2016-2017 Research & Scholarship Report
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Religion and Politics in Post-Communist Romania RELIGION and GLOBAL POLITICS SERIES
Religion and Politics in Post-Communist Romania RELIGION AND GLOBAL POLITICS SERIES Series Editor John L. Esposito University Professor and Director Prince Alwaleed Bin Talal Center for Muslim-Christian Understanding Georgetown University Islamic Leviathan Islam and the Making of State Power Seyyed Vali Reza Nasr Rachid Ghannouchi A Democrat within Islamism Azzam S. Tamimi Balkan Idols Religion and Nationalism in Yugoslav States Vjekoslav Perica Islamic Political Identity in Turkey M. Hakan Yavuz Religion and Politics in Post-Communist Romania lavinia stan lucian turcescu 1 2007 3 Oxford University Press, Inc., publishes works that further Oxford University’s objective of excellence in research, scholarship, and education. Oxford New York Auckland Cape Town Dar es Salaam Hong Kong Karachi Kuala Lumpur Madrid Melbourne Mexico City Nairobi New Delhi Shanghai Taipei Toronto With offices in Argentina Austria Brazil Chile Czech Republic France Greece Guatemala Hungary Italy Japan Poland Portugal Singapore South Korea Switzerland Thailand Turkey Ukraine Vietnam Copyright # 2007 by Oxford University Press, Inc. Published by Oxford University Press, Inc. 198 Madison Avenue, New York, New York 10016 www.oup.com Oxford is a registered trademark of Oxford University Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior permission of Oxford University Press. Library of Congress Cataloging-in-Publication Data Stan, Lavinia. Religion and politics in post-communist Romania / Lavinia Stan, Lucian Turcescu. p. cm.—(Religion and global politics series) Includes bibliographical references and index. ISBN 978-0-19-530853-2 1. -
North America Free Download
NORTH AMERICA FREE DOWNLOAD Libby Koponen | 48 pages | 01 Mar 2009 | Children's Press(CT) | 9780531218303 | English | New York, NY, United States North America Plymouth remains the de jure capital. With soldiers in tow, his goal was to find gold for the Spanish Crown. United States of America Bureau of the Census. Nearly North America million immigrants have a four-year college degree or better. Retrieved 3 October This North America a list of North American countries and dependent territories by population. New Spain, a territory that stretched from the southwestern modern-day U. He explained the rationale for the name in the accompanying book Cosmographiae Introductio : [6]. This section needs expansion. Oceans portal Book Category. About ten years later another trading company, the West India Company, settled groups of colonists on Manhattan Island and at Fort Orange. North America has been historically referred to by other names. The first attempt by Europeans to colonize the New World occurred around A. Weishampel, David B. Demographics by North America. Other French-speaking locales include the Province of Ontario the official language is English, but there are an estimated North America, Franco-Ontariansthe Province of Manitoba co-official as de jure with Englishthe French West Indies and Saint-Pierre et Miquelonas well as North America US state of Louisiana, where French is also an official language. Canada shows significant growth in the sectors of services, mining and manufacturing. Inexplicably, Vineland was abandoned after only a few years. Between and Frobisher as well as John Davis explored along the Atlantic coast. Central Intelligence Agence. -
Carbon and Strontium Isotope Stratigraphy of the Permian from Nevada and China: Implications from an Icehouse to Greenhouse Transition
Carbon and strontium isotope stratigraphy of the Permian from Nevada and China: Implications from an icehouse to greenhouse transition Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Kate E. Tierney, M.S. Graduate Program in the School of Earth Sciences The Ohio State University 2010 Dissertation Committee: Matthew R. Saltzman, Advisor William I. Ausich Loren Babcock Stig M. Bergström Ola Ahlqvist Copyright by Kate Elizabeth Tierney 2010 Abstract The Permian is one of the most important intervals of earth history to help us understand the way our climate system works. It is an analog to modern climate because during this interval climate transitioned from an icehouse state (when glaciers existed extending to middle latitudes), to a greenhouse state (when there were no glaciers). This climatic amelioration occurred under conditions very similar to those that exist in modern times, including atmospheric CO2 levels and the presence of plants thriving in the terrestrial system. This analog to the modern system allows us to investigate the mechanisms that cause global warming. Scientist have learned that the distribution of carbon between the oceans, atmosphere and lithosphere plays a large role in determining climate and changes in this distribution can be studied by chemical proxies preserved in the rock record. There are two main ways to change the distribution of carbon between these reservoirs. Organic carbon can be buried or silicate minerals in the terrestrial realm can be weathered. These two mechanisms account for the long term changes in carbon concentrations in the atmosphere, particularly important to climate. -
Lavinia Stan
Lavinia Stan Departmental Address: Department of Political Science Phone: (902) 867-5084 St. Francis Xavier University Fax: (902) 867-3243 Antigonish, Nova Scotia, Canada Email: [email protected] ResearchGate: https://www.researchgate.net/profile/Lavinia_Stan Web of Science/Publons ResearcherID: A-1337-2008 Google Scholar: https://scholar.google.ca/citations?user=OZN8mWAAAAAJ&hl=en&oi=ao ORCID Identifier: https://orcid.org/00 EMPLOYMENT HISTORY Program Coordinator, Public Policy and Governance (PGOV), Brian Mulroney Institute of Government, St. Francis Xavier University, 2019-2020. Jules Leger Research Chair, St. Francis Xavier University, July 2018 – June 2020 Professor, Department of Political Science, St. Francis Xavier University, 2017 - present Chair, Department of Political Science, St. Francis Xavier University, May 2015 - May 2017 Associate Professor, Department of Political Science, St. Francis Xavier University, 2009 - 2017 Member, Centre canadien d'études allemandes et européennes, Universite de Montreal, 2014 - present Visiting Professor, Centre canadien d'études allemandes et européennes, Université de Montréal, 2013-14 Assistant Professor, Department of Political Science, StFX, January 2004-2009 Assistant Professor, Department of Political Science, Concordia University, 2006-2008 Killam Postdoctoral Fellow, Department of Political Science, Dalhousie University, 2001-2003 EDUCATION Ph. D., Political Science, University of Toronto, 2001 M.A., Political Science, University of Toronto, 1996 B.Com. (Honors Thesis), Academy of Economic -
2015 Conference Program
2015 International Conference Linking Past, Present and Future: The 25th Anniversary of Regime Change in Romania and Moldova (1989/1991) PROGRAM 17-19 iunie / 17-19 June 2015 Faculty of Political Science, University of Bucharest Co-organizers: The Society for Romanian Studies is an international interdisciplinary academic organization based in the United States of America and dedicated to promoting the professional study, criticism, and research of all aspects of Romanian culture and civilization, particularly concerning the countries of Romania and Moldova. Established in 1973 by a group of enthusiasts, the Society has become the premier Romanian Studies organization in the world, gathering scholars, students and government officials from a variety of countries. SRS Board: Lavinia Stan (President) James Koranyi (President Elect) Irina Livezeanu (Past President) Paul Michelson (Secretary) William Crowther (Treasurer) Roland Clark (Newsletter Editor) Emilian Ghelase (Webmaster) Margaret Beissinger (contact person with the Romanian Studies Association of America) Jennifer Cash Monica Ciobanu Jill Massino Bruce O’Neill Paul E. Sum Andrei Terian Roxana Cazan (student representative) Jonathan Stillo (student representative) Information on the Society is listed on its website, http://www.society4romanianstudies.org. The Society runs a number of programs and activities relevant for scholars, students, and governmental officials. Every year, it offers a prize for the best graduate student essay written in English on a Romanian Studies topic. The Society also awards a biennial prize for the best monograph published in English on a Romanian Studies theme, with an internationally recognized press. In partnership with Polirom, the Society also publishes a book collection. Its annual general meeting takes place every year in November in conjunction with the conference of the Association for Slavic, East European & Eurasian Studies (ASEEES). -
Justice, Memory and Redress in Romania
Justice, Memory and Redress in Romania Justice, Memory and Redress in Romania: New Insights Edited by Lavinia Stan and Lucian Turcescu Justice, Memory and Redress in Romania: New Insights Edited by Lavinia Stan and Lucian Turcescu This book first published 2017 Cambridge Scholars Publishing Lady Stephenson Library, Newcastle upon Tyne, NE6 2PA, UK British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library Copyright © 2017 by Lavinia Stan, Lucian Turcescu and contributors All rights for this book reserved. No part of this book may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the copyright owner. ISBN (10): 1-4438-3152-2 ISBN (13): 978-1-4438-3152-9 TABLE OF CONTENTS List of Illustrations .................................................................................... vii List of Tables ............................................................................................ viii Introduction ................................................................................................ ix Lavinia Stan Part 1. Memory, Reckoning, Legitimacy, and Justice: Theoretical Considerations Chapter One ................................................................................................. 2 Conceptions of Memory and Historical Redress Cristian Tileaga Chapter Two ............................................................................................. -
Illawarra Reversal: the fingerprint of a Superplume That Triggered Pangean Breakup and the End-Guadalupian (Permian) Mass Extinction
Gondwana Research 15 (2009) 421–432 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Illawarra Reversal: The fingerprint of a superplume that triggered Pangean breakup and the end-Guadalupian (Permian) mass extinction Yukio Isozaki Department of Earth Science and Astronomy, The University of Tokyo, Komaba, Meguro, Tokyo 153-8902, Japan article info abstract Article history: The Permian magnetostratigraphic record demonstrates that a remarkable change in geomagnetism occurred in Received 22 July 2008 the Late Guadalupian (Middle Permian; ca. 265 Ma) from the long-term stable Kiaman Reverse Superchron Received in revised form 10 December 2008 (throughout the Late Carboniferous and Early-Middle Permian) to the Permian–Triassic Mixed Superchron with Accepted 11 December 2008 frequent polarity changes (in the Late Permian and Triassic). This unique episode called the Illawarra Reversal Available online 24 December 2008 probably reflects a significant change in the geodynamo in the outer core of the planet after a 50 million years of Keywords: stable geomagnetism. The Illawarra Reversal was likely led by the appearance of a thermal instability at the – Illawarra Reversal 2900 km-deep core mantle boundary in connection with mantle superplume activity. The Illawarra Reversal Permian and the Guadalupian–Lopingian boundary event record the significant transition processes from the Paleozoic Superplume to Mesozoic–Modern world. One of the major global environmental changes in the Phanerozoic occurred Geodynamo almost simultaneously in the latest Guadalupian, as recorded in 1) mass extinction, 2) ocean redox change, 3) Mass extinction sharp isotopic excursions (C and Sr), 4) sea-level drop, and 5) plume-related volcanism. -
Read Book Continent Ebook Free Download
CONTINENT PDF, EPUB, EBOOK Jim Crace | 176 pages | 04 Jan 2008 | Pan MacMillan | 9780330453318 | English | London, United Kingdom Continent - Wikipedia Geologists theorize that continents move. This theory is called plate tectonics , which holds that the lithosphere , the outermost layer of Earth where continents are , lies on top of a semifluid layer of partially molten magma called the asthenosphere. Convection from the decay of radioactive elements in the mantle causes continental and oceanic plates to move. Pangea is a landmass of the Early Permian to Early Jurassic Periods that incorporated almost all modern landmasses and is thus considered a supercontinent. There is great variation in the sizes of continents; Asia is more than five times as large as Australia. The largest island in the world, Greenland , is only about one-fourth the size of Australia. The continents differ sharply in their degree of compactness. Africa has the most regular coastline and, consequently, the lowest ratio of coastline to total area. Europe is the most irregular and indented and has by far the highest ratio of coastline to total area. The continents are not distributed evenly over the surface of the globe. The distribution of the continental platforms and ocean basins on the surface of the globe and the distribution of the major landform features have long been among the most intriguing problems for scientific investigation and theorizing. Each continent has one of the so-called shield areas that formed 2 billion to 4 billion years ago and is the core of the continent to which the remainder most of the continent has been added. -
Red Rock Canyon Visitor Guide
RED ROCK CANYON A NATIONAL CONSERVATION AREA ADMINISTERED BY THE BUREAU OF LAND KEYSTONE MANAGEMENT VISITOR GUIDE Proudly presented by Southern Nevada Conservancy in partnership with the Bureau of Land Management. FIRST STOP- VISITOR CENTER Be sure to stop by the Red Rock Canyon Visitor Center before you start your day. The Scenic Drive will not return you to that area so you don’t want to miss it! The Visitor Center is an informational hub for visitors filled with indoor and outdoor exhibits, plant specimens from throughout the canyon, and a desert tortoise habitat. Check out the Information Desk for hike recommendations, participate in a program, and pick up something at the gift shop to remember your trip. WELCOME Welcome to one of America’s most beautiful landscapes! In addition to hikes and trails. Red Rock Canyon’s spectacular sandstone escarpment, fantastic scenery, Red Rock Canyon National Conservation Area offers the iconic desert tortoise, and the thickets of Joshua trees herald the some of the best hiking, rock climbing, biking, and outdoor recreation natural world of geology, animals, and plants to be experienced in the activities in the region. The 13-mile Scenic Drive offers several scenic over 200,000 acre National Conservation Area, managed by the Bureau overlooks, parking areas, picnic areas, and access to dozens of day of Land Management. If you are looking for more information, please stop by the visitor center to view exhibits, pick up informational handouts and talk with staff about how you can make your visit more special. Once you get home, take a peek at our website redrockcanyonlv.org or blm.gov/site-page/rrcnca GET READY TO SAFELY EXPLORE Search and rescue incidents are unfortunate but do occur in Red Rock National Conservation Area. -
EVOLUTION of the NORTH AMERICAN CORDILLERA William R. Dickinson
7 Apr 2004 20:19 AR AR211-EA32-02.tex AR211-EA32-02.sgm LaTeX2e(2002/01/18) P1: GCE 10.1146/annurev.earth.32.101802.120257 Annu. Rev. Earth Planet. Sci. 2004. 32:13–45 doi: 10.1146/annurev.earth.32.101802.120257 Copyright c 2004 by Annual Reviews. All rights reserved First published online as a Review in Advance on November 10, 2003 EVOLUTION OF THE NORTH AMERICAN CORDILLERA William R. Dickinson Department of Geosciences, University of Arizona, Tucson, Arizona 85721; email: [email protected] Key Words continental margin, crustal genesis, geologic history, orogen, tectonics ■ Abstract The Cordilleran orogen of western North America is a segment of the Circum-Pacific orogenic belt where subduction of oceanic lithosphere has been under- way along a great circle of the globe since breakup of the supercontinent Pangea began in Triassic time. Early stages of Cordilleran evolution involved Neoproterozoic rifting of the supercontinent Rodinia to trigger miogeoclinal sedimentation along a passive continental margin until Late Devonian time, and overthrusting of oceanic allochthons across the miogeoclinal belt from Late Devonian to Early Triassic time. Subsequent evolution of the Cordilleran arc-trench system was punctuated by tectonic accretion of intraoceanic island arcs that further expanded the Cordilleran continental margin during mid-Mesozoic time, and later produced a Cretaceous batholith belt along the Cordilleran trend. Cenozoic interaction with intra-Pacific seafloor spreading systems fostered transform faulting along the Cordilleran continental margin and promoted incipient rupture of continental crust within the adjacent continental block. INTRODUCTION Geologic analysis of the Cordilleran orogen, forming the western mountain system of North America, raises the following questions: 1. -
Lucian Turcescu Page 1 of 38 9 July 2020 Professor Dr. LUCIAN
Professor Dr. LUCIAN TURCESCU Mailing Address Tel: (514) 848-2424 ext. 2341 Department of Theological Studies E-mail: [email protected] Concordia University, S-D-201 http://www.concordia.ca/artsci/theology.html 1455 de Maisonneuve Blvd. W. Citizenship Montreal, QC H3G 1M8 Canada Canadian and Romanian (European Union) EMPLOYMENT HISTORY Full Professor, Historical Theology, Department of Theological Studies, Concordia University, since 1 June 2010. Graduate Program Director, Department of Theological Studies, Concordia University, Montreal, January 2007-May 2011, June 2016-March 2018. Chair, Department of Theological Studies, Concordia University, Montreal, June 1, 2011-May 31, 2016. Associate Professor (Re-tenured at Concordia on June 1, 2007), Historical Theology, Department of Theological Studies, Concordia University, July 2005-May 2010. Adjunct Professor, Faculté de théologie et de sciences des religions, Université de Montréal, Canada, 2008-2014. Chair, Department of Religious Studies, St. Francis Xavier University, Antigonish, Nova Scotia, Canada. May 2004-April 2005. Associate Professor (Tenured effective 1 September 2004), Department of Religious Studies, St. Francis Xavier University, Antigonish, NS, Canada. Sep. 2003-June 2005. Assistant Professor (tenure track), Department of Religious Studies and Catholic Studies Program, St. Francis Xavier University, Antigonish, NS. July 2000-Aug 2003. Assistant Professor, Catholic Studies Program, St. Francis Xavier University, Antigonish, NS, Canada. July 1999-June 2000. Adjunct Professor, Ignatius University (distance learning), Staten Island, NY, Spring 1999. Sessional Instructor, Continuing Education, University of St. Michael's College, Toronto, Fall 1998. Sessional Professor, St. Paul University, Ottawa, ON, Fall 1996. Research Assistant to Dr. Paul J. Fedwick's SSHRC-funded Bibliotheca Basiliana Vniversalis: A Study of the Manuscript Tradition of the Works of Basil of Caesarea. -
The Role of Megacontinents in the Supercontinent Cycle Chong Wang1,2, Ross N
https://doi.org/10.1130/G47988.1 Manuscript received 6 June 2020 Revised manuscript received 1 October 2020 Manuscript accepted 5 October 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 25 November 2020 The role of megacontinents in the supercontinent cycle Chong Wang1,2, Ross N. Mitchell1*, J. Brendan Murphy3, Peng Peng1 and Christopher J. Spencer4 1 State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2 Deparment of Geosciences and Geography, University of Helsinki, Helsinki 00014, Finland 3 Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia B2G 2W5, Canada 4 Department of Geological Sciences and Geological Engineering, Queen’s University, Kingston, Ontario K7L 2N8, Canada ABSTRACT Baltica (and subsequently outboard additions) Supercontinent Pangea was preceded by the formation of Gondwana, a “megacontinent” (Wan et al., 2019). Assembly of Eurasia started about half the size of Pangea. There is much debate, however, over what role the assembly with the central Asian orogenic belt that weld- of the precursor megacontinent played in the Pangean supercontinent cycle. Here we dem- ed Baltica and Siberia at ca. 250 Ma. This as- onstrate that the past three cycles of supercontinent amalgamation were each preceded by sembly overlaps with the tenure and breakup of ∼200 m.y. by the assembly of a megacontinent akin to Gondwana, and that the building of a Pangea and represents an early assembly phase megacontinent is a geodynamically important precursor to supercontinent amalgamation. of the proposed future supercontinent Amasia The recent assembly of Eurasia is considered as a fourth megacontinent associated with (Mitchell et al., 2012).