Structural Context of the Paleogeography of the Cenomanian-Turonian Anoxic Event in the Eastern Atlas Basins of the Maghreb Mohamed Soua
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Policy Notes for the Trump Notes Administration the Washington Institute for Near East Policy ■ 2018 ■ Pn55
TRANSITION 2017 POLICYPOLICY NOTES FOR THE TRUMP NOTES ADMINISTRATION THE WASHINGTON INSTITUTE FOR NEAR EAST POLICY ■ 2018 ■ PN55 TUNISIAN FOREIGN FIGHTERS IN IRAQ AND SYRIA AARON Y. ZELIN Tunisia should really open its embassy in Raqqa, not Damascus. That’s where its people are. —ABU KHALED, AN ISLAMIC STATE SPY1 THE PAST FEW YEARS have seen rising interest in foreign fighting as a general phenomenon and in fighters joining jihadist groups in particular. Tunisians figure disproportionately among the foreign jihadist cohort, yet their ubiquity is somewhat confounding. Why Tunisians? This study aims to bring clarity to this question by examining Tunisia’s foreign fighter networks mobilized to Syria and Iraq since 2011, when insurgencies shook those two countries amid the broader Arab Spring uprisings. ©2018 THE WASHINGTON INSTITUTE FOR NEAR EAST POLICY. ALL RIGHTS RESERVED. THE WASHINGTON INSTITUTE FOR NEAR EAST POLICY ■ NO. 30 ■ JANUARY 2017 AARON Y. ZELIN Along with seeking to determine what motivated Evolution of Tunisian Participation these individuals, it endeavors to reconcile estimated in the Iraq Jihad numbers of Tunisians who actually traveled, who were killed in theater, and who returned home. The find- Although the involvement of Tunisians in foreign jihad ings are based on a wide range of sources in multiple campaigns predates the 2003 Iraq war, that conflict languages as well as data sets created by the author inspired a new generation of recruits whose effects since 2011. Another way of framing the discussion will lasted into the aftermath of the Tunisian revolution. center on Tunisians who participated in the jihad fol- These individuals fought in groups such as Abu Musab lowing the 2003 U.S. -
30. Turonian–Santonian Benthic
Mascle, J., Lohmann, G.P., and Moullade, M. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 159 30. TURONIAN–SANTONIAN BENTHIC FORAMINIFER ASSEMBLAGES FROM SITE 959D (CÔTE D’IVOIRE-GHANA TRANSFORM MARGIN, EQUATORIAL ATLANTIC): INDICATION OF A LATE CRETACEOUS OXYGEN MINIMUM ZONE1 Ann E.L. Holbourn2,3 and Wolfgang Kuhnt2 ABSTRACT Turonian–Santonian organic-rich fissile black claystones with laminated intervals from Hole 959D on the Côte d’Ivoire- Ghana Transform Margin, drilled during Ocean Drilling Program Leg 159, contain benthic foraminifer assemblages dominated by buliminid associations. The lower Turonian assemblage from Core 159-959D-68R is strongly dominated by Bolivina anam- bra, Praebulimina sp. 1, Praebulimina sp. 2, Praebulimina sp. 3, and Gavelinella spp. The upper Turonian to lower Coniacian assemblage from Core 159-959D-67R displays low abundance and low diversity and consists mostly of organically cemented agglutinated taxa and/or some corroded tests of Lenticulina, Bolivina, Gyroidinoides ex gr. nitidus. The middle Coniacian to lower Santonian assemblage from Core 159-959D-66R and from the base of Core 159-959D-65R contains high numbers of Praebulimina robusta, Praebulimina fang, Neobulimina subregularis, and Buliminella cf. gabonica, but shows marked fluctua- tions in abundance and diversity, which appear to be related to changes in total organic carbon. The distinct composition of the two buliminid associations in Core 159-959D-68R and Core 159-959D-66R suggests that endemism was stronger during the early Turonian, when circulation was probably more restricted and connections between equatorial Atlantic basins were lim- ited. We interpret the late Coniacian–early Santonian depositional environment to be an oxygen minimum zone in a more open marine outer shelf or upper slope setting. -
Quelques Aspects Problematiques Dans La Transcription Des Toponymes Tunisiens
QUELQUES ASPECTS PROBLEMATIQUES DANS LA TRANSCRIPTION DES TOPONYMES TUNISIENS Mohsen DHIEB Professeur de géographie (cartographie) Laboratoire SYFACTE FLSH de Sfax TUNISIE [email protected] Introduction Quelle que soit le pays ou la langue d’usage, la transcription toponymique des noms de lieux géographiques sur un atlas ou un autre document cartographique en particulier ou tout autre document d’une façon générale pose problème notamment dans des pays où il n’y a pas de tradition ou de « politique » toponymique. Il en est de même pour les contrées « ouvertes » à l’extérieur et par conséquent ayant subi ou subissant encore les influences linguistiques étrangères ou alors dans des régions caractérisées par la complexité de leur situation linguistique. C’est particulièrement le cas de la Tunisie, pays méditerranéen bien « ancré » dans l’histoire, mais aussi bien ouvert à l’étranger et subissant les soubresauts de la mondialisation, et manquant par ailleurs cruellement de politique toponymique. Tout ceci malgré l’intérêt que certains acteurs aux profils différents y prêtent depuis peu, intérêt matérialisé, entre autres manifestations scientifiques, par l’organisation de deux rencontres scientifiques par la Commission du GENUING en 2005 et d’une autre août 2008 à Tunis, lors du 35ème Congrès de l’UGI. Aussi, il s’agit dans le cadre de cette présentation générale de la situation de la transcription toponymique en Tunisie, dans un premier temps, de dresser l’état des lieux, de mettre en valeur les principales difficultés rencontrées en manipulant les noms géographiques dans leurs différentes transcriptions dans un second temps. En troisième lieu, il s’agit de proposer à l’officialisation, une liste-type de toponymes (exonymes et endonymes) que l’on est en droit d’avoir par exemple sur une carte générale de Tunisie à moyenne échelle. -
Role of the NE-SW Hercynian Master Fault Systems and Associated
Chapter 6 Role of the NE-SW Hercynian Master Fault Systems and Associated Lineaments on the Structuring and Evolution of the Mesozoic and Cenozoic Basins of the Alpine Margin, Northern Tunisia Fetheddine Melki, Taher Zouaghi, Mohamed Ben Chelbi, Mourad Bédir and Fouad Zargouni Additional information is available at the end of the chapter http://dx.doi.org/10.5772/50145 1. Introduction The Mesozoic and Cenozoic evolution of the northern edge of the African margin (Fig. 1), and particularly the northern Tunisia, fossilized successive paleogeographic and tectonic episodes. In fact, after rifting and extensional periods, which started at the end of the Paleozoic and continued during the Mesozoic [1‐6], was settled the Alpine orogeny that results from the convergence movements between the African and Eurasian plates; it is induced by compres‐ sive tectonic stresses, beginning at least since the Tertiary intervals and probably the Late Cretaceous [7‐24]. This orogeny has induced, on the Mediterranean edges, many mountains chains extend from the Apennines at the East to the Betic Cordilleras at the West. The various geological works established in northern Tunisia [25‐42,18,43‐47], north‐eastern Algeria [48‐50,23] and in the Siculo‐Tunisian strait [51‐57], demonstrated that the NE‐SW inherit‐ ed fault networks have controlled sedimentation during the Tethyan rifting and have also con‐ trolled the structuring of the central and northern Atlas during the successive tectonic events. This margin of northern Tunisia, including the Tell and the Tunisian furrow domains (Fig. 2), is limited to the East by the Zaghouan master fault, which appears to have effect on the sedimentation since the Jurassic [58,59,33]. -
Entreprise Code Sec Ville Siege Adresse Tel Fax
ENTREPRISE CODE_SEC VILLE_SIEGE ADRESSE TEL FAX 1 BELDI IAA ARIANA Route de Mateur Km 8 71 521 000 71 520 577 2 BISCUITERIE AZAIZ IAA ARIANA 71 545 141 71 501 412 3 COOPERATIVE VITICOLE DE TUNIS IAA ARIANA Sabalet ben Ammar 71 537 120 71 535 318 4 GENERAL FOOD COMPANY IAA ARIANA Rue Metouia BORJ LOUZIR 71 691 036 70 697 104 5 GRANDE FABRIQUE DE CONFISERIE ORIENTALE - GFCO IAA ARIANA 11, Rue des Entrepreneurs Z.I Ariana Aroport 2035 Tunis-Carthage 70837411 70837833 6 HUILERIE BEN AMMAR IAA ARIANA Cebelet Ben Ammar Route de Bizerte Km 15 71 537 324 71 785 916 7 SIROCCO IAA ARIANA Djebel Ammar 71 552 365 71 552 098 8 SOCIETE AMANI IAA ARIANA Route Raoued Km 5 71 705 434 71 707 430 9 SOCIETE BGH IAA ARIANA Z.I Elalia Ben Gaied Hassine 71 321 718/70823945 70823944 10 SOCIETE CARTHAGE AGRO-ALIMENTAIRE IAA ARIANA Bourj Touil 70684001 70684002 11 SOCIETE DE SERVICES AGRICOLES ZAHRA IAA ARIANA Bouhnech - KALAAT EL ANDALUS 25 100 200 12 SOCIETE FROMAGERIE SCANDI IAA ARIANA 23 346 143/706800 70 680 009 13 SOCIETE FRUIT CENTER IAA ARIANA 35 Rue Mokhtar ATTIA 71 334 710 71 857 260 14 SOCIETE GIGA IAA ARIANA 70 308 441 71 308 476 15 SOCIETE GREEN LAND ET CIE IAA ARIANA route el battane jedaida 1124 mannoba 71798987 71784116 16 SOCIETE JASMIN EXPORT IAA ARIANA Rue Mohamed El Habib Route de Raoued Km 7 71 866 817 71 866 826 17 SOCIETE KACEM DE PATISSERIE - KAPCO IAA ARIANA 20 Rue Kalaat Ayoub Riadh El Andalous 71 821 388 71 821 466 18 SOCIETE LABIDI VIANDES IAA ARIANA Borj Touil 71 768 731 71 769 080 19 SOCIETE LE TORREFACTEUR IAA ARIANA Rue de l'argent -
Cenomanian Turonian Coniacian Santonian Campanian
walteri aff. aff. spp. spp. imperfectus spp. (prisms) Chronostratigraphy Offshore Norway sp. 1 Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Allomorphina halli / pyriformis Sigmoilina antiqua Textularia Gavelinella intermeda gracillima Valvulineria Bulbobaculites problematicus Caudammina ovuloides Nuttallinella florealis Stensioeina granulata polonica Inoceramus Rzehakina minima Rzehakina epigona Fenestrella bellii Gaudryina filiformis Trochamminoides Haplophragmoides Gavelinella usakensis Caudammina ovula Coarse agglutinated spp. LCO dubia Tritaxia Plectorecurvoides alternans Reussella szajnochae Recurvoides Hippocrepina depressa Psammosphaera sphaerical radiolarians Ma Age/Stage Lingulogavelinella jarzevae elegans Lt NCF19 Maastrichtian volutus LCO 70 NCF18 E szajnochae dubia Lt 75 LCO of NCF17 Campanian Deep Water M Agglutinated 80 Foraminifera E bellii NCF16 Lt Inoceramus LCO NCF15 85 Santonian M E polonica NCF14 Lt Coniacian M E Marginotruncana NCF13 90 Lt Turonian M E Dicarinella NCF12 95 Lt brittonensis M NCF11 Cenomanian delrioensis LCO NCF10 E antiqua NCF9 100 Figure 2.8c. Stratigraphic ranges of Upper Cretaceous benthic foraminifera, and miscellaneous index taxa, oshore mid-Norway, with the foraminiferal zonation established in this study. s.l. Chronostratigraphy Offshore Norway Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Abathomphalus mayaroensis Pseudotextularia elegans Hedbergella planispira Hedbergella hoelzi Praeglobotruncana delrioensis Praeglobotruncana stephani -
Upper Cenomanian •fi Lower Turonian (Cretaceous) Calcareous
Studia Universitatis Babeş-Bolyai, Geologia, 2010, 55 (1), 29 – 36 Upper Cenomanian – Lower Turonian (Cretaceous) calcareous algae from the Eastern Desert of Egypt: taxonomy and significance Ioan I. BUCUR1, Emad NAGM2 & Markus WILMSEN3 1Department of Geology, “Babeş-Bolyai” University, Kogălniceanu 1, 400084 Cluj Napoca, Romania 2Geology Department, Faculty of Science, Al-Azhar University, Egypt 3Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Sektion Paläozoologie, Königsbrücker Landstr. 159, D-01109 Dresden, Germany Received March 2010; accepted April 2010 Available online 27 April 2010 DOI: 10.5038/1937-8602.55.1.4 Abstract. An assemblage of calcareous algae (dasycladaleans and halimedaceans) is described from the Upper Cenomanian to Lower Turonian of the Galala and Maghra el Hadida formations (Wadi Araba, northern Eastern Desert, Egypt). The following taxa have been identified: Dissocladella sp., Neomeris mokragorensis RADOIČIĆ & SCHLAGINTWEIT, 2007, Salpingoporella milovanovici RADOIČIĆ, 1978, Trinocladus divnae RADOIČIĆ, 2006, Trinocladus cf. radoicicae ELLIOTT, 1968, and Halimeda cf. elliotti CONARD & RIOULT, 1977. Most of the species are recorded for the first time from Egypt. Three of the identified algae (T. divnae, S. milovanovici and H. elliotti) also occur in Cenomanian limestones of the Mirdita zone, Serbia, suggesting a trans-Tethyan distribution of these taxa during the early Late Cretaceous. The abundance and preservation of the algae suggest an autochthonous occurrence which can be used to characterize the depositional environment. The recorded calcareous algae as well as the sedimentologic and palaeontologic context of the Galala Formation support an open-lagoonal (non-restricted), warm-water setting. The Maghra el Hadida Formation was mainly deposited in a somewhat deeper, open shelf setting. -
The National Sanitation Utility
OFFICE NATIONAL DE L’ASSAINISSEMENT (THE NATIONAL SANITATION UTILITY) 32,rue Hédi Nouira 1001 TUNIS Tel.:710 343 200 – Fax :71 350 411 E-mail :[email protected] Web site :www.onas.nat.tn ANNUAL REPORT 2004 O.N.A.S.IN BRIEF MEMBERS OF THE EXECUTIVE BOARD Khalil ATTIA President of the E. B. 1.Establishment Maher KAMMOUN Prime Ministry Noureddine BEN REJEB Ministry of Agriculture The National Sanitation Utility (O.N.A.S.) is a public company of an and Hydraulic Resources industrial and commercial character,serving under the authority of the Mohamed BELKHIRIA Ministry of the Interior and Local Ministry of the Environment and Sustainable Development, and Development enjoying the status of a civil entity and financial independence. It was Moncef MILED Ministry of Development and established by Law N° 73/74, dated August 1974, and entrusted with International Cooperation the management of the sanitation sector. Rakia LAATIRI Ministry of Agriculture and The Law establishing O.N.A.S. was amended pursuant to Law N° Hydraulic Resources 41/93, dated 19 April 1993, which promoted the Utility from the sta- Mohamed Tarek EL BAHRI Ministry of Equipment, Housing tus of a networks and sewers management authority to the status of and Land Use Planning a key operator in the field of protection of the water environment. Abderrahmane GUENNOUN National Environment Protection Agency (ANPE) 2.O.N.A.S.Mission: Abdelaziz MABROUK National Water Distribution Utility (SONEDE) •Combating all forms of water pollution and containing its sources; Slah EL BALTI Municipality of Ariana •Operation, management and maintenance of all sanitation facilities in O.N.A.S. -
The Turonian - Coniacian Boundary in the United States Western Interior
Acta Geologica Polonica, Vol. 48 (1998), No.4, pp. 495-507 The Turonian - Coniacian boundary in the United States Western Interior IRENEUSZ WALASZCZYKI & WILLIAM A. COBBAN2 I Institute of Geology, University of Warsaw, AI. Zwirki i Wigury 93, PL-02-089 Warszawa, Poland E-mail: [email protected] 270 Estes Street, Lakewood, Colorado 80226, USA ABSTRACT: WALASZCZYK, I. & COBBAN, W.A. 1998. The Turonian - Coniacian boundary in the United States Western Interior. Acta Geologica Polonica, 48 (4),495-507. Warszawa. The Turonian/Coniacian boundary succession in the United States Western Interior is characterized by the same inoceramid faunas as recognized in Europe, allowing the application of the same zonal scheme in both regions; Mytiloides scupini and Cremnoceramus waltersdorfensis waltersdorfensis zones in the topmost Turonian and Cremnoceramus deformis erectus Zone in the lowermost Coniacian. The correla tion with Europe is enhanced, moreover, by a set of boundary events recognized originally in Europe and well represented in the Western Interior: Didymotis I Event and waltersdorfensis Event in the topmost Turonian, and erectus I, II and ?III events in the Lower Coniacian. First "Coniacian" ammonite, Forresteria peruana, appears in the indisputable Turonian, in the zone of M. scupini, and the reference to Forresteria in the boundary definition should be rejected. None of the North American sections, pro posed during the Brussels Symposium as the potential boundary stratotypes, i.e. Wagon Mound and Pueblo sections, appears better than the voted section of the Salzgitter-Salder. The Pueblo section is relatively complete but markedly condensed in comparison with the German one, but it may be used as a very convenient reference section for the Turonian/Coniacian boundary in the Western Interior. -
Report 2015–1087
Chronostratigraphic Cross Section of Cretaceous Formations in Western Montana, Western Wyoming, Eastern Utah, Northeastern Arizona, and Northwestern New Mexico, U.S.A. Pamphlet to accompany Open-File Report 2015–1087 U.S. Department of the Interior U.S. Geological Survey Chronostratigraphic Cross Section of Cretaceous Formations in Western Montana, Western Wyoming, Eastern Utah, Northeastern Arizona, and Northwestern New Mexico, U.S.A. By E.A. Merewether and K.C. McKinney Pamphlet to accompany Open-File Report 2015–1087 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Merewether, E.A., and McKinney, K.C., 2015, Chronostratigraphic cross section of Cretaceous formations in western Montana, western Wyoming, eastern Utah, northeastern Arizona, and northwestern New Mexico, U.S.A.: U.S. Geological Survey Open-File Report 2015–1087, 10 p. -
Turonian–Campanian Strata East of the Trans-Alaska Pipeline Corridor, North Slope Foothills, Alaska: Progress During the 2001–02 and 2007 Field Seasons
PIR 2008-1G 85 TURONIAN–CAMPANIAN STRATA EAST OF THE TRANS-ALASKA PIPELINE CORRIDOR, NORTH SLOPE FOOTHILLS, ALASKA: PROGRESS DURING THE 2001–02 AND 2007 FIELD SEASONS by David L. LePain1, Russell Kirkham2, Robert Gillis1, and Jacob Mongrain3 ABSTRACT Lower Turonian through Campanian strata are discontinuously exposed along an unnamed drainage approximately 6 km east of the Sagavanirktok River, in the Sagavanirktok Quadrangle, in the foothills north of the Brooks Range. In spite of some outcrop-scale deformation, this succession is viewed as a rela- tively continuous and unbroken succession deposited basinward (east and north) of the terminal Nanushuk shelf edge. South-dipping exposures of sandstone, siltstone, and tuff are separated by long tundra-covered intervals inferred to be underlain by fi ner-grained lithologies. Field studies by DGGS in 2001, 2002, and 2007 document the depositional setting of this succession and provide a framework for more detailed facies analysis and bedrock geological mapping in the area. Lower Turonian strata at the northwest end of the succession consist dominantly of shale with 18–30- m-thick packages of interbedded mudstone and sandstone recording deposition as sandstone lobes in basin fl oor settings. This part of the succession is tentatively correlated with Seabee Formation west of the Trans- Alaska pipeline corridor. Santonian to lower Campanian strata in the middle of the succession also consist dominantly of shaly lithologies interrupted by 25–60-m-thick packages of interbedded mudstone, sandstone, minor conglomerate, and silicifi ed tuff deposited as sandstone lobes and overbank deposits (levees) and submarine ashfalls in proximal basin to lower slope settings. -
Upper Cretaceous Subsurface Stratigraphy and Structure of Coastal Georgia and South Carolina
i, 5 Upper Cretaceous Subsurface Stratigraphy and Structure of Coastal Georgia and South Carolina GEOtQGIC AL SURVE:Y PROFESSIONAL PAPER 1222 Upper Cretaceous Subsurface Stratigraphy and Structure of Coastal Georgia and South Carolina By PAGE C. VALENTINE GEOLOGICAL SURVEY PROFESSIONAL PAPER 1222 A study based on 24 wells along transects from the Southeast Georgia Embayment northeastward to the Cape Fear Arch and offshore to the Outer Continental Shelf UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Valentine, Page C. Upper Cretaceous subsurface stratigraphy and structure of coastal Georgia and South Carolina. (Geological Survey professional paper ; 1222) "A study based on 24 wells along transects from the Southeast Georgia Embayment northeastward to the Cape Fear Arch and offshore to the Outer Continental Shelf." Bibliography: p. Supt. of Docs, no.: 119.16:1222 1. Geology, Stratigraphic-Cretaceous. 2. Geology-Georgia. 3. Geology-South Carolina. 4. Coasts-Georgia. 5. Coasts-South Carolina. I. Title. II. Series: United States. Geological Survey. Professional paper ; 1222. QE688.V35 551.7T09757 80-607868 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Abstract ___________. Upper Cretaceous stratigraphy-Continued Introduction _________. Clubhouse Crossroads corehole 1, South Carolina _____ 15 Acknowledgments