African Basins
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Environmental and Social Impact Assessment
Final Environmental and Social Impact Assessment Report for the Proposed 100MW Solar Independent Power Plant and 18 KM Transmission Line Project, Ganjuwa Local Government Area, Bauchi State by Nigerian Solar Capital Partners/Globeleq/ARM- Harith June 2017 100 MW Independent Solar Power Plant, Bauchi State Environmental and Social Impact Assessment Table of Contents List of Tables iii List of Figures iv List of Acronyms and Abbreviations v List of ESIA Preparers viii Executive Summary ix Chapter One: Introduction 1.1 Background 1-1 1.2 Overview 1-2 1.3 Project Scope 1-2 1.4 Project Location 1-3 1.5 Study Objectives and Terms of Reference 1-6 1.6 Report Structure 1-6 Chapter Two: Policy, Legal and Administrative Framework 2.1 Applicable National Policies 2-8 2.2 Applicable National Regulations 2-10 2.3 Institutional Framework 2-14 2.4 Applicable International Agreements and Policies 2-19 2.5 Permit Requirements 2-21 Chapter Three: Project Description 3.1 Project Overview 3-23 3.2 Project Requirements 3-23 3.3 Project Components 3-24 3.4 Operation and Maintenance 3-34 3.5 Project Activities 3-35 3.5.1 Construction 3-35 3.6 Implementation Schedule 3-35 Chapter Four: Description of the Project Environment 4.1 General 4-38 4.2 Study Area and Location 4-38 4.2.1 Reconnaissance Field Visit 4-38 4.2.2 Baseline Data Acquisition 4-38 4.2.3 Sampling Design 4-45 4.2.4 Field Sampling Methods 4-45 4.2.5 Laboratory Methods 4-47 4.3 Bio-Physical Environmental Baseline Condition 4-47 4.3.1 Climate and Meteorology 4-47 4.3.2 Ambient Air Quality 4-52 4.3.2.1 -
Apatite Thermochronology in Modern Geology
Downloaded from http://sp.lyellcollection.org/ by guest on September 24, 2021 Apatite thermochronology in modern geology F. LISKER1*, B. VENTURA1 & U. A. GLASMACHER2 1Fachbereich Geowissenschaften, Universita¨t Bremen, PF 330440, 28334 Bremen, Germany 2Institut fu¨r Geowissenschaften, Ruprecht-Karls-Universita¨t Heidelberg, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany *Corresponding author (e-mail: fl[email protected]) Abstract: Fission-track and (U–Th–Sm)/He thermochronology on apatites are radiometric dating methods that refer to thermal histories of rocks within the temperature range of 408–125 8C. Their introduction into geological research contributed to the development of new concepts to interpreting time-temperature constraints and substantially improved the understanding of cooling processes within the uppermost crust. Present geological applications of apatite thermochronological methods include absolute dating of rocks and tectonic processes, investigation of denudation histories and long-term landscape evolution of various geological settings, and basin analysis. Thermochronology may be described as the the analysis of radiation damage trails (‘fission quantitative study of the thermal histories of rocks tracks’) in uranium-bearing, non-conductive using temperature-sensitive radiometric dating minerals and glasses. It is routinely applied on the methods such as 40Ar/39Ar and K–Ar, fission minerals apatite, zircon and titanite. Fission tracks track, and (U–Th)/He (Berger & York 1981). are produced continuously through geological time Amongst these different methods, apatite fission as a result of the spontaneous fission of 238U track (AFT) and apatite (U–Th–Sm)/He (AHe) atoms. They are submicroscopic features with an are now, perhaps, the most widely used thermo- initial width of approximately 10 nm and a length chronometers as they are the most sensitive to low of up to 20 mm (Paul & Fitzgerald 1992) that can temperatures (typically between 40 and c. -
AJST) Science and Engineering Series Vol
African Journal of Science and Technology (AJST) Science and Engineering Series Vol. 4, No. 2, pp. 80-89 ISOTOPE AND GEOCHEMICAL CHARACTERIZATION OF SURFACE AND SUBSURFACE WATERS IN THE SEMI-ARID SOKOTO BASIN, NIGERIA S.M.A. Adelana1, P.I. Olasehinde1 and P.Vrbka2 1Department of Geology & Mineral Sciences, University of Ilorin, P.M.B. 1515, Ilorin, Kwara State, Nigeria. 2Kaupstrasse 37, Germany (formerly Geology Institute, Technical University Darmstadt, Germany). ABSTRACT:- Stable isotopes and geochemical studies have been applied in the investigation of groundwater resources in Sokoto Basin, northwestern Nigeria. Generally, the characteristic hydrochemical classification in the study area is calcium-alkali-bicarbonate. Surface waters are characterized by alkali-calcium-bicarbonate while groundwater is of Ca-Mg-HCO3. The plot of δ18O versus δ2H shows that five isotopic groups can be distinguished. Group I-III is of groundwater origin while group IV and V represent surface water. A combination of the hydrochemical and isotope data (14C, 13C and 3H) reveals the Sokoto basin aquifers generally contains good quality groundwater of Holocene age (100 to 10,000 years BP). Keywords: stable isotopes, geochemical characterization, groundwater, Sokoto Basin. INTRODUCTION condition by one kilometre yearly into northern Nigeria threatens agriculture. It is in the light of this that the Northwestern Nigeria is a region with great potential for Federal government of Nigeria under a joint project with future large-scale economic development due to warm the International Atomic and Energy Agency, Vienna has temperatures and bountiful resources; including thermal planned a number of irrigation schemes in order to energy, farmlands and minerals. Water resources data in increase agricultural activities in the area to two planting this area, as far back as the 60s, are available in literature seasons, thereby boosting food production. -
Tracing the Central African Rift and Shear Systems Offshore Onto
Tracing the West and Central African Rift and Shear Systems offshore onto oceanic crust: a ‘rolling’ triple junction William Dickson (DIGs), and James W. Granath, PhD, (Granath & Associates) Abstract Compared to the understood kinematics of its continental margins and adjacent ocean basins, the African continent is unevenly or even poorly known. Consequently, the connections from onshore fault systems into offshore spreading centers and ridges are inaccurately positioned and inadequately understood. This work considers a set of triple junctions and the related oceanic fracture systems within the Gulf of Guinea from Nigeria to Liberia. Our effort redefines the greater Benue Trough, onshore Nigeria, and reframes WCARS (West and Central African Rift and Shear Systems) as it traces beneath the onshore Niger Delta and across the Cameroon Volcanic Line (CVL), Figure 1. We thus join onshore architecture to oceanic fracture systems, forming a kinematically sound whole. This required updating basin outlines and relocating mis- positioned features, marrying illustrations from the literature to imagery suitable for basin to sub- basin mapping. The resulting application of systems structural geology explains intraplate deformation in terms of known structural styles and interplay of their elements. Across the Benue Trough and along WCARS, we infer variations in both structural setting and thermal controls that require further interpretation of their petroleum systems. Introduction Excellent work has defined Africa's onshore geology and the evolution and driving mechanisms of the adjacent (particularly the circum-Atlantic) ocean basins. However, understanding of the oceanic realm has outpaced that of the continent of Africa. This paper briefly reviews onshore work. We then discuss theoretical geometry of tectonic boundaries (including triple junctions) and our data (sources and compilation methods). -
The Mesozoic to Early Cenozoic Magmatism of the Benue Trough (Nigeria); Geochemical Evidence for the Involvement of the St Helen
JOURNAL OF PETROLOGY VOLUME 37 NUMBER 6 PAGES 1341-1358 1996 C. COULON1*, P. VIDAL2, C. DUPUY3, P. BAUDIN1, M. POPOFF*, H. MALUSKI5 AND D. HERMITTE1 'PETROLOGIE MAGMATIQUE, URA 1277, CEREGE, BP 80, 15545 AIX EN PROVENCE CEDEX 4, FRANCE 'CENTRE DE RECHERCHES VOLCANOLOGIQUES, URA 10, 63038 CLERMONT FERRAND CEDEX, FRANCE 'CENTRE GEOLOGIO.UE ET GEOPHYSIO.UE, CNRS, PLACE BATAILLON, J4095 MONTPELLIER CEDEX, FRANCE *INSTITUT DE GEODYNAMIQ.UE, URA 1279, UNIVERSITE DE NICE—SOPHIA ANTIPOLIS, AVENUE EINSTEIN, 06560 VALBONNE, FRANCE JLABORATOIRE DE GEOCHRONOLOGIE—GEOCHIMIE, URA 176J, PLACE BATAILLON, 34095 MONTPELLIER CEDEX, FRANCE The Mesozoic to Early Cenozoic Downloaded from https://academic.oup.com/petrology/article/37/6/1341/1406521 by guest on 28 September 2021 Magmatism of the Benue Trough (Nigeria); Geochemical Evidence for the Involvement of the St Helena Plume The Benue Trough is a continental rift related to the opening of Equatorial Atlantic. Moreover, the geochemical similarity the equatorial domain of the South Atlantic which was initi- between the alkaline magmatism of the Benue Trough and that ated in Late Jurassic-Early Cretaceous times. Highly diversi- of the Cameroon Line suggests that both magmatic provinces fied and volumetrically restricted Mesozoic to Cenozoic were related to the St Helena plume. Finally, the temporal magmatic products are scattered throughout the rift. Three per- change of the mantle sources observed in the Benue Trough can iods of magmatic activity have been recognized on the basis of be accounted for by the recent models of plume dynamics, in the *°Ar-39Ar ages: 147-106 Ma, 97-81 Ma and 68-49 Ma. -
Oblique Rifting of the Equatorial Atlantic: Why There Is No Saharan Atlantic Ocean
Originally published as: Heine, C., Brune, S. (2014 online): Oblique rifting of the Equatorial Atlantic: Why there is no Saharan Atlantic Ocean. – Geology 10.1130/G35082.1. Oblique rifting of the Equatorial Atlantic: Why there is no Saharan Atlantic Ocean 1 2,1 Christian Heine , Sascha Brune 1 EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia 2 Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Section 2.5, Geodynamic Modelling, Potsdam, Germany ABSTRACT Rifting between large continental plates results in either continental breakup and the formation of conjugate passive margins or rift abandonment and a set of aborted rift basins. The driving mechanisms behind “successful” or “failed” rifting have so far never been scrutinized by joint kinematic and forward numerical modelling. We analyse the Early Cretaceous extension between Africa and South America which was preceded by about 20-30 Myrs of extensive rifting prior to the final separation between the two plates. While the South and Atlantic conjugate margins continued into seafloor spreading mode, forming the Atlantic ocean basin, Cretaceous-aged African intraplate rifts eventually “failed” soon after South America broke up from Africa. We address the spatio-temporal dynamics of rifting in domains by comparing a new plate kinematic model for the South Atlantic and 3D forward rift models. This joint approach elucidates (1) the dynamic competition of Atlantic and extensional systems, (2) two stage kinematics of the South Atlantic rift system, and (3) the acceleration of the South American plate prior to final break-up. We suggest that obliquity the success of the Equatorial Atlantic rift, ultimately prohibiting the formation of a “Saharan Atlantic Ocean” in the Early Cretaceous, and exerting a primary control on the increase in observed extensional velocities between the South American and African plates. -
The Aim of the Project Is to Carry out Integrated Studies of the Anambra
Preliminary Integrated Hydrocarbon Prospectivity Evaluation of the Bida Basin in North Central Nigeria By N. G. Obaje1, D. O. Balogu1, A. Idris-Nda2, I. A. Goro2, S. I. Ibrahim1, M. K. Musa1, S. H. Dantata2, I. Yusuf1, N. Mamud-Dadi1, I. A. Kolo1+ Abstract The Bida Basin is a NW-SE trending intracratonic structure extending from slightly south of Kontagora in Niger State in the north to the area slightly beyond Lokoja (Kogi State) in the south. All geological maps available on the Bida Basin had lumped the sediments in the basin as one undifferentiated Nupe Sandstone, making it impossible to infer the prospectivity of the basin for hydrocarbon exploration. The delineation of inferred boundaries between the formations in the basin is a significant initial criterion in evaluating the hydrocarbon prospectivity. The formations deposited in the Bida Basin comprise the Bida Sandstone at the base, followed successively upward by the Sakpe, Enagi and Batati Formations in the Northern/Central Bida Basin while the Lokoja, Patti and Agbaja Formations constitute lateral equivalents in the Southern Bida Basin. An institutional research project of the Ibrahim Badamasi Babangida University Lapai (IBBUL), supported by the Niger State Government, has carried out preliminary geological mapping and completed a prospectivity map for the Bida Basin. Geochemical analysis of samples from drilled shallow wells (at Agaie and Kudu) and outcrops was also undertaken along with interpretation of geophysical aeromagnetic data. From the preliminary geological map prepared, prospective areas, ranked as Less Prospective, Prospective and More Prospective are discernable. Geochemical data show that mainly gas and some oil would have been generated within the Prospective and More Prospective sections in the basin. -
The Eastern Sirte Basin, Libya
D-18 REVIEW OF THE REMAINING POTENTIAL IN THE EASTERN SIRTE BASIN , LIBYA RUT GE R G RAS a nd DREG J . AMBROSE Scfflumberger O ilfreld Services . Schlumberger House. Buckingham Gate , Gatwíck Airport West Sussex RH6 ONZ, UK A bstract In the Sine Basfin more than 1600 exploration wens drilled since 195 6 have discovered an estimated total of 130 bipion barrels of original all-equivalent in place (Thomas 1995, Gras & Thusu 1996). The play types testel successfully in the Sirte Basfin are botte carbonate and siliciclastic plays. The first category are predominantly Paleocene carbonate buildups, occurring in the tentral and western party of the basin, while Middle Eocene nummulite shoals are praductive in the southeast Sirte Basfin (e .g . Gialo field) . The oilfíelds in the Sine Basfin witte siliciclastic reservoirs are principally related to the consecutive Midfile Triassic and Late .lurassic-Early Cretaceotis rifting of the basin, and occur in the eastern part of the Sirte Basfin (fig. 1 ) . 20 MEDITERRANEAN N ,--'J 777 AK HD A R ~ I T CYRENAICA - d PLATFORM . 3 0 ry v 1 30 W EST ER N B AR H ~~- JAG HBU C S H EL F q~ HAME IM AT TROUGH Dr~ G IAL~-MESS LAH H4GH LE G END r~r n a SAR IR TROUGH G'l ,~T FQRM 0 ST RUCTU RAI IOWS ZEE YEN SOU T H 6F P RFSSIO N PLATFORM T E RTIARY YOL CANICS CAM6RIAN -óft Dl'11-1 CI ,: N SO UTHERN ~ S HE L F SARIR 20 2 0 TIB E STI 0 200 4 00 km 20 Figurc l : 5tructural overview of the Sirte Basfin. -
Structure and Evolution of the Petroliferous Euphrates Graben System, Southeast Syria1
Structure and Evolution of the Petroliferous Euphrates Graben System, Southeast Syria1 Robert K. Litak,2 Muawia Barazangi,3 Graham Brew,3 Tarif Sawaf,4 Anwar Al-Imam,4 and Wasif Al-Youssef4 ABSTRACT Cenozoic inversion of some structures also is evi- dent. Approximately 30 oil fields have been dis- The northwest-trending Euphrates graben sys- covered in the Euphrates graben system since tem is an aborted intracontinental rift of Late 1984. Recoverable reserves discovered to date Cretaceous age that has subsequently been hidden reportedly exceed 1 billion barrels of oil and less- by Cenozoic burial. Approximately 100 km wide, er amounts of gas. Light oil is primarily found in the system comprises an extensive network of Lower Cretaceous sandstone reservoirs juxtaposed grabens and half grabens extending some 160 km by normal faulting against Upper Cretaceous synrift from the Anah graben in western Iraq to the sources and seals. Palmyride fold belt in central Syria, where it becomes more subdued. The youngest prerift rocks are presently at a maximum depth of about 5 km. INTRODUCTION Based primarily on interpretation of 1500 km of seismic reflection profiles and data from 35 wells, Recent detailed studies on a number of continen- we mapped a complex network of numerous tal rifts have shed considerable light on the archi- branching normal and strike-slip faults, generally tecture and evolution of these types of basins (e.g., striking northwest and west-northwest. Both Rosendahl, 1987; Morley, 1995). Continental rifts branched and single-strand linear normal faults of hosting major hydrocarbon accumulations include generally steep dip, as well as positive and negative the North Sea (e.g., Stewart et al., 1992), Gulf of flower structures, are manifest on seismic sections. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics. -
Towards Interactive Global Paleogeographic Maps, New Reconstructions at 60, 40 and 20 Ma
Earth-Science Reviews 214 (2021) 103508 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete a,b,*, G. Dupont-Nivet a,c, A. Licht d, D.J.J. van Hinsbergen e, P. Roperch a, M. G. Mihalynuk f, S.T. Johnston g, F. Guillocheau a, G. Baby a, F. Fluteau h, C. Robin a, T.J. M. van der Linden e,i, D. Ruiz c, M.L.J. Baatsen j a G´eosciences Rennes, UMR CNRS 6118, Rennes, 35042 Rennes Cedex, France b Departamento de Geología, Facultad de Ciencias Físicas y Matematicas,´ Universidad de Chile, Chile c Universitat¨ Potsdam, Institute of Geoscience, 14476 Potsdam, Germany d Centre Europ´een de Recherche et d’Enseignement des G´eosciences de l’Environnement (Cerege), UMR CNRS 7330, 13545 Aix-en-Provence, France e Department of Earth Sciences, Utrecht University, Princetonlaan 8a, 3584 CB, Utrecht, the Netherlands f British Columbia Geological Survey, Vancouver, Canada g Department of Earth and Atmospheric Sciences, University of Alberta, Canada h Universit´e de Paris, Institut de physique du globe de Paris, CNRS, F-75005 Paris, France i Thomas van der Linden – LinGeo, Berlin, Germany j IMAU, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands ARTICLE INFO ABSTRACT Keywords: Paleogeographic maps are essential tools for understanding Earth system dynamics. They provide boundary Paleogeographic maps conditions for climate and geodynamic modelling, for analysing surface processes and biotic interactions. Paleoelevation However, the temporal and spatial distribution of key features such as seaways and mountain belts that govern Cenozoic climate changes and biotic interchange differ between various paleogeographies that require regular updates Eocene-Oligocene transition with new data and models. -
Council for Innovative Research Peer Review Research Publishing System Journal of Advances in Physics
ISSN 2347-3487 Evaluation of the Existing State of Geothermal Exploration and Development in Nigeria Sedara, Samuel Omosule1, Joshua,E.O 2 1Oduduwa University, Ipetumodu, Department of Physical Sciences [email protected] 2University of Ibadan, Department of Physics, Ibadan Nigeria ABSTRACT Relatively little expenditure for hydroelectricity and fossil fuels have had a restraining influence on levels of exploration and development for geothermal energy resources in Nigeria for the past several years. The focus of development has been in the areas of low temperature geothermal energy involving the exploration and assessment of hot spring resources primarily for recreational applications – although possibly for other direct uses depending on local infrastructure and access to appropriate energy markets. The geological structure of Nigeria influences geothermal exploration extent within each geological province. Sedimentary basins in Nigeria have been explored for hydrocarbons for several decades, thus the oil companies collected large subsurface temperature data basis. But not much is known about geothermal conditions within Nigerian Precambrian crystalline province. On the basis of BHT data from oil wells it has been found that geothermal gradient in Niger Delta ranges from 1.5 to 4.9°C/100m and in Anambra Basin (directly to the north) it can reach 5.7°C/100m. Exploration for geothermal energy in northern Nigeria based on shallow water wells (down to 600 m deep) was carried out over 20 years ago. The other aspect of geothermal exploration in Nigeria is investigating of the thermal springs and seepages, which occur mainly within sediments of the Middle and Upper Benue Trough. The water of the warmest springs in that area: Akiri and Ruwan Zafi have the temperature about 56°C and it suggests the occurrence of some geothermal anomalies.