DOCSLIB.ORG

Narg Newsletter 2019

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Narg Newsletter 2019 20 in 2020 View across the Argana Basin, Morocco Fieldwork New Projects New Starts More Early Cretaceous Regional Tectono- Ian Mounteney starts MPhil sections logged and stratigraphy of MSGBC – examining Cretaceous sampled in Morocco for utilising Petrosen and TGS clastic provenance in facies and provenance seismic data Senegal New Sponsors Pierre-Olivier Bruna joins as Triassic Synrift in Eastern PostDoc working on North Africa Research Group Research North Africa Hunt Oil, Mazarine Energy and Morocco – regional fractured reservoirs- Tunisia provenance study Shell join in 2019 Results coming in from TGS Seismic NARG ……….. Senegal Provenance Study MSGBC Basin Study As part of a suite of projects in Senegal and the 20 years of experience working • MSGBC , in collaboration with Petrosen and TGS, we A new PhD will commence in 2019 to across North Africa are undertaking a regional source to sink study, with examine the regional Tectono- MPhil student Ian Mounteney, working at the BGS. stratigraphy of the MSGBC Basin • Over 10 Academic s, 3 PostDocs undertaking regional mapping and and 6 PhDs, 2 MSc/MRes Sampling was completed in 2019, with 135 integrating well data provided by core/cuttings from 19 wells across Senegal (Silurian, students Petrosen with regional seismic data Devonian, Early/Late Cretaceous and Palaeogene). provided by TGS and Spectrum. This Modern river samples were also collected for • Global collaborations with leading build on existing reconnaissance specialists comparison. In total 32 kg of core/cuttings/sand biostratigtphic work and results from produced 4 kg of fine (63-125 micron) sand. Results examining 3D seismic donated by TGS in are expected shortly. See page 5. The Gambia . • Working with local institutions • Active projects underway in New Projects Morocco, Senegal, Mauritania, Tunisia, Egypt, Central Atlantic NARG is constantly starting new projects. In 2019 we move back to Tunisia, to begin reservoir characterisation studies with the appointment of Dr Pierre-Olivier Bruna at • Projects cover all aspects of the Tu Delft. We also have plans in place to undertake new Welcome to our New petroleum system: Depositional studies in Libya and Egypt in 2019/20. fairways, source to sink, clastic Sponsors and carbonate sedimentology, reservoir characterisation, thermo-geochronology Contents Highlights biostratigraphy, landscape evolution and modellling Triassic study …. Page 2 Heavy minerals / Provenance studies…. Page 4 and 5 Carbonates …. Page 7 The Africa Experts Latest publications …. Page 11 Staff and Researcher list …. Page 12 Assessing the provenance and contribution of local vs regional drainage systems for the Upper Triassic fluvial deposits, James Lovell-Kennedy, Jonathan Redfern, [email protected] Challenges 1. Introduction 1. Was there a regional axial rift fluvial system linking Oukaimeden, Kerrouchen, the High Plateaux and the Oujda Mountains during the Upper Triassic? 2. To what extent did local drainage influence sediment deposition during the Upper Triassic? 3. Can proximal, medial and distal fluvial successions be identified and correlated across the Triassic basins across Morocco? Aims of Study A. Analysis of heavy mineral assemblages from Triassic Basins to attempt to recognise signals from distinct source regions. B. Build on previous work on regional uplift to identify Triassic source areas and drainage systems. C. Compare the stratigraphy of the individual Triassic basins to assess the evolution of the depositional system and aid with correlation between basins. D. Perform a High Resolution Heavy Mineral Analysis (HRHMA) to identify the provenance of the Triassic deposits E. Combine heavy mineral analysis with field studies and subsurface data to reconstruct the Triassic paleodrainage and paleogeography Figure 1 : Map of the Triassic Basins, potential source areas and major faults in the study region. 2. Geological Setting and Fieldwork Geological setting Fieldwork Figure 5: Paleocurrent data from Kerrouchen Basin. Units K3 and K4 record a paleoflow flow toward the The inverted Mesozoic rift basins of the Atlas Mountains expose a thick Fieldwork and sampling of coarse clastic NNE, indicating a flow from the Triassic continental red-bed sequence. intervals has been undertaken in the Oukaimeden Basin and Central High Kerrouchen Basin and Oujda Mountains Atlas and towards the Oujda The Triassic basin fill of the Central and Middle Atlas is predominantly to augment previous work done in the Mountains (Figure 6). ephemeral and perennial fluvial deposits, with alluvial fans, occasional Oukaimeden and Argana Basins. The conglomerates of the K2 units aeolian deposits and interbedded lacustrine and, playa mudstones and record variable paleoflows, away from the basinal highs from which rare carbonates deposited in a series of rift basins following the break up of Whilst direct correlation between they are sourced. Pangea. The northern Oujda Mountains records a deltaic plain succession the basins is hampered by the lack with a Carnian transgression of Tethys prior to the establishment of of biostratigraphic data, similar widespread marine conditions in the Jurassic. depositional processes can be identified across the basins such Divergent paleocurrent measurements in the Massif Ancien indicate the as the K3 unit, Kerrouchen, and the F5 presence of a drainage divide, with flow to the west towards Argana and ‘Oukaimeden Sandstone’ within the flow to the east towards Oukaimeden (Figure 6). Oukaimeden Basin. Figure 4: Conglomeritic channels (A) at the base of Unit K3 outcropping in the Kerrouchen Basin, Middle Atlas. The conglomerates are conformably overlain by mud Figure 2: Photo ofT thehe Hercynian Triassic syn-rift continental clastics were deposited at the 140 SE clast conglomerates and stacked fluvial sandstones. The fluvial sands grade into point Unconformity from within the Kerrouchen bar deposits with mud drapes near the top of Unit K3. Basin, Middle Atlas. The basement formed a intra-basinal high.onset Debris flow depositsof rifting. They are proven reservoirs in the Essaouira Basin B (Unit K2) derived from the paleohigh onlap A C Triassic Source to Sink the unconformity.and Unit K3 andthe K4 are recent Sound Energy gas discovery in Tendrara, on the absent at this locality, as they were deposited in basinward lows to the east. The basement andHigh conglomerates Plateaux are Figure 3:, Compositehas logre of- theinvigorated Triassic interest in the play. 1m capped by the massive red mudstones of sequence in the Kerrouchen Basin. 2m 5m Unit K5. Eastern Morocco The reservoirs are tight fluvial sandstones and a key factor is to 3. Future Work betterFigure 6 understand Map of Triassic Source areas and measured and Methodology and Sampling potential paleoflows. 5 potential source areas for reservoirTriassic sediments have quality been identified; After successfully completing his MSc by Research in September 2018Initial heavy, James mineral analysis Lovell will be carried -out on Hercynian Granites, Precambrian Granites, samples from the F5 and K3 units from Metamorphic, Volcanic and Precambrian and Oukaimeden and Kerrouchen, along with deltaic and distribution. Paleozoic sediments. Kennedy, has now commenced a PhD into the provenance of the Triassicplain samples fromfluvial Oujda and samples from the Tendrara Field provided by Sound Energy. Table 1: Table shows the age range of each Tendrara reservoir (TAGI) in Eastern Morocco. During the first year of the PhD, alongside Thepotential sourcesystem for the Triassic has sediments from Discovery These samples are believed to be coeval based on the published literature. For the Precambrian and environment of deposition. Paleozoic sediments, the age range of their detri- potentialtal zircon population isoffshore given. The sedimentary de- training provided by the NERC CDT Oil and Gas, he undertook further field and core posits of the Anti-Atlas contain locally reworked Once the samples have undergone a heavy zircons from the Precambrian inliers. The combi- sampling season in November 2018. More samples have been collectedmineral separation, from a QEMSCAN the will be used to onnation bothof petrographic conjugate analysis of the heavy min- identify the abundance of Apatite, Tourmaline, erals should be able to identify reworked grains, Garnet, Zircon, Rutile, Chrome and Monzonite. The which would help differentiate between a Precam- Kerrouchen Basin, Middle Atlas, and from wells drilled in the High Plateau.ratio of these minerals In (specificallyaddition (ATi, GZi, RZi, Atlanticbrian granitic or sedimentary margin source fors the Trias- CZi and MZi) are provenance sensitive. sic sediment. we have been generously donated data from the Tendrara Block by Sound Energy. wherePotential Source thereRegion Radiometric is Date Range As the potential source areas in the region could Hercynian Granites 275Ma - 326Ma Precambrian and Paleozoic Sedi- 570Ma-2093Ma* Sound Energy and Regional Context of the High have significant overlap between heavy mineral ments *Detrital Zircon populations age populations, petrographic work will be done attempt limitedVolcanoclastic Deposits overburden. 617Ma Metamorphic Units 617Ma – 660Ma These samplesPlateaux are being‘the white space analysed for petrographic…..’ and heavy mineralto identify signatures between reworked and first and cycle grains. Precambrian Granites 617Ma – 2293Ma Acknowledgements: Special thanks to a representative sample selected for detrital zircon geochronology analysisI would
Load more

Recommended publications
  • Indices Par Commune
    Indices par commune Province Commune Centre Taux_pauvreté indice_volumétrique indice_séverité Vulnérabilité Azilal Azilal (M) 10,26 1,96 0,55 19,23 Azilal Demnate (M) 6,99 1,27 0,34 16,09 Azilal Agoudi N'Lkhair 26,36 5,84 1,88 30,84 Azilal Ait Abbas 50,01 16,62 7,33 23,59 Azilal Ait Bou Oulli 37,95 9,65 3,45 31,35 Azilal Ait M'Hamed 35,58 8,76 3,04 30,80 Azilal Tabant 19,21 3,24 0,81 33,95 Azilal Tamda Noumercid 15,41 2,90 0,82 27,83 Azilal Zaouiat Ahansal 35,27 9,33 3,45 28,53 Azilal Ait Taguella 17,08 3,28 0,95 28,09 Azilal Bni Hassane 16,10 2,87 0,77 29,55 Azilal Bzou 8,56 1,32 0,32 24,68 Azilal Bzou (AC) Bzou 5,80 1,02 0,27 16,54 Azilal Foum Jemaa 15,22 2,51 0,62 31,18 Azilal Foum Jemaa (AC) Foum Jemaa 13,26 2,56 0,72 22,54 Azilal Moulay Aissa Ben Driss 13,38 2,42 0,66 26,59 Azilal Rfala 21,69 4,46 1,35 30,64 Azilal Tabia 8,88 1,42 0,35 23,59 Azilal Tanant 11,63 2,12 0,59 23,41 Azilal Taounza 13,76 2,60 0,74 25,52 Azilal Tisqi 10,35 1,66 0,40 25,26 Azilal Ait Mazigh 24,23 4,91 1,47 33,72 Azilal Ait Ouqabli 18,31 3,25 0,88 33,12 Azilal Anergui 35,18 9,25 3,41 28,49 Azilal Bin El Ouidane 7,96 1,14 0,25 25,44 Azilal Isseksi 16,21 2,97 0,81 29,19 Azilal Ouaouizeght 9,00 1,19 0,25 29,46 Azilal Ouaouizeght (AC) Ouaouizeght 9,61 1,85 0,52 18,05 Azilal Tabaroucht 51,04 15,52 6,36 27,11 Province Commune Centre Taux_pauvreté indice_volumétrique indice_séverité Vulnérabilité Azilal Tagleft 27,66 6,89 2,44 26,89 Azilal Tiffert N'Ait Hamza 16,84 3,99 1,37 21,90 Azilal Tilougguite 24,10 5,32 1,70 30,13 Azilal Afourar 5,73 0,80 0,17 20,51 Azilal
    [Show full text]
  • La Liste Des Jardins D'enfants Relevant Du Ministère De La Jeunesse Et Des Sports
    la liste des Jardins d'Enfants relevant du Ministère de la Jeunesse et des Sports Délégation Etablissement Milieu Adresse Région : Rabat -Salé -Kenitra Rabat Alazhar Urbain Lotissement Alhaj Slimane n°15 C.Y.M Annahda Urbain Derb elfassi Rue joutiya n° 06 Souika Yaacoub eddar Urbain Rue 48 n° 1 Hay El Barid C.Y.M Provincial Urbain Avenue Sidi Mohamed Ben Abdellah C.Y.M Touarga Almichouar Said Touarga Urbain Almichouar Said Touarga Sale Tabrekte Urbain Hay Almazraä tabrekte Bettana Urbain Avenue Palestine Sale Achahbaa Urbain Avenue 2 Mars Rue Said Hajji Salé Alaayayda 1 Urbain Lgazzara Laayayda 1 Salé Alaayayda 2 Urbain Terrain Benaacher Alaayayda 2 Salé Skhirate Témara Almanzah Rural Commune Almanzah Sidi Yahya Rural Sidi Yahya zaër Ain Aaouda Urbain Eglise Ain Aaouda Annasr Urbain Hay Annasr Témara Hay Alfath Rural Hay Alfath skhirate Khémisset Provincial Urbain Avenue Idriss Elharti hay Essalam khémisset J.G Alaman Urbain Al hay alidari Khémisset Almahalli Urbain Rue Maarakate Badr Alkobra Khémisset Alamal Urbain Avenue la marche verte Tifelte Central « Almarkazi » Urbain N°66 rue almaazize hay alfarkh tifelte Albahraoui Rural - Arromani Rural Hay alamal Arromani Alghandour Rural Alghandour centre Alkanzara Rural Alkanzara centre Almaaziz Rural Almaaziz Alhay Alidari Ait Ikou Rural Ait Ikou centre Had Elbrachwa Rural Had Elbrachwa centre Ait Yadine Rural Ait Yadine centre Tiddasse Rural Tiddasse centre Khmisse Sidi Yahya Rural Commune Khmisse Sidi Yahya Oulmes Rural Oulmes centre Kénitra Alminaa Urbain Villa n°276 biir errami algharbiya
    [Show full text]
  • Cadastre Des Autorisations TPV Page 1 De
    Cadastre des autorisations TPV N° N° DATE DE ORIGINE BENEFICIAIRE AUTORISATIO CATEGORIE SERIE ITINERAIRE POINT DEPART POINT DESTINATION DOSSIER SEANCE CT D'AGREMENT N Casablanca - Beni Mellal et retour par Ben Ahmed - Kouribga - Oued Les Héritiers de feu FATHI Mohamed et FATHI Casablanca Beni Mellal 1 V 161 27/04/2006 Transaction 2 A Zem - Boujad Kasbah Tadla Rabia Boujad Casablanca Lundi : Boujaad - Casablanca 1- Oujda - Ahfir - Berkane - Saf Saf - Mellilia Mellilia 2- Oujda - Les Mines de Sidi Sidi Boubker 13 V Les Héritiers de feu MOUMEN Hadj Hmida 902 18/09/2003 Succession 2 A Oujda Boubker Saidia 3- Oujda La plage de Saidia Nador 4- Oujda - Nador 19 V MM. EL IDRISSI Omar et Driss 868 06/07/2005 Transaction 2 et 3 B Casablanca - Souks Casablanca 23 V M. EL HADAD Brahim Ben Mohamed 517 03/07/1974 Succession 2 et 3 A Safi - Souks Safi Mme. Khaddouj Bent Salah 2/24, SALEK Mina 26 V 8/24, et SALEK Jamal Eddine 2/24, EL 55 08/06/1983 Transaction 2 A Casablanca - Settat Casablanca Settat MOUTTAKI Bouchaib et Mustapha 12/24 29 V MM. Les Héritiers de feu EL KAICH Abdelkrim 173 16/02/1988 Succession 3 A Casablanca - Souks Casablanca Fès - Meknès Meknès - Mernissa Meknès - Ghafsai Aouicha Bent Mohamed - LAMBRABET née Fès 30 V 219 27/07/1995 Attribution 2 A Meknès - Sefrou Meknès LABBACI Fatiha et LABBACI Yamina Meknès Meknès - Taza Meknès - Tétouan Meknès - Oujda 31 V M. EL HILALI Abdelahak Ben Mohamed 136 19/09/1972 Attribution A Casablanca - Souks Casablanca 31 V M.
    [Show full text]
  • A Note from Sir Richard Branson
    A NOTE FROM SIR RICHARD BRANSON “ In 1998, I went to Morocco with the goal of circumnavigating the globe in a hot air balloon. Whilst there, my parents found a beautiful Kasbah and dreamed of turning it into a wonderful Moroccan retreat. Sadly, I didn’t quite manage to realise my goal on that occasion, however I did purchase that magnificent Kasbah and now my parents’ dream has become a reality. I am pleased to welcome you to Kasbah Tamadot, (Tamadot meaning soft breeze in Berber), which is perhaps one of the most beautiful properties in the high Atlas Mountains of Morocco. I hope you enjoy this magical place; I’m sure you too will fall in love with it.” Sir Richard Branson 2- 5 THINGS YOU NEED TO KNOW 14 Babouches ACTIVITIES AT KASBAH Babysitting TAMADOT Cash and credit cards Stargazing Cigars Trekking in the Atlas Mountains Departure Asni Market Tours WELCOME TO KASBAH TAMADOT Do not disturb Cooking classes Fire evacuation routes Welcome to Kasbah Tamadot (pronounced: tam-a-dot)! Four legged friends We’re delighted you’ve come to stay with us. Games, DVDs and CDs This magical place is perfect for rest and relaxation; you can Kasbah Tamadot Gift Shop 1 5 do as much or as little as you like. Enjoy the fresh mountain air The Berber Boutique KASBAH KIDS as you wander around our beautiful gardens of specimen fruit Laundry and dry cleaning Activities for children trees and rambling rose bushes, or go on a trek through the Lost or found something? Medical assistance and pharmacy High Atlas Mountains...the choice is yours.
    [Show full text]
  • Rowan C. Martindale Curriculum Vitae Associate Professor (Invertebrate Paleontology) at the University of Texas at Austin
    ROWAN C. MARTINDALE CURRICULUM VITAE ASSOCIATE PROFESSOR (INVERTEBRATE PALEONTOLOGY) AT THE UNIVERSITY OF TEXAS AT AUSTIN Department of Geological Sciences E-mail: [email protected] Jackson School of Geosciences Website: www.jsg.utexas.edu/martindale/ 2275 Speedway Stop C9000 Orchid ID: 0000-0003-2681-083X Austin, TX 78712-1722 Phone: 512-475-6439 Office: JSG 3.216A RESEARCH INTERESTS The overarching theme of my work is the connection between Earth and life through time, more precisely, understanding ancient (Mesozoic and Cenozoic) ocean ecosystems and the evolutionary and environmental events that shaped them. My research is interdisciplinary, (paleontology, sedimentology, biology, geochemistry, and oceanography) and focuses on: extinctions and carbon cycle perturbation events (e.g., Oceanic Anoxic Events, acidification events); marine (paleo)ecology and reef systems; the evolution of reef builders (e.g., coral photosymbiosis); and exceptionally preserved fossil deposits (Lagerstätten). ACADEMIC APPOINTMENTS Associate Professor, University of Texas at Austin September 2020 to Present Assistant Professor, University of Texas at Austin August 2014 to August 2020 Postdoctoral Researcher, Harvard University August 2012 to July 2014 Department of Organismic and Evolutionary Biology; Mentor: Dr. Andrew H. Knoll. EDUCATION Doctorate, University of Southern California 2007 to 2012 Dissertation: “Paleoecology of Upper Triassic reef ecosystems and their demise at the Triassic-Jurassic extinction, a potential ocean acidification event”. Advisor: Dr. David J. Bottjer, degree conferred August 7th, 2012. Bachelor of Science Honors Degree, Queen’s University 2003 to 2007 Geology major with a general concentration in Biology (Geological Sciences Medal Winner). AWARDS AND RECOGNITION Awards During Tenure at UT Austin • 2019 National Science Foundation CAREER Award: Awarded to candidates who are judged to have the potential to serve as academic role models in research and education.
    [Show full text]
  • Chapitre VI La Ville Et Ses Équipements Collectifs
    Chapitre VI La ville et ses équipements collectifs Introduction L'intérêt accordé à la connaissance du milieu urbain et de ses équipements collectifs suscite un intérêt croissant, en raison de l’urbanisation accélérée que connaît le pays, et de son effet sur les équipements et les dysfonctionnements liés à la répartition des infrastructures. Pour résorber ce déséquilibre et assurer la satisfaction des besoins, le développement d'un réseau d'équipements collectifs appropriés s'impose. Tant que ce déséquilibre persiste, le problème de la marginalisation sociale, qui s’intensifie avec le chômage et la pauvreté va continuer à se poser La politique des équipements collectifs doit donc occuper une place centrale dans la stratégie de développement, particulièrement dans le cadre de l’aménagement du territoire. La distribution spatiale de la population et par conséquent des activités économiques, est certes liée aux conditions naturelles, difficiles à modifier. Néanmoins, l'aménagement de l'espace par le biais d'une politique active peut constituer un outil efficace pour mettre en place des conditions favorables à la réduction des disparités. Cette politique requiert des informations fiables à un niveau fin sur l'espace à aménager. La présente étude se réfère à la Base de données communales en milieu urbain (BA.DO.C) de 1997, élaborée par la Direction de la Statistique et concerne le niveau géographique le plus fin à savoir les communes urbaines, qui constituent l'élément de base de la décentralisation et le cadre d'application de la démocratie locale. Au recensement de 1982, était considéré comme espace urbain toute agglomération ayant un minimum de 1 500 habitants et qui présentait au moins quatre des sept conditions énumérées en infra1.
    [Show full text]
  • Crustal Versus Asthenospheric Origin of the Relief of the Atlas Mountains of Morocco
    Crustal versus asthenospheric origin of the relief of the Atlas Mountains of Morocco. Y. Missenard, H. Zeyen, D. Frizon de Lamotte, P. Leturmy, C. Petit, M. Sebrier To cite this version: Y. Missenard, H. Zeyen, D. Frizon de Lamotte, P. Leturmy, C. Petit, et al.. Crustal versus astheno- spheric origin of the relief of the Atlas Mountains of Morocco.. Journal of Geophysical Research, American Geophysical Union, 2006, 111, pp.B03401. 10.1029/2005JB003708. hal-00092374 HAL Id: hal-00092374 https://hal.archives-ouvertes.fr/hal-00092374 Submitted on 1 Mar 2021 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. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, B03401, doi:10.1029/2005JB003708, 2006 Crustal versus asthenospheric origin of relief of the Atlas Mountains of Morocco Yves Missenard,1 Hermann Zeyen,2 Dominique Frizon de Lamotte,1 Pascale Leturmy,1 Carole Petit,3 Michel Se´brier,3 and Omar Saddiqi4 Received 2 March 2005; revised 18 October 2005; accepted 9 November 2005; published 1 March 2006. [1] We investigate the respective roles of crustal tectonic shortening and asthenospheric processes on the topography of the High Atlas and surrounding areas (Morocco).
    [Show full text]
  • Pauvrete, Developpement Humain
    ROYAUME DU MAROC HAUT COMMISSARIAT AU PLAN PAUVRETE, DEVELOPPEMENT HUMAIN ET DEVELOPPEMENT SOCIAL AU MAROC Données cartographiques et statistiques Septembre 2004 Remerciements La présente cartographie de la pauvreté, du développement humain et du développement social est le résultat d’un travail d’équipe. Elle a été élaborée par un groupe de spécialistes du Haut Commissariat au Plan (Observatoire des conditions de vie de la population), formé de Mme Ikira D . (Statisticienne) et MM. Douidich M. (Statisticien-économiste), Ezzrari J. (Economiste), Nekrache H. (Statisticien- démographe) et Soudi K. (Statisticien-démographe). Qu’ils en soient vivement remerciés. Mes remerciements vont aussi à MM. Benkasmi M. et Teto A. d’avoir participé aux travaux préparatoires de cette étude, et à Mr Peter Lanjouw, fondateur de la cartographie de la pauvreté, d’avoir été en contact permanent avec l’ensemble de ces spécialistes. SOMMAIRE Ahmed LAHLIMI ALAMI Haut Commissaire au Plan 2 SOMMAIRE Page Partie I : PRESENTATION GENERALE I. Approche de la pauvreté, de la vulnérabilité et de l’inégalité 1.1. Concepts et mesures 1.2. Indicateurs de la pauvreté et de la vulnérabilité au Maroc II. Objectifs et consistance des indices communaux de développement humain et de développement social 2.1. Objectifs 2.2. Consistance et mesure de l’indice communal de développement humain 2.3. Consistance et mesure de l’indice communal de développement social III. Cartographie de la pauvreté, du développement humain et du développement social IV. Niveaux et évolution de la pauvreté, du développement humain et du développement social 4.1. Niveaux et évolution de la pauvreté 4.2.
    [Show full text]
  • Nostalgias in Modern Tunisia Dissertation
    Images of the Past: Nostalgias in Modern Tunisia Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By David M. Bond, M.A. Graduate Program in Near Eastern Languages and Cultures The Ohio State University 2017 Dissertation Committee: Sabra J. Webber, Advisor Johanna Sellman Philip Armstrong Copyrighted by David Bond 2017 Abstract The construction of stories about identity, origins, history and community is central in the process of national identity formation: to mould a national identity – a sense of unity with others belonging to the same nation – it is necessary to have an understanding of oneself as located in a temporally extended narrative which can be remembered and recalled. Amid the “memory boom” of recent decades, “memory” is used to cover a variety of social practices, sometimes at the expense of the nuance and texture of history and politics. The result can be an elision of the ways in which memories are constructed through acts of manipulation and the play of power. This dissertation examines practices and practitioners of nostalgia in a particular context, that of Tunisia and the Mediterranean region during the twentieth and early twenty-first centuries. Using a variety of historical and ethnographical sources I show how multifaceted nostalgia was a feature of the colonial situation in Tunisia notably in the period after the First World War. In the postcolonial period I explore continuities with the colonial period and the uses of nostalgia as a means of contestation when other possibilities are limited.
    [Show full text]
  • Climbing in the Atlas Mountains a Survey
    HAMISH BROWN Climbing in the Atlas Mountains A Survey (Plates 24-27) magine a country with eighty per cent sunshine throughout the year, I grand mountain scenery, its rock climbing potential barely touched, all within easy reach, with no political hassles orcostly fees, and a lovely people. It may sound too good to be true but it all exists in Europe's nearest truly exotic foreign country: Morocco. The Atlas Mountains, which sweep across from north-east to south-west, separating 'the desert and the sown', offer a climber's paradise. Quite why the Atlas has suffered neglect by climbers from Britain is hard to understand. Perhaps the names are too difficult - there's no kudos in reporting unpronounceable climbs - or the information is hidden away in French publications. 1 Time the cat escaped from out of the bag. I spent a winter in the Atlas in 1965 and repeated this delight in 1966. Having gone there specifically to climb (Notes in AJ 1966) I ended simply hooked on the whole Atlas ambience and began to wander rather than be restricted to one area. The natural outcome of this was an end-to-end trek 2 in 1995 : 96 days, 900 miles and about 30 peaks bagged. Farfrom rounding off my knowledge, the trip introduced me to a score of new worthy areas to visit and I've had five Atlas months every year since. 3 The scope for climbing is vast. The country must have 50 limestone gorges, miles long and up to 2000 feet deep, each ofwhich would fill volumes ofclimbs if located in Europe, while on the mountains there are crests to be traversed and notable granite faces still virgin.
    [Show full text]
  • Télécharger Le Document
    CARTOGRAPHIE DU DÉVELOPPEMENT LOCAL MULTIDIMENSIONNEL NIVEAU ET DÉFICITS www.ondh.ma SOMMAIRE Résumé 6 Présentation 7 1. Approche méthodologique 8 1.1. Portée et lecture de l’IDLM 8 1.2. Fiabilité de l’IDLM 9 2. Développement, niveaux et sources de déficit 10 2.1. Cartographie du développement régional 11 2.2. Cartographie du développement provincial 13 2.3. Développement communal, état de lieux et disparité 16 3. L’IDLM, un outil de ciblage des programmes sociaux 19 3.1 Causes du déficit en développement, l’éducation et le niveau de vie en tête 20 3.2. Profil des communes à développement local faible 24 Conclusion 26 Annexes 27 Annexe 1 : Fiabilité de l’indice de développement local multidimensionnel (IDLM) 29 Annexe 2 : Consistance et méthode de calcul de l’indice de développement local 30 multidimensionnel Annexe 3 : Cartographie des niveaux de développement local 35 Annexes Communal 38 Cartographie du développement communal-2014 41 5 RÉSUMÉ La résorption ciblée des déficits socio-économiques à l’échelle locale (province et commune) requiert, à l’instar de l’intégration et la cohésion des territoires, le recours à une cartographie du développement au sens multidimensionnel du terme, conjuguée à celle des causes structurelles de son éventuel retard. Cette étude livre à cet effet une cartographie communale du développement et de ses sources assimilées à l’éducation, la santé, le niveau de vie, l’activité économique, l’habitat et les services sociaux, à partir de la base de données «Indicateurs du RGPH 2014» (HCP, 2017). Cette cartographie du développement et de ses dimensions montre clairement que : - La pauvreté matérielle voire monétaire est certes associée au développement humain, mais elle ne permet pas, à elle seule, d’identifier les communes sous l’emprise d’autres facettes de pauvreté.
    [Show full text]
  • MPLS VPN Service
    MPLS VPN Service PCCW Global’s MPLS VPN Service provides reliable and secure access to your network from anywhere in the world. This technology-independent solution enables you to handle a multitude of tasks ranging from mission-critical Enterprise Resource Planning (ERP), Customer Relationship Management (CRM), quality videoconferencing and Voice-over-IP (VoIP) to convenient email and web-based applications while addressing traditional network problems relating to speed, scalability, Quality of Service (QoS) management and traffic engineering. MPLS VPN enables routers to tag and forward incoming packets based on their class of service specification and allows you to run voice communications, video, and IT applications separately via a single connection and create faster and smoother pathways by simplifying traffic flow. Independent of other VPNs, your network enjoys a level of security equivalent to that provided by frame relay and ATM. Network diagram Database Customer Portal 24/7 online customer portal CE Router Voice Voice Regional LAN Headquarters Headquarters Data LAN Data LAN Country A LAN Country B PE CE Customer Router Service Portal PE Router Router • Router report IPSec • Traffic report Backup • QoS report PCCW Global • Application report MPLS Core Network Internet IPSec MPLS Gateway Partner Network PE Router CE Remote Router Site Access PE Router Voice CE Voice LAN Router Branch Office CE Data Branch Router Office LAN Country D Data LAN Country C Key benefits to your business n A fully-scalable solution requiring minimal investment
    [Show full text]