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A Review of the Neoproterozoic to Cambrian Tectonic Evolution
Accepted Manuscript Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution H. Fritz, M. Abdelsalam, K.A. Ali, B. Bingen, A.S. Collins, A.R. Fowler, W. Ghebreab, C.A. Hauzenberger, P.R. Johnson, T.M. Kusky, P. Macey, S. Muhongo, R.J. Stern, G. Viola PII: S1464-343X(13)00104-0 DOI: http://dx.doi.org/10.1016/j.jafrearsci.2013.06.004 Reference: AES 1867 To appear in: African Earth Sciences Received Date: 8 May 2012 Revised Date: 16 June 2013 Accepted Date: 21 June 2013 Please cite this article as: Fritz, H., Abdelsalam, M., Ali, K.A., Bingen, B., Collins, A.S., Fowler, A.R., Ghebreab, W., Hauzenberger, C.A., Johnson, P.R., Kusky, T.M., Macey, P., Muhongo, S., Stern, R.J., Viola, G., Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution, African Earth Sciences (2013), doi: http://dx.doi.org/10.1016/j.jafrearsci.2013.06.004 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. 1 Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian 2 tectonic evolution 3 H. -
Deformation and Sedimentary Evolution of the Lake Albert Rift (Uganda, East African Rift System)
Deformation and sedimentary evolution of the Lake Albert Rift (Uganda, East African Rift System) Brendan Simon, François Guillocheau, Cécile Robin, Olivier Dauteuil, Thierry Nalpas, Martin Pickford, Brigitte Senut, Philippe Lays, Philippe Bourges, Martine Bez To cite this version: Brendan Simon, François Guillocheau, Cécile Robin, Olivier Dauteuil, Thierry Nalpas, et al.. Defor- mation and sedimentary evolution of the Lake Albert Rift (Uganda, East African Rift System). Ma- rine and Petroleum Geology, Elsevier, 2017, 86, pp.17-37. 10.1016/j.marpetgeo.2017.05.006. insu- 01519685 HAL Id: insu-01519685 https://hal-insu.archives-ouvertes.fr/insu-01519685 Submitted on 9 May 2017 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. Accepted Manuscript Deformation and sedimentary evolution of the Lake Albert Rift (Uganda, East African Rift System) Brendan Simon, François Guillocheau, Cécile Robin, Olivier Dauteuil, Thierry Nalpas, Martin Pickford, Brigitte Senut, Philippe Lays, Philippe Bourges, Martine Bez PII: S0264-8172(17)30166-6 DOI: 10.1016/j.marpetgeo.2017.05.006 Reference: JMPG 2898 To appear in: Marine and Petroleum Geology Received Date: 19 November 2016 Revised Date: 29 March 2017 Accepted Date: 1 May 2017 Please cite this article as: Simon, B., Guillocheau, Franç., Robin, Cé., Dauteuil, O., Nalpas, T., Pickford, M., Senut, B., Lays, P., Bourges, P., Bez, M., Deformation and sedimentary evolution of the Lake Albert Rift (Uganda, East African Rift System), Marine and Petroleum Geology (2017), doi: 10.1016/ j.marpetgeo.2017.05.006. -
Table 2. Geographic Areas, and Biography
Table 2. Geographic Areas, and Biography The following numbers are never used alone, but may be used as required (either directly when so noted or through the interposition of notation 09 from Table 1) with any number from the schedules, e.g., public libraries (027.4) in Japan (—52 in this table): 027.452; railroad transportation (385) in Brazil (—81 in this table): 385.0981. They may also be used when so noted with numbers from other tables, e.g., notation 025 from Table 1. When adding to a number from the schedules, always insert a decimal point between the third and fourth digits of the complete number SUMMARY —001–009 Standard subdivisions —1 Areas, regions, places in general; oceans and seas —2 Biography —3 Ancient world —4 Europe —5 Asia —6 Africa —7 North America —8 South America —9 Australasia, Pacific Ocean islands, Atlantic Ocean islands, Arctic islands, Antarctica, extraterrestrial worlds —001–008 Standard subdivisions —009 History If “history” or “historical” appears in the heading for the number to which notation 009 could be added, this notation is redundant and should not be used —[009 01–009 05] Historical periods Do not use; class in base number —[009 1–009 9] Geographic treatment and biography Do not use; class in —1–9 —1 Areas, regions, places in general; oceans and seas Not limited by continent, country, locality Class biography regardless of area, region, place in —2; class specific continents, countries, localities in —3–9 > —11–17 Zonal, physiographic, socioeconomic regions Unless other instructions are given, class -
Re-Imagining and Re-Imaging the Development of the East African Rift
Thematic set: Tectonics and petroleum systems of East Africa Petroleum Geoscience Published Online First https://doi.org/10.1144/petgeo2017-036 Re-imagining and re-imaging the development of the East African Rift P. G. Purcell P&R Geological Consultants Pty Ltd, 141 Hastings Street, Scarborough, WA 6019, Australia P.G.P., 0000-0001-5006-5863 [email protected] Abstract: The East African Rift (EAR) has fascinated and challenged the geological imagination since its discovery nearly a century ago. A new series of images showing the sequential development of faulting and volcanism along the Rift from 45 Ma to present offers a regional overview of that development. The EAR is the latest phase of the extensive Phanerozoic rifting of the East African continental plate, interwoven with the lithospheric fabrics knitted together during its complex Proterozoic past. South of 5° S, the EAR variously follows or cuts across the Karoo rift trends; north of 5° S, it is almost totally within new or reworked Neoproterozoic terranes, while the Karoo rifts are almost totally outside them. The compilations raise several aspects of rift development seemingly in need of re-imagining, including tight-fit reconstructions of the Gulf of Aden, and the projection of Mesozoic rifts from Yemen to Somalia. Overall, the rifting process does not accord well with a mechanistic paradigm and is better imagined within the Prigoginian paradigm, which accepts instability and disorder within natural processes such as mantle plumes. The structural complexity of Afar and its non-alignment with magnetic anomalies suggests that the seafloor spreading process is, in its beginnings at least, more chaos than order. -
Rasbdb Subject Keywords
Leigh Marymor, Compiler KEYWORD GUIDE A joint project of the Museum of Northern Arizona and the Bay Area Rock Art Research Association KEYWORD GUIDE Compiled by Leigh Marymor, Research Associate, Museum of Northern Arizona. 1 September 15, 2020 KEYWORD GUIDE Mortars, cupules, and pecked curvilinear nucleated forms. Canyon Trail Park, San Francisco Bay Area, California, USA. Compiled by Leigh Marymor, Research Associate, Museum of Northern Arizona. 2 September 15, 2020 KEYWORD GUIDE Aerial Photography .......................................... 9 Archival storage ............................................... 9 Table of Contents Augmented Reality .......................................... 9 Bias ................................................................... 9 INTRODUCTION: .................................................. 7 Casts ................................................................. 9 Classification .................................................... 9 SUBJECT KEYWORDS: ........................................... 8 Digital Sound Recording................................... 9 CULTURAL CONTEXT ..............................................8 Digital Storage ................................................. 9 CULTURAL RESOURCE MANAGEMENT ..................8 Drawing.......................................................... 10 Cultural Tourism ...............................................8 Historic Documentation ................................. 10 Community Involvement ...................................8 Laser Scanning -
Controls of Basement Fabric on Rift Coupling And
1 2 3 4 5 This manuscript is currently undergoing peer-review. Please note that the manuscript is yet to be 6 formally accepted for publication. Subsequent versions of this manuscript may have slightly 7 different content. If accepted, the final version of this manuscript will be available via the ‘Peer- 8 reviewed Publication DOI’ link on the right-hand side of this webpage. Please feel free to contact 9 any of the authors. We look forward to your feedback. 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 1 30 CONTROLS OF BASEMENT FABRIC ON RIFT COUPLING AND DEVELOPMENT 31 OF NORMAL FAULT GEOMETRIES: INSIGHTS FROM THE RUKWA – NORTH 32 MALAWI RIFT 33 34 35 36 37 38 Erin Heilman1 39 Folarin Kolawole2 40 Estella A. Atekwana3* 41 Micah Mayle1 42 Mohamed G. Abdelsalam1 43 44 45 46 1Boone Pickens School of Geology 47 Oklahoma State University 48 Stillwater, Oklahoma, USA 49 50 2ConocoPhillips School of Geology & Geophysics 51 University of Oklahoma 52 Norman, Oklahoma, USA 53 54 3Department of Geological Sciences 55 College of Earth, Ocean, and Environment 56 University of Delaware 57 Newark, Delaware, USA 58 59 *Corresponding author email: [email protected] 60 61 62 63 64 65 66 67 68 69 70 71 72 August 2018 2 73 Highlights 74 • To the SW, newfound strike-slip fault links the Rukwa and North Malawi Rift (RNMRS) 75 • To the NE, RNMRS border faults, intervening faults and volcanic centers are colinear 76 • RNMRS border faults and transfer structures align with pre-existing basement fabrics 77 • Basement fabrics guide the development of normal fault geometries and rift bifurcation 78 • Basement fabrics facilitate the coupling of the RMRS border faults and transfer structures 79 80 81 ABSTRACT 82 The Rukwa Rift and North Malawi Rift Segments (RNMRS) both define a major rift-oblique 83 segment of the East African Rift System (EARS), and although the two young rifts show colinear 84 approaching geometries, they are often regarded as discrete rifts due to the presence of the 85 intervening Mbozi Block uplift located in-between. -
ED463609.Pdf
DOCUMENT RESUME ED 463 609 EC 308 901 AUTHOR Calhoun, Mary C.; Goldstein, Jeren; Walford, Sylvia B.; Purdum, Betsy TITLE World Geography: Skills and Regions. Teacher's Guide (and Student Guides]. Parallel Alternative Strategies for Students (PASS). INSTITUTION Leon County Schools, Tallahassee, FL. Exceptional Student Education.; Florida State Dept. of Education, Tallahassee. Bureau of Instructional Support and Community Services. REPORT NO ESE-9362.A; ESE-9362.B; ESE-9362.0 PUB DATE 2001-00-00 NOTE 788p.; Course no. 2103300. Teacher's Guide reprinted 2001; Student Guide--Skills reprinted 1998; Student Guide--Regions reprinted 1999. Part of the Curriculum Improvement Project funded under the Individuals with Disabilities Education Act (IDEA), Part B. AVAILABLE FROM Florida State Dept. of Education, Div. of Public Schools and Community Education, Bureau of Instructional Support and Community Services, Turlington Bldg., Room 628, 325 West Gaines St., Tallahassee, FL 32399-0400 (Teacher's guide, $5; Student guide--Skills, $4.30; Student guide--Regions, $11.15) .Tel: 800-487-0186 (Toll Free); Tel: 850-487-0186; Fax: 850-487-2679; e-mail: [email protected]; Web site: http://www.leon.k12.fl.us/public/pass ($5). PUB TYPE Guides Classroom Learner (051) Guides Classroom Teacher (052) EDRS PRICE MF05/PC32 Plus Postage. DESCRIPTORS *Academic Accommodations (Disabilities); Academic Standards; *Mild Disabilities; Secondary Education; Special Needs Students; State Standards; Student Educational Objectives; *Units of Study; *World Geography IDENTIFIERS *Florida ABSTRACT This teacher's guide and student guides on world geography skills and regions are part of a series of supplementary curriculum packages of alternative methods and activities designed to meet the needs of Florida secondary students with mild disabilities or other special learning needs. -
82796749.Pdf
Journal of African Earth Sciences 86 (2013) 65–106 Contents lists available at SciVerse ScienceDirect Journal of African Earth Sciences journal homepage: www.elsevier.com/locate/jafrearsci Invited Review Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution ⇑ H. Fritz a, , M. Abdelsalam b, K.A. Ali c, B. Bingen d, A.S. Collins e, A.R. Fowler f, W. Ghebreab g, C.A. Hauzenberger a, P.R. Johnson h, T.M. Kusky i, P. Macey j, S. Muhongo k,n, R.J. Stern l, G. Viola d,m a Department of Earth Sciences, University of Graz, 8010 Graz, Heinrichstrasse 26, Austria b Boone Pickens School of Geology, Oklahoma State University, Noble Research Center, Stillwater, OK 74078, USA c Faculty of Earth Sciences King Abdulaziz University, Jeddah 21589, Saudi Arabia d Geological Survey of Norway, Trondheim, Norway e Tectonics Resources and Exploration (TRaX), Geology and Geophysics, School of Earth andEnvironmental Sciences, The University of Adelaide, SA 5005, Australia f Geology Department, Faculty of Sciences, United Arab Emirates University, P.O Box 17551, Al-Ain, Abu Dhabi, United Arab Emirates g University of Asmara, Department of Earth Sciences, P.O. Box 1220, Asmara, Eritrea h 6016 SW Haines Street, Portland, OR 97219, USA i Three Gorges Research Center for Geohazards, State Key Laboratory of GeologicalProcesses and Mineral Resources, China University of Geosciences, Wuhan, China j Council for Geoscience (CGS), 280 Pretoria Street, Silverton, South Africa k Ministry of Energy and Minerals, 754/33 Samora Avenue, Dar Es Salaam,Tanzania l Geosciences Department, University of Texas at Dallas, Richardson, TX, USA m Norwegian University of Science and Technology, Trondheim, Norway n University of Dar Es Salaam, Department of Geology, P.O.Box 35052, Dar Es Salaam, Tanzania article info abstract Article history: The East African Orogen, extending from southern Israel, Sinai and Jordan in the north to Mozambique and Received 8 May 2012 Madagascar in the south, is the world´ s largest Neoproterozoic to Cambrian orogenic complex. -
Name P 2015 Urbclas Pchclas Denclas Trajectories Abakanskiy
Name P_2015 UrbClas PChClas DenClas Trajectories Abakanskiy Khrebet 51773 5 5 4 554 Absaroka Range 6388 6 1 4 614 Adamawa 4179507 1 2 3 123 Agri Dagi 3253 6 4 4 644 Ailao Shan 2301549 2 2 3 223 Air Mountains 26224 6 4 4 644 Al Hajar Mountains 678829 1 4 4 144 Ala Dag 32153 1 4 3 143 Ala Daglari 38850 6 5 4 654 Alayskiy Khrebet 1057504 1 2 3 123 Albertine Rift Mountains 23647008 1 3 1 131 Alborz Mountains 6080078 1 4 3 143 Ali Shan 50841 6 1 4 614 Allahu Ekber Daglari 39589 6 1 4 614 Altai Mountains 357455 2 5 4 254 Altiplano 1251606 1 3 4 134 Altiplano de Mexico 1375858 1 2 4 124 Anaconda Range 8876 5 2 4 524 Anamas Dagi 42345 6 5 4 654 Andringitra Mountains 766654 6 4 4 644 Ankaratra Mountains 1884601 2 2 3 223 Anti-Atlas Range 661787 6 1 4 614 Anyemaqen Shan 1411185 2 3 4 234 Apennines 3717875 3 5 3 353 Appalachian Mountains 3473059 3 2 4 324 Arakan Yoma 461372 5 4 4 544 Aravali Range 952817 1 3 2 132 Asahi dake 19519 6 1 4 614 Asir Mountains 2911684 1 4 3 143 Aur Mountains 1525474 1 3 2 132 Aydin Daglari 74300 6 4 4 644 Babatag Khrebet 249446 1 3 3 133 Balaban Daglari 61248 2 5 3 253 Balkan Mountains 722117 2 5 3 253 Bangma Shan 1410357 2 1 3 213 Banyan Har Shan 575241 6 3 4 634 Barguzinskiy Khrebet 11119 5 1 4 514 Barisan Mountains 6451484 2 2 3 223 Bashchelakskiy Khrebet 32948 6 1 4 614 Big Plateau 1562821 1 4 3 143 Binboga Daglari 67262 4 2 4 424 Bingel Daglari 28499 4 1 4 414 Bismarck Range 781320 1 4 3 143 Bitterroot Range 120001 6 1 4 614 Black Forest 524102 2 1 2 212 Blue Mountains 46614 5 2 4 524 Blue Mountains (Congo) 65295 -
Mountains and Climate Change from Understanding to Action © 2012 3Rd Edition First Edition 2009 Second Edition 2010
Mountains and Climate Change From Understanding to Action © 2012 3rd edition First edition 2009 Second edition 2010 Published by the Centre for Development and Environment (CDE), Institute of Geography, University of Bern, with the support of the Swiss Agency for Development and Cooperation (SDC) Copyright: Geographica Bernensia and SDC 2010 Editors: Thomas Kohler (CDE), Daniel Maselli (SDC) Concept: Daniel Maselli (SDC), Thomas Kohler (CDE) Design and Layout: Simone Kummer (CDE) Proofreading: Theodore Wachs (CDE) Cartography / Statistics: Ursula Gaemperli Krauer, Jürg Krauer, Sylvia Loercher (CDE) Alex Hermann (Institute of Geography, University of Bern) Citation: Kohler T. and Maselli D. (eds) 2009. Mountains and Climate Change - From Understanding to Action. Published by Geographica Bernensia with the support of the Swiss Agency for Development and Cooperation (SDC), and an international team of contributors. Bern. This publication is available from: Mountain Partnership Secretariat – FAO Viale delle Terme di Caracalla 00153 Rome - Italy www.mountainpartnership.org Swiss Agency for Development and Cooperation (SDC) CH-3003 Bern, Switzerland www.deza.admin.ch Centre for Development and Environment (CDE) University of Bern CH-3012 Bern, Switzerland www.cde.unibe.ch Cover photo: Daniel Maselli ISBN: 978-3-905835-16-8 Contents Foreword 3 1 Climate Change in Mountains 5 2 Mountain Waters 11 Key Issues, and Case Studies from the European Alps, Andes, and Rocky Mountains 3 Mountain Glaciers 21 Key Issues, and Case Studies from Peru, New Zealand, -
Landforms and Landscapes
Britannica LaunchPacks | Landforms and Landscapes Landforms and Landscapes For Years 6-8 This Pack contains: 17 ARTICLES 16 IMAGES 7 VIDEOS 1 WEBSITE © 2020 Encyclopædia Britannica, Inc. 1 of 91 Britannica LaunchPacks | Landforms and Landscapes Antarctica The icy continent surrounding the South Pole is called Antarctica. Its name means “opposite to the Arctic,” referring to the region around the North Pole. Antarctica is the fifth in size among the continents, larger than Europe and Australia. It is a cold and forbidding land that has no permanent human population and is almost devoid of animal or plant life. However, the ocean surrounding Antarctica teems with life. A map of Antarctica highlights the major geographic regions, ice sheets, and research stations (with … Encyclopædia Britannica, Inc. Gentoo penguins live in Antarctica. Paul Souders—Stone/Getty Images © 2020 Encyclopædia Britannica, Inc. 2 of 91 Britannica LaunchPacks | Landforms and Landscapes Researchers study the Ross Ice Shelf at the Bay of Whales, Antarctica. Michael Van Woert/NOAA NESDIS, ORA Ice and stormy seas kept anyone from seeing Antarctica until about 1820. In 1950 more than half the continent still had not been seen. Now airplanes and tractors have taken people to most parts of Antarctica, and satellite photographs have revealed the rest. But Antarctica remains a frontier, and much is yet to be learned about it. Almost no one goes to Antarctica except scientists and some adventurous tourists. The continent has natural resources that someday may be used, but the harsh environment of the area makes them difficult to exploit. Countries interested in Antarctica have signed a treaty that reserves the region for science and other peaceful purposes. -
Crustal and Sub-Continental Lithospheric Mantle Decoupling Beneath the Malawi Rift
CRUSTAL AND SUB-CONTINENTAL LITHOSPHERIC MANTLE DECOUPLING BENEATH THE MALAWI RIFT By EMMANUEL ATEM NJINJU Bachelor of Science in Geology University of Buea Buea, Cameroon 2012 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE May, 2016 CRUSTAL AND SUB-CONTINENTAL LITHOSPHERIC MANTLE DECOUPLING BENEATH THE MALAWI RIFT Thesis Approved: Dr. Estella A. Atekwana Thesis Adviser Dr. Mohamed G. Abdelsalam Dr. Daniel A. Laó-Dávila ii ACKNOWLEDGEMENTS I would like to express my sincere gratitude to my advisor Dr. Estella A. Atekwana for her supervision, encouragement and coaching. Without her help, this work would not have been possible. Many thanks are due to my committee members, Dr. Mohamed G. Abdelsalam and Dr. Daniel A. Laó-Dávila for their recommendations in improving my thesis. Special thanks go to Dr. Eliot A. Atekwana for his major inputs and contributions to my project. This project is funded by the National Science Foundation – Continental Dynamics grant # EAR 1255233 “Integrated Studies of Continental Rifting: From Nascent Extension (Okavango Rift Zone) to Continental Breakup (Afar Depression)”. I would like to thank Oklahoma State University and the Boone Pickens School of Geology for the excellent quality of education they offered me. I am also grateful for the scholarships awarded to me. These include the RE and KR McPhail Geology Scholarship. Luel Emishaw, Kitso Matende, Andrew Katumwehe, and Tadesse Alemu, helped me tremendously during this study. Thanks also go to Dr. Kennedy Fozoa in the University of Buea, for acting as my source of inspiration.