region were chosen for detailed study in terms of geological and engineering geological condition of the rocks in to which they are hewn. Both of them are affected by weathering and seepage. Both are carved into Mesozoic Adigrat sandstone that occupy higher elevations in topography, red in color and with iron and silica-rich alternating bands. Petrographic data suggest that the rock is dominated by quartz followed by feldspars; opaque and heavy minerals; pore spaces and carbonate/iron/silica cement. The rock is characterized by low to medium unconfined compressive strength. The alternating bands with varying mineralogical composition differ in mechanical properties and are responding differently to weathering and erosion. This is resulting in the development of minor spalling, pitting etc in the pillars, walls and roofs of the churches. Keeping the geological condition in view remedial measures are to be planned to minimize deterioration with time.
    [Show full text]
  • Geology and Petroleum Resources of Central and East-Central Africa by James A. Peterson* Open-File Report 85-589 This Report Is
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology and petroleum resources of central and east-central Africa By James A. Peterson* Open-File Report 85-589 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature Missoula, Montana 1985 CONTENTS Page Abs tract 1 Introduction 2 Sources of Information 2 Geography 2 Acknowledgment s 2 Regional geology 5 Structure 5 Horn of Africa 5 Plateau and rift belt 11 Red Sea and Gulf of Aden Basins 13 Central Africa interior basins 13 Upper Nile Basin (Sudan trough) 13 Chad, Doba-Doseo (Chari), and lullemmeden (Niger) Basins 13 Benue trough 15 Stratigraphy 15 Precambrian 19 Paleozoic 19 Mesozoic 21 East-central Africa 21 Jurassic 21 Cretaceous 22 Tertiary 22 Central Africa interior basins 26 Benue trough 27 Petroleum geology 27 Somali basin 28 Res ervo i r s 2 9 Source rocks 29 Seals 29 Traps 2 9 Estimated resources 30 Plateau and rift belt 30 Red Sea Basin (western half) 30 Reservoirs 30 Source rocks 34 Seals 34 Traps 34 Estimated resources 34 Central Africa interior basins 34 Reservoirs, source rocks, seals 36 Traps 36 Estimated resources 36 Benue trough 40 Res er voi r s 4 0 Source rocks 40 Seals 40 Traps 40 Estimated resources 40 CONTENTS (continued) Page Resource assessment 42 Procedures 42 As s es smen t 4 3 Comments 43 Selected references 45 ILLUSTRATIONS Figure 1. Index map of north and central Africa 3 2. Generalized structural map of central and east Africa 4 3.
    [Show full text]
  • Micropaleontology and Facies Analysis of Carbonate Unit in Mugher Area (Sodoble Stratigraphic Section), North Western Ethiopia
    ADDIS ABABA UNIVERSITY SCHOOL OF GRADUATE STUDIES SCHOOL OF EARTH SCIENCES MICROPALEONTOLOGY AND FACIES ANALYSIS OF CARBONATE UNIT IN MUGHER AREA (SODOBLE STRATIGRAPHIC SECTION), NORTH WESTERN ETHIOPIA MSc. THESIS BY: BERTUKAN GEBRE DETEBO A thesis submitted to the school of Graduate Studies of Addis Ababa University in the partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences (Paleontology and Paleoenvironment) May, 2018 Addis Ababa, Ethiopia ADDIS ABABA UNIVERSITY SCHOOL OF GRADUATE STUDIES SCHOOL OF EARTH SCIENCES MICROPALEONTOLOGYAND FACIES ANALYSIS OF CARBONATE UNIT IN MUGHER AREA (SODOBLE STRATIGRAPHIC SECTION), NORTH WESTERN ETHIOPIA BY BERTUKAN GEBRE DETEBO ADVISOR: BALEMWAL ATNAFU (PhD) A thesis submitted to the School of Graduate Studies of Addis Ababa University in Partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences (Paleontology and Paleoenvironment) May 30, 2018 Addis Ababa, Ethiopia ADDIS ABABA UNIVERSITY SCHOOL OF EARTH SCIENCES MICROPALEONTOLOGY AND FACIES ANALYSIS OF CARBONATE UNIT IN MUGHER AREA (SODOBLE SECTION), NORTH WESTERN ETHIOPIA BY BERTUKAN GEBRE DETEBO Approved by the Examining Committee Dr. Balemwal Atnafu ------------ -------------- Head, School of Earth Sciences Signature Date Dr. Balemwal Atnafu -------------- -------------- Advisor Signature Date Examiner --------------- ------------- Dr. Mulugeta Fesseha Signature Date Dr. Gilamichael Kidanemariam ---------------- -------------- Examiner Signature Date May, 2018 Addis Ababa,
    [Show full text]
  • Mass Movement Mapping for Geomorphological Understanding and Sustainable Development: Tigray, Ethiopia Catena
    Catena 75 (2008) 45–54 Contents lists available at ScienceDirect Catena journal homepage: www.elsevier.com/locate/catena Mass movement mapping for geomorphological understanding and sustainable development: Tigray, Ethiopia J. Moeyersons a,⁎, M. Van Den Eeckhaut b, J. Nyssen c, Tesfamichael Gebreyohannes d, J. Van de Wauw e, J. Hofmeister f, J. Poesen b, J. Deckers g, Haile Mitiku h a Royal Museum for Central Africa,B-3080 Tervuren, Belgium b Physical and Regional Geography Research Group, K.U. Leuven, Celestijnenlaan 200 E, B-3001 Heverlee, Belgium c Geography Department, Ghent University, Krijgslaan 281, B-9000 Ghent, Belgium d Mekelle University, Department of Applied Geology, P.O. Box 231, Mekelle, Ethiopia e Department of Geology and Soil Science, Ghent University, Krijgslaan 281 S8, B-9000 Ghent, Belgium f Department of Geography, University of Marburg, Germany g Division Soil and Water Management, K.U. Leuven, Celestijnenlaan 200 E, B-3001 Heverlee, Belgium h Mekelle University, P.O. Box 231, Mekelle, Ethiopia ARTICLE INFO ABSTRACT Keywords: Mass movement topography characterises the escarpments and piedmont zones of the tabular ridges in the Creep western part of the Mekelle outlier, Tigray, Ethiopia. Several types of mass movements can be distinguished. Ethiopia The first type is rockfall produced by 357 km rocky escarpments and cliffs during the rainy season. In the Landslides study area, every current kilometer of Amba Aradam sandstone cliff annually produces 3.7 m3 of rock Mass movements fragments. However, this is an under-estimation of the actual cliff and escarpment evolution, which is also Rockfall characterised by debris slides and small rock slides.
    [Show full text]
  • University of Gondar Institutional Repository
    University of Gondar College of Natural and Computational Sciences Department of Geology MSc program in Paleontology and Paleoenvironment MSc thesis Entitled Upper Jurassic Bivalves of Dejen - Gohatsion Section, Blue Nile Basin, Central Ethiopia by WORKU BIRHAN Advisor: - Dawit lebene (PHD.) September,2020 Gondar, Ethiopia College of Natural and Computational Sciences Department of Geology MSc program in Paleontology and Paleoenvironment MSc thesis Entitled Upper Jurassic Bivalves of Dejen - Gohatsion Section, Blue Nile Basin, Central Ethiopia by WORKU BIRHAN Approved by Wuletaw mulualem __________ _________ Head, Department of geology signature Date Dr. Dawit Lebenie __________ _________ Advisor Signature Date Dr. Balemwal Atnafu __________ ________ External Examiner Signature Date Wuletaw Mulualem _________ ________ Assistant Prof Internal Examiner Signature Date Zerihun Dawit _________ ________ Assistant Prof Cherman Signature Date Declaration I declare that this thesis is my original master degree work and has not been submitted to any university or institution in the past for the award of any degree or diploma at any other university. All sources and materials used for this thesis work have been well referenced and duly acknowledged. Worku Birhan __________ __________ Student Signature Date Approved by Dr. Dawit Lebene __________ __________ (Advisor) Signature Date ABSTRACT The study area has excellent exposures of upper Jurassic sedimentary rock which is situated in north western Ethiopian plateau. This research is focused on detail field investigation, description and systematics of upper Jurassic bivalves for the reconstruction of depositional environment and ecology. Different scientific methods were followed in order to achieve and accomplish the stated research problem and the objectives of the study with three main methods.
    [Show full text]
  • Building Stone of Central and Southern Ethiopia: Deposits and Resource Potential
    NGU-BULL 436,2000 - PAGE 175 Building stone of central and southern Ethiopia: deposits and resource potential HAILEYE SU SWALLE, SINTAYEHU ZEWDE& TOM HELDAL Walle, H., Zewde, S. & Heldal, T. 2000: Buildin g stone of central and southern Ethiopi a: deposit s and resource pot ent ial. Norges geologiske undersekeise Bulletin 436, 175-182. The bedrock geology of Eth iopia exhibits a variety of rock types th at can pote ntially be developed for bu ilding sto ne prod uction. The ETH IONOR project has so far includ ed investigation of such resources in t he southern and central part s of Ethi op ia. Wit hin t he Precamb rian, th ere are several deposits of pin k and grey granitoids, grey and w hite marble, soapstone and serpent inite; a number of these deposits are current ly exploite d by Ethiopian companies. Mesozoic sandstone and limestone are fou nd at several places in the east-central and central part of the cou ntry, and in addition to t he small number of exist ing quarry opera tio ns, a potent ial existsfor the developme nt of new deposits. Basalt, tufts and igni mbrite are exte nsively used for local housing and construction in Ethiopia. Such resources represent a potential for low-cost supp ly of an excellent construction material. and could be developed furt her. Hail eyesus Walle & Sintayehu Zewde, Eth iopian Institu te of Geological Surveys, Add isAbaba, Ethiopia. Tom Heldal, Norgesgeo /ogi ske undersekelse, N-749 7Trond heim, Nor way. tance th at th e depo sit can give commercial-sized blocks Introduction (minimum 220 x 120 x 100 cm) and/o r slabs of uniform qual­ Durin g th e last 20 years, th e production and use of building ity, wit h produ ction costs matching th e market price (Shad­ stone1 hassteadily increased wo rldwide, and today stone has mon 1996).
    [Show full text]
  • By TADESSE B. ALEMU Bachelor of Science in Earth Sciences Addis Ababa University Addis Ababa, Ethiopia 2009 Master of Science
    INTRACONTINENTAL SAGS (ICONS) FORMATION, EXHUMATION AND LANDSCAPE EVOLUTION: THE ETHIOPIAN TESTIMONY By TADESSE B. ALEMU Bachelor of Science in Earth Sciences Addis Ababa University Addis Ababa, Ethiopia 2009 Master of Science in Earth Sciences (Fossil Fuel Exploration) Addis Ababa University Addis Ababa, Ethiopia 2012 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, 2019 INTRACONTINENTAL SAGS (ICONS) FORMATION, EXHUMATION AND LANDSCAPE EVOLUTION: THE ETHIOPIAN TESTIMONY Dissertation Approved: Dr. Mohamed Abdelsalam, Chair Dissertation Adviser Dr. Estella Atekwana Dr. Jack Pashin Dr. Runar Nygaard ii ACKNOWLEDGEMENTS My greatest gratitude goes to my advisor, Dr. Mohamed Abdelsalam, whose work and enthusiasm for advancing the geology of Africa was an important motivation that ultimately led me to join Oklahoma State University. His mentorship and patience has been an invaluable asset that helped me navigate the most difficult times. Thank you for giving me the latitude to explore, and for helping me acquire the versatility needed to grow. I am grateful for the opportunities and exposures that my Committee member Dr. Estella Atekwana provided. Thank you to Committee members Dr. Jack Pashin, and Dr. Nygaard Runar for their time and valuable suggestions. Special thanks to Dr. Kevin Mickus for his help with potential data and methods. I am grateful to Statoil whose funding to my advisor made possible most of my work in the Mekele Basin. I thank the Boone Pickens School of Geology for the fellowships, and assistantships. I immensely benefited from the discussion at the Tectonics Research Group meetings.
    [Show full text]
  • 453719 1 En Bookfrontmatter 1..34
    GeoGuide Series Editors Wolfgang Eder, University of Munich, Munich, Germany Peter T. Bobrowsky, Geological Survey of Canada, Natural Resources Canada, Sidney, BC, Canada Jesús Martínez-Frías, CSIC-Universidad Complutense de Madrid, Instituto de Geociencias, Madrid, Spain Axel Vollbrecht, Geowissenschaftlichen Zentrum der UniversitätGöttingen, Göttingen, Germany The GeoGuide series publishes travel guide type short monographs focussed on areas and regions of geo-morphological and geological importance including Geoparks, National Parks, World Heritage areas and Geosites. Volumes in this series are produced with the focus on public outreach and provide an introduction to the geological and environmental context of the region followed by in depth and colourful descriptions of each Geosite and its significance. Each volume is supplemented with ecological, cultural and logistical tips and information to allow these beautiful and fascinating regions of the world to be fully enjoyed. More information about this series at http://www.springer.com/series/11638 Jan Nyssen Á Miro Jacob Á Amaury Frankl Editors Geo-trekking in Ethiopia’s Tropical Mountains The Dogu’a Tembien District 123 Editors Jan Nyssen Miro Jacob Department of Geography Department of Geography Ghent University Ghent University Ghent, Belgium Ghent, Belgium Amaury Frankl Department of Geography Ghent University Ghent, Belgium ISSN 2364-6497 ISSN 2364-6500 (electronic) GeoGuide ISBN 978-3-030-04954-6 ISBN 978-3-030-04955-3 (eBook) https://doi.org/10.1007/978-3-030-04955-3 Library
    [Show full text]
  • In Vitro Production of Virus Free Sweet Potato
    SINET: Ethiop. J. Sci., 39(1): 34–49, 2016 ISSN: 0379–2897 (Print) © College of Natural Sciences, Addis Ababa University, 2016 2520–7997 (Online) SULFIDES, STABLE ISOTOPES AND OTHER DIAGENETIC FEATURES OF THE MESOZOIC CARBONATE-MARL-SHALE SUCCESSION IN NORTHERN ETHIOPIA Worash Getaneh School of Earth Sciences, Addis Ababa University, PO Box 1176, Addis Ababa, Ethiopia. E-mail: [email protected] ABSTRACT: This study investigates the carbonate-marl-shale succession (usually called Antalo Limestone and Agula Shale) in northern Ethiopia. The purpose of this study is to explain the diagenetic features, diagenetic environments and factors controlling them. The study is conducted by characterizing the whole rock carbon and oxygen isotopes, trace elements, mineral and textural features. Thirty samples were analyzed for carbon and oxygen isotopes, Sr and Mn; the latter two elements are chosen because of their sensitivity to diagenetic alterations. Moreover, 24 thin sections and 5 polished sections were investigated using petrographic and ore microscopes. The diagenetic features identified include sulfidation, micritization, silicification, cementation, neomorphism, pressure solution, vein development and hematitization. Oxidation rims around early diagenetic sulfides, development of clear spary calcite cement, and development dissolution features are common in the Agula Shale and lower part of Antalo Limestone. The δ13C of the Antalo Limestone ranges from -0.23‰ to 2.22‰ PDB and δ18O‰ is between -7.42‰ and -3.16‰ PDB. In the Agula Shale δ13C is between -3.25‰ and -0.12‰ and δ18O ranges from -17.07‰ to -6.48‰. The Mn/Sr ratio is higher for the Agula Shale (2.12) compared to that of the Antalo Limestone (0.35).
    [Show full text]
  • Spatial Patterns of Old, Deep-Seated Landslides: a Case-Study in the Northern Ethiopian Highlands
    Geomorphology 105 (2009) 239–252 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Spatial patterns of old, deep-seated landslides: A case-study in the northern Ethiopian highlands M. Van Den Eeckhaut a,b,⁎, J. Moeyersons c, J. Nyssen d, Amanuel Abraha e, J. Poesen a, Mitiku Haile e, J. Deckers f a Physical and Regional Geography Research Group, K.U. Leuven, Celestijnenlaan 200 E, B-3001 Heverlee, Belgium b Research Foundation-Flanders, Belgium c Royal Museum for Central Africa, B-3080 Tervuren, Belgium d Department of Geography, Ghent University, B-9000 Ghent, Belgium e Mekelle University, Mekelle, Ethiopia f Institute for Land and Water Management, K.U. Leuven, B-3001 Heverlee, Belgium article info abstract Article history: During the last decade, slope failures were reported in a 500 km2 study area in the Geba–Werei catchment, Received 17 March 2008 northern Ethiopia, a region where landslides were not considered an important hazard before. Field Received in revised form 24 September 2008 observations, however, revealed that many of the failures were actually reactivations of old deep-seated Accepted 29 September 2008 landslides after land use changes. Therefore, this study was conducted (1) to explore the importance of Available online 25 October 2008 environmental factors controlling landslide occurrence and (2) to estimate future landslide susceptibility. A landslide inventory map of the study area derived from aerial photograph interpretation and field checks Keywords: Ethiopian highlands shows the location of 57 landslides and six zones with multiple landslides, mainly complex slides and debris Landslide susceptibility flows. In total 14.8% of the area is affected by an old landslide.
    [Show full text]
  • Mesozoic Mekele Sedimentary Basin in Ethiopia: an Example of an Exhumed Intracontinental Sag (ICONS) Basin
    Journal of African Earth Sciences 143 (2018) 40e58 Contents lists available at ScienceDirect Journal of African Earth Sciences journal homepage: www.elsevier.com/locate/jafrearsci The Paleozoic e Mesozoic Mekele Sedimentary Basin in Ethiopia: An example of an exhumed IntraCONtinental Sag (ICONS) basin * Tadesse Alemu a, Mohamed G. Abdelsalam a, , Enkurie L. Dawit b, Balemwal Atnafu c, Kevin L. Mickus d a Boone Pickens School of Geology, Oklahoma State University, 105 Noble Research Center, Stillwater, OK, 74078, USA b Department of Geology, University of Gondar, P.O. Box 196, Gondar, Ethiopia c School of Earth Sciences, Addis Ababa University, P.O. Box 1176, Addis Ababa, Ethiopia d Department of Geography, Geology and Planning, Missouri State University, 901 S., Springfield, MO, USA article info abstract Article history: We investigated the evolution of the Mekele Sedimentary Basin (MSB) in northern Ethiopia using Received 15 November 2017 geologic field and gravity data. The depth to Moho and lithospheric structure beneath the basin was Received in revised form imaged using two-dimensional (2D) radially-averaged power spectral analysis, Lithoflex three- 6 March 2018 dimensional (3D) forward and inverse modeling, and 2D forward modeling of the Bouguer gravity Accepted 12 March 2018 anomalies. Previous studies proposed that the basin was formed as part of a multi-branched rift system Available online 15 March 2018 related to the breakup of Gondwana. Our results show that the MSB: (1) is circular to elliptical in map view and saucer shaped in cross sectional view, (2) is filled with terrestrial and shallow marine sedi- Keywords: fi Mekele Sedimentary Basin mentary rocks, (3) does not signi cantly structurally control the sedimentation and the major faults are IntraCONtinental Sag (ICONS) post-depositional, (4) is characterized by a concentric gravity minima, (5) is underlain by an unstretched Exhumation crust (~40 km thick) and thicker lithosphere (~120 km thick).
    [Show full text]