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Petrological and Geochemical Characteristics of Metamorphic and Igneous Units from the Allochthonous Madre De Dios Terrane, Southern Chile ⁎ F.A
Petrological and geochemical characteristics of metamorphic and igneous units from the allochthonous Madre de Dios Terrane, Southern Chile ⁎ F.A. Sepúlveda a, , F. Hervé a, M. Calderón a, J.P. Lacassie b,c a Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Casilla 13518, Correo 21, Santiago, Chile b Paleoproterozoic Mineralization Research Group, Department of Geology, University of Johannesburg, Auckland Park, Johannesburg, 2006, South Africa c SERNAGEOMIN, Av. Santa María 0104, Providencia, Santiago, Chile Abstract The Denaro Complex, part of the Madre de Dios Terrane is composed of metamorphosed pillow basalts, metahyaloclastites, banded metalliferous and radiolarian metacherts, metapelites and redeposited calcareous metasandstones. The basaltic rocks show primary textures, minerals and structures. They are foliated especially in the vicinities of thrust faults, interpreted to have developed during the accretion of the terrane to the Gondwana margin. Composition of relic primary augite and chromite crystals plots into the MORB field of tectonic discriminant diagrams, as do the analyses of whole rock geochemistry, which indicates that these rocks are akin to volcanic rocks erupted along a constructive plate margin (N- and E-type MORBs), probably in a spreading axis-centered oceanic plateau or ridge. The metamorphic assemblages of pumpellyite–actinolite facies bear witness of metamorphism in a frontal accretionary wedge at elevated P and low T conditions, probably related to the Late Triassic–Early Jurassic Chonide event, which has been recognized elsewhere in the Patagonian Andes. Keywords: Metamorphism; Terrane accretion; Pumpellyite–actinolite facies; Seamount subduction; Frontal accretion 1. Introduction The rocks which crop out at the Madre de Dios archipelago (50°–50°50'S), referred to by Hervé and Mpodozis (2005) as 1.1. -
Geologists of Russian Origin in Latin America
REVISTA DEL MUSEO DE LA PLATA 2018, Volumen 3, Número 2: 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1 , A.C. Riccardi 2 , †M. Durand Delga3 , R. Alonso 4 , 7 8 M. Wiasemsky5 , D. Boltovskoy 6 , R. Charrier , E. Minina 1Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3Passed away August19, 2012 4Universidad Nacional de Salta, Argentina, [email protected] 581, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6Dep. Ecologia, Genetica y Evolucion, Fac. Ciencias Exactas y Naturales, Univ. de Buenos Aires, Argentina, [email protected] 7History of Geology Group, Sociedad Geológica de Chile, Santiago de Chile, [email protected] 8State Geological Museum “V.I.Vernadsky”, Mohovaya ul. 11/11, Moscow 125009, Russian Federation, [email protected] REVISTA DEL MUSEO DE LA PLATA / 2018, Volumen 3, Número 2: 223-295 / ISSN 2545-6377 ISSN 2545-6377 UNIVERSIDAD NACIONAL DE LA PLATA - FACULTAD DE CIENCIAS NATURALES Y MUSEO Revista del Museo de La Plata 2018 Volumen 3, Número 2 (Julio-Diciembre): 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1, A.C. Riccardi2, †M. Durand Delga3, R. Alonso4, M. Wiasemsky5, D. Boltovskoy6, R. Charrier7, E. Minina8 1 Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2 Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3 Passed away August19, 2012 4 Universidad Nacional de Salta, Argentina, [email protected] 5 81, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6 Dep. -
GONDWANA I11 Du Toit
GONDWANA 503 i11 du Toit < Gondwana, Samfrau > ... the really important point is not so much to disprove Wegener’s particular views as to decide from the relevant evidence whether or not continental drift is a genuine variety of earth movement. —Holmes, 1944.1 A geologist who looked for geological evidence to test Wegener’s hypothesis of continental drift was Alexander Logie du Toit (1878-1948). As a field geologist for the Geological Survey of South Africa he became familiar with the regional geology of that country. Curious to see firsthand how well, if at all, the geology either side of the Atlantic matched, he applied for and upon receiving a generous grant from the Carnegie Institution of Washington in 1923 he spent five months in South America familiarizing himself with the geology of Argentina, Paraguay and Brazil. His seminal paper, A Geological Comparison of South America with South Africa, was published in 1927. He wrote, “The concordance between the opposed shores, incidentally pointed out and discussed by others long before Wegener, has consistently been extended by each fresh geological observation until at present the amount of agreement is 5 In his book, Our Wandering Continents nothing short of marvellous.” Persuasive of a former (1937)2 is the statement: “from the proximity of the two continents are the discoverable linkages mid-Palaeozoic onwards the lands must have that “cross from coast to coast, not only directly but crept northwards for thousands of kilometers diagonally as well, and are furthermore of widely different to account for their deduced climatic ages.” In the map to illustrate this tectonic and phasal (lateral vicissitudes. -
Letter from the President
1 ISSN 1028-1533 International Commission on the History of Geological Sciences INHIGEO NEWSLETTER I No. 44 Covering activitiesI generally in 2011 Issued in 2012 INHIGEO is A Commission of the International Union of Geological Sciences & An affiliate of the International Union of the History and Philosophy of Sciences Compiled and Edited by Barry J. Cooper INHIGEO Secretary-General Printed in Adelaide, South Australia on request Available at www.inhigeo.org 2 3 CONTENTS INHIGEO Newsletter No. 44 (Published in May 2012 covering events generally in 2011) INHIGEO BOARD 6 REPORTS President‘s Message: Silvia Figueirôa 7 Secretary-General‘s Report: Barry Cooper 7 INHIGEO 2012 - BRISBANE, AUSTRALIA 9 INHIGEO BUSINESS NOTICES Minutes of 2011 INHIGEO Business Meeting, Toyohashi, Japan 11 Provisional Agenda INHIGEO Business Meeting, Brisbane, Australia, August 2012 17 Report on ad hoc review by IUGS of INHIGEO, Toyohashi, Japan 17 Revision of the INHIGEO Terms of Reference and By Laws 21 Liaison with other IUGS Commissions and Task Groups 22 CONFERENCE REPORTS INHIGEO Japan, August 2011 23 Austrian Working Group ―History of Earth Sciences‖ Meetings, 2011 29 Conference on ―Geological Collectors and Collecting‖, April 2011 30 Report on the ―Antarctic history: Probing the unknown‖ workshop, July 2011 31 Second Symposium: History of Geology of Chile, August 2011 31 International Conference on the History of Geology and Medicine, November, 2011 33 Centenary Congress, Royal Geological & Mining Society, Netherlands, March 2012 35 EXHIBITION Hungarian -
Supercontinent Evolution and the Proterozoic Metallogeny of South America ⁎ João Batista Guimarães Teixeira A, , Aroldo Misi A, Maria Da Glória Da Silva A,B
Gondwana Research 11 (2007) 346–361 www.elsevier.com/locate/gr GR Focus Supercontinent evolution and the Proterozoic metallogeny of South America ⁎ João Batista Guimarães Teixeira a, , Aroldo Misi a, Maria da Glória da Silva a,b a Grupo de Metalogênese, Centro de Pesquisa em Geofísica e Geologia, Universidade Federal da Bahia, Campus Universitário de Ondina, Sala 201-C, Salvador, 40170-290, Bahia, Brazil b Geological Survey of Brazil (CPRM)-Av. Pasteur, 404, Urca, Rio de Janeiro, 22290-240, Rio de Janeiro, Brazil Received 2 May 2004; accepted 1 May 2006 Available online 8 August 2006 Abstract The cratonic blocks of South America have been accreted from 2.2 to 1.9 Ga, and all of these blocks have been previously involved in the assembly and breakup of the Paleoproterozoic Atlantica, the Mesoproterozoic to Neoproterozoic Rodinia, and the Neoproterozoic to Phanerozoic West Gondwana continents. Several mineralization phases have sequentially taken place during Atlantica evolution, involving Au, U, Cr, W, and Sn. During Rodinia assembly and breakup and Gondwana formation, the crust-dominated metallogenic processes have been overriding, responsible for several mineral deposits, including Au, Pd, Sn, Ni, Cu, Zn, Mn, Fe, Pb, U, P2O5, Ta, W, Li, Be and precious stones. During Rodinia breakup, epicontinental carbonate-siliciclastic basins were deposited, which host important non-ferrous base metal deposits of Cu–Co and Pb–Zn–Ag in Africa and South America. Isotope Pb–Pb analyses of sulfides from the non-ferrous deposits unambiguously indicate an upper crustal source for the metals. A genetic model for these deposits involves extensional faults driving the circulation of hydrothermal mineralizing fluids from the Archean/Paleoproterozoic basement to the Neoproterozoic sedimentary cover. -
Cenozoic Contractional Tectonics in the Fuegian Andes, Southernmost South America: a Model for the Transference of Orogenic Shortening to the Foreland
Geologica Acta, Vol.11, Nº 3, September 2013, 331-357 DOI: 10.1344/105.000001874 Available online at www.geologica-acta.com Cenozoic contractional tectonics in the Fuegian Andes, southernmost South America: a model for the transference of orogenic shortening to the foreland 1 2 P.J. TORRES CARBONELL and L.V. DIMIERI 1 Centro Austral de Investigaciones Científicas (CADIC-CONICET) Bernardo A. Houssay 200, 9410 Ushuaia, Tierra del Fuego, Argentina. E-mail: [email protected] 2 Instituto Geológico del Sur (INGEOSUR-CONICET), Departamento de Geología, Universidad Nacional del Sur San Juan 670, 8000 Bahía Blanca, Buenos Aires, Argentina. E-mail: [email protected] ABS TRACT The Fuegian thrust-fold belt has been subjected to significant shortening during the Cenozoic. Although contemporaneous shortening and uplift was also recognized in the Fuegian Andes central belt (hinterland), previous studies stated that most of that deformation developed out-of-sequence with the thrust-fold belt and hence did not contribute to its shortening. Therefore, no suitable geometric and kinematic model has been proposed for the mechanism that links deformation in both domains. Here we address the style and timing of the younger (Late Cretaceous-Paleogene) structures of the central belt and the structural evolution of the thrust-fold belt, based on published and own data. We reinterpret the style of the central belt structures, proposing a new model in which basement thrusting in the central belt caused all the shortening in the foreland cover. We postulate that the basement was involved in a regional-scale duplex whose roof thrust was the décollement of the thin-skinned thrust-fold belt. -
The Argentine Republic ^ the Argentine Republic
Dear Reader, This book was referenced in one of the 185 issues of 'The Builder' Magazine which was published between January 1915 and May 1930. To celebrate the centennial of this publication, the Pictoumasons website presents a complete set of indexed issues of the magazine. As far as the editor was able to, books which were suggested to the reader have been searched for on the internet and included in 'The Builder' library.' This is a book that was preserved for generations on library shelves before it was carefully scanned by one of several organizations as part of a project to make the world's books discoverable online. Wherever possible, the source and original scanner identification has been retained. Only blank pages have been removed and this header- page added. The original book has survived long enough for the copyright to expire and the book to enter the public domain. A public domain book is one that was never subject to copyright or whose legal copyright term has expired. Whether a book is in the public domain may vary country to country. Public domain books belong to the public and 'pictoumasons' makes no claim of ownership to any of the books in this library; we are merely their custodians. Often, marks, notations and other marginalia present in the original volume will appear in these files – a reminder of this book's long journey from the publisher to a library and finally to you. Since you are reading this book now, you can probably also keep a copy of it on your computer, so we ask you to Keep it legal. -
The Geology of South America - Almut Engler
GEOLOGY – Vol. IV – The Geology of South America - Almut Engler THE GEOLOGY OF SOUTH AMERICA Almut Engler Karl Franzens University of Graz, Graz, Austria Keywords: South America; geology; Andes, South American Platform, Patagonia, Western Gondwana, Cratons, Panafrican/Brasiliano Orogeny Contents 1. Introduction 2. Cratonic Regions 2.1. The Amazonian Craton 2.2. The São Francisco Craton 2.3. The São Luís Craton 2.4. The Rio de La Plata Craton and the Cratonic Region around Buenos Aires 3. Neoproterozoic Orogenic Systems 3.1. The Gurupi Fold Belt 3.2. The Borborema Province 3.3. The Tocantis Province 3.4. The Northern Mantiqueira Province 3.5. The Dom Feliciano Belt and Adjacent Terranes 4. Paleozoic Basement and Marginal Belts in Southwestern South America: Patagonia 5. The Andes 5.1. The Proto-Andean Margin 5.2. The Northern Andes 5.3. The Central Andes 5.4. The Southern Andes 5.5. Tectonic Evolution of the Andes 6. Sedimentary Basins Glossary Bibliography Biographical Sketch SummaryUNESCO – EOLSS The article deals with the geology and the geological evolution of the South American continent. The shield areas of the South American Platform, containing the cratonic regions surroundedSAMPLE by Neoproterozoic fold beltCHAPTERSs, consolidated during Late Proterozoic to Early Paleozoic times in contrast to the Patagonian Platform which mainly evolved during the Early Paleozoic, and has been tectono-thermally active up to the Cenozoic. The highest non-collisional mountain range of the world, the Andes, developed on the western continental margin of the plate, at least from the early Paleozoic on, and its evolution continues until today with active volcanism and seismicity due to continuous subduction of Pacific plates beneath the South American Plate. -
The Paleoproterozoic Record of the São Francisco Craton. Field Workshop, Brazil, 2006 the Paleoproterozoic Record of the São Francisco Craton
The Paleoproterozoic record of the São Francisco craton. Field workshop, Brazil, 2006 The Paleoproterozoic record of the São Francisco craton. Field workshop, Brazil, 2006 The Paleoproterozoic record of the São Francisco craton. Field workshop, Brazil, 2006 THE PALEOPROTEROZOIC RECORD OF THE SÃO FRANCISCO CRATON Field workshop 9-21 September 2006 Bahia and Minas Gerais, Brazil Hosted by the Departamento de Geologia, Escola de Minas, Universidade Federal de Ouro Preto and Instituto de Geociências Universidade da Bahia in collaboration with the International Geological Correlation Program IGCP 509 Palaeoproterozoic Supercontinents & Global Evolution FIELD GUIDE & ABSTRACTS The Paleoproterozoic record of the São Francisco craton. Field workshop, Brazil, 2006 Suggested citation Alkmim, F.F. and Noce, C.M. (eds.) 2006. The Paleoproterozoic Record of the São Francisco Craton. IGCP 509 Field workshop, Bahia and Minas Gerais, Brazil. Field Guide & Abstracts, 114 p. The Paleoproterozoic record of the São Francisco craton. Field workshop, Brazil, 2006 PREFACE The field workshop on the Paleoproterozoic During the first part of the workshop, the field record of the São Francisco craton was designed to trip traverses the Paleoproterozoic orogenic domain provide the participants with a general view of the of northern São Francisco craton in Bahia State, Paleoproterozoic geology of this part of the South emphasizing its most representative rock assemblages, American continent, and thus afford the opportunity tectonic features, and mineral deposits. The second to discuss outcrop evidence for the following topics field trip concentrates on the mining district of the of the scope of the IGCP 509: Quadrilátero Ferrífero in Minas Gerais State, which • Paleoclimatic and Paleoecological significance of corresponds to the foreland domain of the Paleoproterozoic banded iron formation and Paleoproterozoic Mineiro belt of the southern São carbonate sequences. -
A Review on the Tectonic Evolution of the Paleozoic-Triassic Basins from Patagonia: Record of Protracted Westward Migration of the Pre-Jurassic T Subduction Zone
Journal of South American Earth Sciences 95 (2019) 102256 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames A review on the tectonic evolution of the Paleozoic-Triassic basins from Patagonia: Record of protracted westward migration of the pre-Jurassic T subduction zone Rodrigo Suáreza,*, Pablo D. Gonzálezb, Matías C. Ghiglionea a Instituto de Estudios Andinos (Universidad de Buenos Aires - CONICET), Buenos Aires, Argentina b Instituto de Investigación en Paleobiología y Geología (Universidad Nacional de Río Negro - CONICET), General Roca, Argentina ARTICLE INFO ABSTRACT Keywords: The Paleozoic-Triassic Patagonian basins, at present comprising the Andean hinterland and structural basement Patagonia of active basins, document a pre-Jurassic evolution associated with accretionary processes at the paleo-Pacific Antarctic Peninsula convergent margin. The Early Cambrian basins constitute the earliest record for the emplacement of the Terra Accretionary orogenesis Australis Orogen in northern Patagonia and preserve metavolcanic strata derived from an extensional magmatic Retreating slab arc. Together, pre-Jurassic basins document the Early Cambrian to Late Triassic oceanward migration of the Pre-Jurassic trench-forearc system, evidencing that slab retreat was the common subduction setup. Tectonostratigraphy of Paleozoic-Triassic basins Detrital zircons these basins can be divided into three major sequences, from east to west: (i) early-middle Cambrian, (ii) Silurian-Carboniferous and (iii) Late Permian-late Triassic, which are separated by angular unconformities, evidencing large deformational pulses (advancing stages?) at Early Ordovician, early-middle Permian, and Late Triassic-Early Jurassic times. The Early Cambrian basins are mainly represented in the North Patagonian Massif by the Nahuel Niyeu forearc basin and the El Jagüelito backarc basin, which were closed and metamorphosed during the Early Ordovician. -
Geología Y Metalogénesis De Los Depósitos Y Manifestaciones ¡Illls Uraníferos De a 4 I R ■ ЩШ-Ÿ
Geología y Metalogénesis de los Depósitos y Manifestaciones ¡IlllS Uraníferos de A 4 i r ■ ЩШ-ÿ. Sudamérica A C T A S 9 DE UNA REUNION DE UN GRUPO DE TRABAJO О О О О О О SAN LUIS, ARGENTINA 'o О О О ç 21 A 23 DE SEPTIEMBRE DE 1981 Зо О о PROCEEDINGS OF A WORKING GROUP MEETING ООО SAN LUIS, ARGENTINA 21-23 SEPTEMBER 1981 <s><&„ ^ 0 ORGANISMO INTERNACIONAL DE ENERGIA ATOMICA,VIENA, 1984 & INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1984 GEOLOGIA Y METALOGENESIS DE LOS DEPOSITOS Y MANIFESTACIONES URANIFEROS DE SUD AMERICA GEOLOGY AND METALLOGENESIS OF URANIUM DEPOSITS OF SOUTH AMERICA Los siguientes Estados son Miembros del Organismo Internacional de Energía Atómica: AFGANISTAN INDIA REINO UNIDO DE GRAN BRETAÑA ALBANIA INDONESIA E IRLANDA DEL NORTE ARABIA SAUDITA IRAQ REPUBLICA ARABE SIRIA ARGELIA IRLANDA REPUBLICA DE COREA ARGENTINA ISLANDIA REPUBLICA DEMOCRATICA AUSTRALIA ISRAEL ALEMANA AUSTRIA ITALIA REPUBLICA DOMINICANA BANGLADESH JAMAHIRIYA ARABE REPUBLICA FEDERAL DE BELGICA LIBIA ALEMANIA BIRMANIA JAMAICA REPUBLICA ISLAMICA DE IRAN BOLIVIA JAPON REPUBLICA POPULAR DEMOCRATICA BRASIL JORDANIA DE COREA BULGARIA KAMPUCHEA DEMOCRATICA REPUBLICA SOCIALISTA SOVIETICA CANADA KENYA DE BIELORRUSIA COLOMBIA KUWAIT REPUBLICA SOCIALISTA SOVIETICA COSTA DE MARFIL LIBANO DE UCRANIA COSTA RICA LIBERIA REPUBLICA UNIDA DEL CAMERUN CUBA LIECHTENSTEIN REPUBLICA UNIDA DE TANZANIA CHECOSLOVAQUIA LUXEMBURGO RUMANIA CHILE MADAGASCAR SANTA SEDE CHINA MALASIA SENEGAL CHIPRE MALI SIERRA LEONA DINAMARCA MARRUECOS SINGAPUR ECUADOR MAURICIO SRI LANKA EGIPTO MEXICO -
The Upper Precambrian of South America
Boletim IG. Instituto de Geociências, USP. V. 7: 45 - 80, 1976 THE UPPER PRECAMBRIAN OF SOUTH AMERICA by Fernando F M de Almeida * Yociteru Hasui * Benjamim Bley de Brito Neves ** 1. INTRODUCTION A great deal of stratigraphic, petrogra events and units are more easily recognized. phic, structural, tectonic and geochronological The avajlable data on the Middle and l.ower data, as well as geological maps have been Precambrian are still insufficient for an ade published in the past decade on the Precam quate reconstruction of their geological his brian in South America. Some synthesis has tory. been made and the most important ones guided the elaboration of the Tectonic Maps of Brazil (Ferreira, 1972) and of South America (in This paper presents an approach of the print). structural framework and tectonic evolution of the South American Continent during The Upper Precamhrian (1) is the best the Precambrian, with emphasis on the Upper known time interval because its geological Precambrian time intervalo 2. THE SOUTH AMERICAN PLATFORM (2) The South American Platform is the merged under the Atlantic Oceano The Patago ancient platform of South America and oc nian Platform, consolidated in the Upper Paleo rupies the ml90r part of the continent. Its zoic, is at the southern Iimit of the South Ame western border was reworked by tecto-oroge rican Platform. The sedimentary cover over this nic processes of the Andean Chain, and its boundary difficults to trace its exact delinea boundary is covered by sediments. To the tion, but it should be located south of the north and east, the platform's borders are sub- Sierras Australes and east of the Sierras Trans- * Instituto de Geociências, Universidade de São Paulo - Caixa Postal, 20899 - São Paulo, SP - Brazil .