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Actas Del Vi Simposio De La Red Latinoamericana De Estudios Sobre Imagen, Identidad Y Territorio
ACTAS DEL VI SIMPOSIO DE LA RED LATINOAMERICANA DE ESTUDIOS SOBRE IMAGEN, IDENTIDAD Y TERRITORIO “ESCENARIOS DE INQUIETUD. CIUDADES, POÉTICAS, POLÍTICAS” 14, 15 Y 16 DE NOVIEMBRE DE 2016 MICAELA CUESTA M. FERNANDA GONZÁLEZ MARÍA STEGMAYER (COMPS.) 2 Cuesta, Micaela Actas del VI Simposio de la Red Latinoamericana de estudios sobre Imagen, Identidad y Territorio : escenarios de inquietud : ciudades, poéticas, políticas / Micaela Cuesta ; María Fernanda González ; María Stegmayer. - 1a ed compendiada. - Ciudad Autónoma de Buenos Aires : Departamento de Publicaciones de la Facultad de Derecho y Ciencias Sociales de la Universidad de Buenos Aires. Instituto de Investigaciones Gino Germani - UBA, 2016. Libro digital, PDF Archivo Digital: descarga y online ISBN 978-987-3810-27-5 1. Identidad. 2. Imagen. 3. Actas de Congresos. I. González, María Fernanda II. Stegmayer, María III. Título CDD 306 3 ÍNDICE Presentación .............................................................................................................................. 5 Ciudades y memorias Sesión de debates I: Cuerpo y espacio Ciudades performativas: Teatralidad, memoria y experiencia..................................................... 11 Lorena Verzero Fioravante e o vazio: o desenho como estratégia de ausência................................................... 21 Eduardo Vieira da Cunha Percepción geográfica del espacio y los cuatro elementos: Reflexión sobre una interfaz entre fenomenología y astrología......................................................................................................... -
Assembly, Configuration, and Break-Up History of Rodinia
Author's personal copy Available online at www.sciencedirect.com Precambrian Research 160 (2008) 179–210 Assembly, configuration, and break-up history of Rodinia: A synthesis Z.X. Li a,g,∗, S.V. Bogdanova b, A.S. Collins c, A. Davidson d, B. De Waele a, R.E. Ernst e,f, I.C.W. Fitzsimons g, R.A. Fuck h, D.P. Gladkochub i, J. Jacobs j, K.E. Karlstrom k, S. Lu l, L.M. Natapov m, V. Pease n, S.A. Pisarevsky a, K. Thrane o, V. Vernikovsky p a Tectonics Special Research Centre, School of Earth and Geographical Sciences, The University of Western Australia, Crawley, WA 6009, Australia b Department of Geology, Lund University, Solvegatan 12, 223 62 Lund, Sweden c Continental Evolution Research Group, School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia d Geological Survey of Canada (retired), 601 Booth Street, Ottawa, Canada K1A 0E8 e Ernst Geosciences, 43 Margrave Avenue, Ottawa, Canada K1T 3Y2 f Department of Earth Sciences, Carleton U., Ottawa, Canada K1S 5B6 g Tectonics Special Research Centre, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia h Universidade de Bras´ılia, 70910-000 Bras´ılia, Brazil i Institute of the Earth’s Crust SB RAS, Lermontova Street, 128, 664033 Irkutsk, Russia j Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway k Department of Earth and Planetary Sciences, Northrop Hall University of New Mexico, Albuquerque, NM 87131, USA l Tianjin Institute of Geology and Mineral Resources, CGS, No. -
Helicobacter Pylori's Historical Journey Through Siberia and the Americas
Helicobacter pylori’s historical journey through Siberia and the Americas Yoshan Moodleya,1,2, Andrea Brunellib,1, Silvia Ghirottoc,1, Andrey Klyubind, Ayas S. Maadye, William Tynef, Zilia Y. Muñoz-Ramirezg, Zhemin Zhouf, Andrea Manicah, Bodo Linzi, and Mark Achtmanf aDepartment of Zoology, University of Venda, Thohoyandou 0950, Republic of South Africa; bDepartment of Life Sciences and Biotechnology, University of Ferrara, 44121 Ferrara, Italy; cDepartment of Mathematics and Computer Science, University of Ferrara, 44121 Ferrara, Italy; dDepartment of Molecular Biology and Genetics, Research Institute for Physical-Chemical Medicine, 119435 Moscow, Russia; eDepartment of Diagnostic and Operative Endoscopy, Pirogov National Medical and Surgical Center, 105203 Moscow, Russia; fWarwick Medical School, University of Warwick, Coventry CV4 7AL, United Kingdom; gLaboratorio de Bioinformática y Biotecnología Genómica, Escuela Nacional de Ciencias Biológicas, Unidad Profesional Lázaro Cárdenas, Instituto Politécnico Nacional, 11340 Mexico City, Mexico; hDepartment of Zoology, University of Cambridge, Cambridge CB2 3EJ, United Kingdom; and iDepartment of Biology, Division of Microbiology, Friedrich Alexander University Erlangen-Nuremberg, 91058 Erlangen, Germany Edited by Daniel Falush, University of Bath, Bath, United Kingdom, and accepted by Editorial Board Member W. F. Doolittle April 30, 2021 (received for review July 22, 2020) The gastric bacterium Helicobacter pylori shares a coevolutionary speakers). However, H. pylori’s presence, diversity, and structure history with humans that predates the out-of-Africa diaspora, and in northern Eurasia are still unknown. This vast region, hereafter the geographical specificities of H. pylori populations reflect mul- Siberia, extends from the Ural Mountains in the west to the tiple well-known human migrations. We extensively sampled H. -
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R
Proterozoic East Gondwana: Supercontinent Assembly and Breakup Geological Society Special Publications Society Book Editors R. J. PANKHURST (CHIEF EDITOR) P. DOYLE E J. GREGORY J. S. GRIFFITHS A. J. HARTLEY R. E. HOLDSWORTH A. C. MORTON N. S. ROBINS M. S. STOKER J. P. TURNER Special Publication reviewing procedures The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society's Books Editorial Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society has a team of Book Editors (listed above) who ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satis- factory review by two independent referees. The questions on the review forms are similar to those for Journal of the Geological Society. The referees' forms and comments must be available to the Society's Book Editors on request. Although many of the books result from meetings, the editors are expected to commission papers that were not pre- sented at the meeting to ensure that the book provides a balanced coverage of the subject. Being accepted for presentation at the meeting does not guarantee inclusion in the book. Geological Society Special Publications are included in the ISI Science Citation Index, but they do not have an impact factor, the latter being applicable only to journals. -
African Families in a Global Context
RR13X.book Page 1 Monday, November 14, 2005 2:20 PM RESEARCH REPORT NO. 131 AFRICAN FAMILIES IN A GLOBAL CONTEXT Edited by Göran Therborn Nordiska Afrikainstitutet, Uppsala 2006 RR13X.book Page 2 Monday, November 14, 2005 2:20 PM Indexing terms Demographic change Family Family structure Gender roles Social problems Africa Ghana Nigeria South Africa African Families in a Global Context Second edition © the authors and Nordiska Afrikainstitutet, 2004 Language checking: Elaine Almén ISSN 1104-8425 ISBN 91-7106-561-X (print) 91-7106-562-8 (electronic) Printed in Sweden by Elanders Infologistics Väst AB, Göteborg 2006 RR13X.book Page 3 Monday, November 14, 2005 2:20 PM Contents Preface . 5 Author presentations . 7 Introduction Globalization, Africa, and African Family Pattern . 9 Göran Therborn 1. African Families in a Global Context. 17 Göran Therborn 2. Demographic Innovation and Nutritional Catastrophe: Change, Lack of Change and Difference in Ghanaian Family Systems . 49 Christine Oppong 3. Female (In)dependence and Male Dominance in Contemporary Nigerian Families . 79 Bola Udegbe 4. Globalization and Family Patterns: A View from South Africa . 98 Susan C. Ziehl RR13X.book Page 4 Monday, November 14, 2005 2:20 PM RR13X.book Page 5 Monday, November 14, 2005 2:20 PM Preface In the mid-1990s the Swedish Council for Planning and Coordination of Research (Forskningsrådsnämnden – FRN) – subsequently merged into the Council of Sci- ence (Vetenskaprådet) – established a national, interdisciplinary research committee on Global Processes. The Committee has been strongly committed to a multidi- mensional and multidisciplinary approach to globalization and global processes and to using regional perspectives. -
Paleomagnetic and Geochronological Studies of the Mafic Dyke Swarms Of
Precambrian Research 198–199 (2012) 51–76 Contents lists available at SciVerse ScienceDirect Precambrian Research journa l homepage: www.elsevier.com/locate/precamres Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, central India: Implications for the tectonic evolution and paleogeographic reconstructions a,∗ a b a c Vimal R. Pradhan , Joseph G. Meert , Manoj K. Pandit , George Kamenov , Md. Erfan Ali Mondal a Department of Geological Sciences, University of Florida, 241 Williamson Hall, Gainesville, FL 32611, USA b Department of Geology, University of Rajasthan, Jaipur 302004, Rajasthan, India c Department of Geology, Aligarh Muslim University, Aligarh 202002, India a r t i c l e i n f o a b s t r a c t Article history: The paleogeographic position of India within the Paleoproterozoic Columbia and Mesoproterozoic Received 12 July 2011 Rodinia supercontinents is shrouded in uncertainty due to the paucity of high quality paleomagnetic Received in revised form 6 November 2011 data with strong age control. New paleomagnetic and geochronological data from the Precambrian mafic Accepted 18 November 2011 dykes intruding granitoids and supracrustals of the Archean Bundelkhand craton (BC) in northern Penin- Available online 28 November 2011 sular India is significant in constraining the position of India at 2.0 and 1.1 Ga. The dykes are ubiquitous within the craton and have variable orientations (NW–SE, NE–SW, ENE–WSW and E–W). Three dis- Keywords: tinct episodes of dyke intrusion are inferred from the paleomagnetic analysis of these dykes. The older Bundelkhand craton, Mafic dykes, Central ◦ NW–SE trending dykes yield a mean paleomagnetic direction with a declination = 155.3 and an incli- India, Paleomagnetism, Geochronology, ◦ ◦ − Ä ˛ Paleogeography nation = 7.8 ( = 21; 95 = 9.6 ). -
World Heritage Cultural Landscapes a Handbook for Conservation and Management
World Heritage papers26 World Heritage Cultural Landscapes A Handbook for Conservation and Management World Heritage Cultural Landscapes A Handbook for Conservation and Management Nora Mitchell, Mechtild Rössler, Pierre-Marie Tricaud (Authors/Ed.) Drafting group Nora Mitchell, Mechtild Rössler, Pierre-Marie Tricaud Editorial Assistant Christine Delsol Contributors Carmen Añón Feliú Alessandro Balsamo* Francesco Bandarin* Disclaimer Henry Cleere The ideas and opinions expressed in this publication are those of Viera Dvoráková the authors and are not necessarily those of UNESCO and do not Peter Fowler commit the Organization. Eva Horsáková Jane Lennon The designations employed and the presentation of material in this Katri Lisitzin publication do not imply the expression of any opinion whatsoever Kerstin Manz* on the part of UNESCO concerning the legal status of any country, Nora Mitchell territory, city or area or of its authorities, or concerning the delim- Meryl Oliver itation of its frontiers or boundaries. Saúl Alcántara Onofre John Rodger Published in November 2009 by the UNESCO World Heritage Centre Mechtild Rossler* Anna Sidorenko* The publication of this volume was financed by the Netherlands Herbert Stovel Fund-in-Trust. Pierre-Marie Tricaud Herman van Hooff* Augusto Villalon World Heritage Centre Christopher Young UNESCO (* UNESCO staff) 7, place de Fontenoy 75352 Paris 07 SP France Coordination of the World Heritage Paper Series Tel. : 33 (0)1 45 68 15 71 Vesna Vujicic Lugassy Fax: 33 (0)1 45 68 55 70 Website: http://whc.unesco.org -
World Map Showing Surface and Subsurface Distribution, and Lithologic Character of Middle and Late Neoproterozoic Rocks
World Map Showing Surface and Subsurface Distribution, and Lithologic Character of Middle and Late Neoproterozoic Rocks By John H. Stewart1 Open-File Report 2007-1087 2007 U.S. Department of the Interior U.S. Geological Survey 1 Menlo Park, Calif. U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2007 Revised and reprinted: 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Stewart, John H., 2007, World map showing surface and subsurface distribution, and lithologic character of Middle and Late Neoproterozoic rocks: U.S. Geological Survey Open-File Report 2007-1087. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Introduction......................................................................................................................... 3 Sources of information ........................................................................................................ 2 Africa [AF] -
Pan-African Orogeny 1
Encyclopedia 0f Geology (2004), vol. 1, Elsevier, Amsterdam AFRICA/Pan-African Orogeny 1 Contents Pan-African Orogeny North African Phanerozoic Rift Valley Within the Pan-African domains, two broad types of Pan-African Orogeny orogenic or mobile belts can be distinguished. One type consists predominantly of Neoproterozoic supracrustal and magmatic assemblages, many of juvenile (mantle- A Kröner, Universität Mainz, Mainz, Germany R J Stern, University of Texas-Dallas, Richardson derived) origin, with structural and metamorphic his- TX, USA tories that are similar to those in Phanerozoic collision and accretion belts. These belts expose upper to middle O 2005, Elsevier Ltd. All Rights Reserved. crustal levels and contain diagnostic features such as ophiolites, subduction- or collision-related granitoids, lntroduction island-arc or passive continental margin assemblages as well as exotic terranes that permit reconstruction of The term 'Pan-African' was coined by WQ Kennedy in their evolution in Phanerozoic-style plate tectonic scen- 1964 on the basis of an assessment of available Rb-Sr arios. Such belts include the Arabian-Nubian shield of and K-Ar ages in Africa. The Pan-African was inter- Arabia and north-east Africa (Figure 2), the Damara- preted as a tectono-thermal event, some 500 Ma ago, Kaoko-Gariep Belt and Lufilian Arc of south-central during which a number of mobile belts formed, sur- and south-western Africa, the West Congo Belt of rounding older cratons. The concept was then extended Angola and Congo Republic, the Trans-Sahara Belt of to the Gondwana continents (Figure 1) although West Africa, and the Rokelide and Mauretanian belts regional names were proposed such as Brasiliano along the western Part of the West African Craton for South America, Adelaidean for Australia, and (Figure 1). -
Non-Cylindrical Parasitic Folding and Strain Partitioning
Solid Earth Discuss., https://doi.org/10.5194/se-2018-6 Manuscript under review for journal Solid Earth Discussion started: 6 February 2018 c Author(s) 2018. CC BY 4.0 License. Non-cylindrical parasitic folding and strain partitioning during the Pan-African Lufilian orogeny in the Chambishi-Nkana Basin, Central African Copperbelt Koen Torremans1, Philippe Muchez1, Manuel Sintubin2 5 1KU Leuven, Department of Earth and Environmental Sciences, Geodynamics and Geofluids Research Group, Celestijnenlaan 200E, 3001 Leuven, Belgium. 2Present address: Irish Centre for Research in Applied Geosciences, University College Dublin, Dublin 4, Ireland. Correspondence to: Koen Torremans ([email protected]) 1 Solid Earth Discuss., https://doi.org/10.5194/se-2018-6 Manuscript under review for journal Solid Earth Discussion started: 6 February 2018 c Author(s) 2018. CC BY 4.0 License. Abstract. A structural analysis has been carried out along the southeast margin of the Chambishi-Nkana Basin in the Central African Copperbelt, hosting the world-class Cu-Co Nkana orebody. The geometrically complex structural architecture is interpreted to have been generated during a single NE-SW oriented compressional event, clearly linked to the Pan-African 5 Lufilian orogeny. This progressive deformation resulted primarily in asymmetric multiscale parasitic fold assemblages, characterized by non-cylindrical NW-SE elongated, periclinal folds that strongly interfere laterally, leading to fold linkage and bifurcation. The vergence and amplitude of these folds consistently reflect their position along an inclined limb of a NW plunging megascale first-order fold. A clear relation is observed between development of parasitic folds and certain lithofacies assemblages in the Copperbelt Orebody Member, which hosts most of the ore. -
Ai-/Ais-Richtersveld Transfrontier Park “Since This Spectacular Area Is Undeveloped and There Is So Much to Explore, You Feel As If No One Else Has Ever Been Here
/Ai-/Ais-Richtersveld Transfrontier Park “Since this spectacular area is undeveloped and there is so much to explore, you feel as if no one else has ever been here. That the park is yours alone to discover.” Wayne Handley, Senior Ranger, /Ai-/Ais Richtersveld Republic of Namibia Transfrontier Park, Ministry of Environment and Tourism Ministry of Environment and Tourism Discover the /Ai-/Ais Richtersveld 550 metres above. Klipspringer bound up the cliffs and moun- Transfrontier Park tain chats drink from pools left behind from when the river last Experience wilderness on a scale unimaginable. Stand at the edge flowed. Ancient rock formations and isolation add to the sense of of the largest natural gorge in Africa, and the second-largest can- timelessness and elation that mark this challenging hike. yon in the world, the Fish River Canyon. Revel in the dramatic views from Hell’s Corner where it is almost possible to imagine For 4x4 enthusiasts, drives along the rugged eastern rim of the the dramatic natural forces that shaped the canyon. Today the canyon afford stunning views across the canyon from Hell’s /Ai-/Ais Richtersveld Transfrontier Park protects a vast area that Corner and Sulphur Springs vantage points. One hundred ki- crosses the South African border to encompass one of the richest lometres further south, another more leisurely route winds botanical hot spots in the world, the Succulent Karoo biome. along the edge of the Orange River, where masses of water are framed by towering black mountains. Strewn with immense boulders, the bed of the Fish River is also home to one of the most exhilarating adventures in Southern Everywhere there are rare plants, including 100 endemic suc- Africa, the five-day, 90-kilometre Fish River Canyon hiking trail, culents and over 1 600 other plant species, illusive rare animals, for which you need a hiking permit. -
The Structural and Metamorphic Evolution of the Neoproterozoic Basement in Jebel Ja’Alan, East Oman
The Structural and Metamorphic Evolution of the Neoproterozoic Basement in Jebel Ja’alan, East Oman Thesis submitted in accordance with the requirements of the University of Adelaide for an Honours Degree in Geology Brandon Luke Alessio November 2015 Brandon Alessio Neoproterozoic Evolution of Jebel Ja’alan THE STRUCTURAL AND METAMORPHIC EVOLUTION OF THE NEOPROTEROZOIC BASEMENT IN JEBEL JA’ALAN, EAST OMAN RUNNING TITLE: NEOPROTEROZOIC EVOLUTION OF JEBEL JA’ALAN ABSTRACT Jebel Ja’alan (east Oman) displays some of the best exposed and easternmost basement rock in the country. It comprises metasedimentary and intrusive igneous rocks, interpreted to have been generated within the Mozambique Ocean at the margin of Neoproterozoic India. The metamorphic conditions experienced by the basement and implications these conditions have for tectonic models of the region were, until now, poorly understood. The aim of this paper is to constrain these conditions in order to test the hypothesis that the basement of Jebel Ja’alan formed in a Neoproterozoic volcanic arc and unravel the relationship between the structural and metamorphic evolution of the region. Phase equilibria modelling constrains peak metamorphic conditions to c. 670–700 °C and 4.5–6 kbar, following a clockwise P–T path. These conditions are not exclusive to an arc environment but are suggested to represent one due to current and previous interpretations of basement formation based on its geochemistry. U–Pb monazite age data of Hassan Schist samples yields a weighted average age of 833 ± 15 Ma, interpreted to be the age of near peak metamorphism, and is supported by 40Ar–39Ar muscovite age data, which yields a plateau age of 830 ± 6 Ma.