PDF (Volume 2)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Geochemistry and Petrogenesis of the Paleoproterozoic Du Chef Dyke Swarm, Québec, Canada
This is an Open Access document downloaded from ORCA, Cardiff University's institutional repository: http://orca.cf.ac.uk/60323/ This is the author’s version of a work that was submitted to / accepted for publication. Citation for final published version: Ciborowski, Thomas, Kerr, Andrew Craig, McDonald, Iain, Ernst, Richard E., Hughes, Hannah S. R. and Minifie, Matthew John 2014. The geochemistry and petrogenesis of the Paleoproterozoic du Chef dyke swarm, Québec, Canada. Precambrian Research 250 , pp. 151-166. 10.1016/j.precamres.2014.05.008 file Publishers page: http://dx.doi.org/10.1016/j.precamres.2014.05.008 <http://dx.doi.org/10.1016/j.precamres.2014.05.008> Please note: Changes made as a result of publishing processes such as copy-editing, formatting and page numbers may not be reflected in this version. For the definitive version of this publication, please refer to the published source. You are advised to consult the publisher’s version if you wish to cite this paper. This version is being made available in accordance with publisher policies. See http://orca.cf.ac.uk/policies.html for usage policies. Copyright and moral rights for publications made available in ORCA are retained by the copyright holders. The geochemistry and petrogenesis of the Paleoproterozoic du Chef dyke swarm, Québec, Canada T. Jake. R. Ciborowski*1, Andrew C. Kerr1, Iain McDonald1, Richard E. Ernst2, Hannah S. R. Hughes1, and Matthew J. Minifie1. 1School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff, Wales, CF10 3AT, UK 2Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, K1S 5B6, Canada & Ernst Geosciences, 43 Margrave Ave. -
History of Radiation and Nuclear Disasters in the Former USSR
History of radiation and nuclear disasters in the former USSR M.V.Malko Institute of Power Engineering National Academy of Sciences of Belarus Akademicheskaya Str.15, Minsk, 220 000, Republic of Belarus E-mail: [email protected] Abstracts. The report describes the history of radiation and nuclear accidents in the former USSR. These accidents accompanied development of military and civilian use of nuclear energy. Some of them as testing of the first Soviet nuclear, Kyshtym radiation accident, radiation contamination of the Karachai lake and the Techa river, nuclear accidents at the Soviet submarine on August 10, 1985 in the Chazhma Bay (near Vladivostok) as well as nuclear accidents on April 26, 1986 at the Chernobyl NPP were of large scale causing significant radiological problems for many hundreds thousands of people. There were a number of important reasons of these and other accidents. The most important among them were time pressure by development of nuclear weapon, an absence of required financial and material means for adequate management of problems of nuclear and radiation safety, and inadequate understanding of harmful interaction of ionizing radiation on organism as well as a hypersecrecy by realization of projects of military and civilian use of nuclear energy in the former USSR. Introduction. The first nuclear reactor in the USSR reached the critical state on the 25 December 1946 [1] or 4 years later than reactor constructed by Enrico Fermi [2]. The first Soviet reactor was developed at the Laboratory N2 in Moscow (later I.V.Kurchatov Institute of Atomic Energy). This was a very important step in a realization of the Soviet military atomic program that began in September 1942. -
The Picking Table Volume 50, No. 2 – Fall 2009
2009FallPT:Layout 1 8/27/2009 10:21 AM Page 1 JOURNAL OF THE FRANKLIN-OGDENSBURG MINERALOGICAL SOCIETY Volume 50, No. 2 – Fall 2009 $20.00 U.S. SPECIAL EDITION TH 50 ANNIVERSARY The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. 2009FallPT:Layout 1 8/27/2009 10:21 AM Page 2 The Franklin-Ogdensburg Mineralogical Society, Inc. OFFICERS and STAFF 2009 PRESIDENT SLIDE COLLECTION CUSTODIAN Bill Truran Edward H. Wilk 2 Little Tarn Court, Hamburg, NJ 07419 202 Boiling Springs Avenue (973) 827-7804 E. Rutherford, NJ 07073 [email protected] (201) 438-8471 VICE-PRESIDENT TRUSTEES Richard Keller C. Richard Bieling (2009-2010) 13 Green Street, Franklin, NJ 07416 Richard C. Bostwick (2009-2010) (973) 209-4178 George Elling (2008-2009) [email protected] Steven M. Kuitems (2009-2010) Chester S. Lemanski, Jr. (2008-2009) SECOND VICE-PRESIDENT Lee Lowell (2008-2009) Joe Kaiser Earl Verbeek (2008-2009) 40 Castlewood Trail, Sparta, NJ 07871 Edward H. Wilk (2008-2009) (973) 729-0215 Fred Young (2008-2009) [email protected] LIAISON WITH THE EASTERN FEDERATION SECRETARY OF MINERALOGICAL AND LAPIDARY Tema J. Hecht SOCIETIES (EFMLS) 600 West 111TH Street, Apt. 11B Delegate Joe Kaiser New York, NY 10025 Alternate Richard C. Bostwick (212) 749-5817 (Home) (917) 903-4687 (Cell) COMMITTEE CHAIRPERSONS [email protected] Auditing William J. Trost Field Trip Warren Cummings TREASURER Historical John L. Baum Denise Kroth Mineral Exchange Richard C. Bostwick 240 Union Avenue Nominating William Kroth Wood-Ridge, NJ 07075 Program Fred Young (201) 933-3029 Swap & Sell Chester S. -
The Mineral Indutry of Russia in 1998
THE MINERAL INDUSTRY OF RUSSIA By Richard M. Levine Russia extends over more than 75% of the territory of the According to the Minister of Natural Resources, Russia will former Soviet Union (FSU) and accordingly possesses a large not begin to replenish diminishing reserves until the period from percentage of the FSU’s mineral resources. Russia was a major 2003 to 2005, at the earliest. Although some positive trends mineral producer, accounting for a large percentage of the were appearing during the 1996-97 period, the financial crisis in FSU’s production of a range of mineral products, including 1998 set the geological sector back several years as the minimal aluminum, bauxite, cobalt, coal, diamonds, mica, natural gas, funding that had been available for exploration decreased nickel, oil, platinum-group metals, tin, and a host of other further. In 1998, 74% of all geologic prospecting was for oil metals, industrial minerals, and mineral fuels. Still, Russia was and gas (Interfax Mining and Metals Report, 1999n; Novikov significantly import-dependent on a number of mineral products, and Yastrzhembskiy, 1999). including alumina, bauxite, chromite, manganese, and titanium Lack of funding caused a deterioration of capital stock at and zirconium ores. The most significant regions of the country mining enterprises. At the majority of mining enterprises, there for metal mining were East Siberia (cobalt, copper, lead, nickel, was a sharp decrease in production indicators. As a result, in the columbium, platinum-group metals, tungsten, and zinc), the last 7 years more than 20 million metric tons (Mt) of capacity Kola Peninsula (cobalt, copper, nickel, columbium, rare-earth has been decommissioned at iron ore mining enterprises. -
70-26,250 University Microfilms, a XEROX Company, Ann Arbor
70-26,250 BICKEL, Edwin David, 1941- PLEISTOCENE NON-MARINE MOLLUSCA OF THE GATINEAU VALLEY AND OTTAWA AREAS OF QUEBEC AND ONTARIO, CANADA. The Ohio State University, Ph.D., 1970 Geology University Microfilms, A XEROX Company, Ann Arbor, Michigan PLEISTOCENE NON-KARINE NCLLUSCA OF THE GATINEAU VALLEY AND OTTAWA AREAS OF QUEBEC AND ONTARIO, CANADA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy In the Graduate School of The Ohio State University By Edwin David Bickel, A.B., M.Sc* * * * * * The Ohio State University 1970 Approved by r I' N J U u Adviser // Department of Geology ACKNOWLEDGMENTS I am most appreciative of the valuable guidance and assistance Professor Aurele La Rocque has given to this work and my other academic endeavors at The Ohio State University. Ky wife, Barbara Sue, deserves special recognition for many hours of skillful help in the field and laboratory. I wish to thank John G. Fyles and R, J. Kott of the Geological Survey of Canada, who generously made available samples and data gathered in conjunction with Dr. Mott*s research. Figure 3 from Geological Survey Memoir 2 M is reproduced as Fig. 2 of this paper by permission of the Geological Survey of Canada, Financial assistance for field work was provided by National Science Foundation Grant GB-818. I am grateful to the Friends of Orton Hall Fund for helping defray the cost of reproducing the illustrations. Finally, I wish to dedicate this dissertation to four teachers who have inspired and directed my scientific training. Professors Daniel F. -
B Clifford Frondel
CATALOGUE OF. MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM -B CLIFFORD FRONDEL BU.LLETIN OF THEAMRICANMUSEUM' OF NA.TURAL HISTORY. VOLUME LXVII, 1935- -ARTIC-LE IX- NEW YORK Tebruary 26, 1935 4 2 <~~~~~~~~~~~~~7 - A~~~~~~~~~~~~~~~, 4~~~~~~~~~~~~~~~~~~~~~~~~~~~~~4 4 4 A .~~~~~~~~~~~~~~~~~~~~~~~~~~4- -> " -~~~~~~~~~4~~. v-~~~~~~~~~~~~~~~~~~t V-~ ~~~~~~~~~~~~~~~~ 'W. - /7~~~~~~~~~~~~~~~~~~~~~~~~~~7 7-r ~~~~~~~~~-A~~~~ ~ ~ ~ ~ ~ ~ ~ ~ ~ -'c~ ~ ~ ' -7L~ ~ ~ ~ ~ 7 54.9:07 (74.71) Article IX.-CATALOGUE OF MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM OF NATURAL HISTORY' BY CLIFFORD FRONDEL CONTENTS PAGE INTRODUCTION .................. 389 Definition.389 Literature.390 New Pseudomorphse .393 METHOD OF DESCRIPTION.393 ORIGIN OF SUBSTITUTION AND INCRUSTATION PSEUDOMORPHS.396 Colloidal Origin: Adsorption and Peptization.396 Conditions Controlling Peptization.401 Volume Relations.403 DESCRIPTION OF SPECIMENS.403 INTRODUCTION DEFINITION.-A pseudomorph is defined as a mineral which has the outward form proper to another species of mineral whose place it has taken through the action of some agency.2 This precise use of the term excludes the regular cavities left by the removal of a crystal from its matrix (molds), since these are voids and not solids,3 and would also exclude those cases in which organic material has been replaced by quartz or some other mineral because the original substance is here not a mineral. The general usage of the term is to include as pseudomorphs both petrifactions and molds, and also: (1) Any mineral change in which the outlines of the original mineral are preserved, whether this surface be a euhedral crystal form or the irregular bounding surface of an embedded grain or of an aggregate. (2) Any mineral change which has been accomplished without change of volume, as evidenced by the undistorted preservation of an original texture or structure, whether this be the equal volume replacement of a single crystal or of a rock mass on a geologic scale. -
Use of Local Minerals in the Treatment of Radioactive Waste
O = 0(0H) •=Si(AI) O = 0(0H) # = AI, Mg, Fe, etc. TECHNICAL REPORTS SERIES No. 136 Use of Local Minerals in the Treatment of Radioactive Waste INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1972 USE OF LOCAL MINERALS IN THE TREATMENT OF RADIOACTIVE WASTE The following States are Members of the International Atomic Energy Agency: AFGHANISTAN GUATEMALA PAKISTAN ALBANIA HAITI PANAMA ALGERIA HOLY SEE PARAGUAY ARGENTINA HUNGARY PERU AUSTRALIA ICELAND PHILIPPINES AUSTRIA INDIA POLAND BELGIUM INDONESIA PORTUGAL BOLIVIA IRAN ROMANIA BRAZIL IRAQ SAUDI ARABIA BULGARIA IRELAND SENEGAL BURMA ISRAEL SIERRA LEONE BYELORUSSIAN SOVIET ITALY SINGAPORE SOCIALIST REPUBLIC IVORY COAST SOUTH AFRICA CAMEROON JAMAICA SPAIN CANADA JAPAN SUDAN CEYLON JORDAN SWEDEN CHILE KENYA SWITZERLAND CHINA KHMER REPUBLIC SYRIAN ARAB REPUBLIC COLOMBIA KOREA, REPUBLIC OF THAILAND COSTA RICA KUWAIT TUNISIA CUBA LEBANON TURKEY CYPRUS LIBERIA UGANDA CZECHOSLOVAK SOCIALIST LIBYAN ARAB REPUBLIC UKRAINIAN SOVIET SOCIALIST REPUBLIC LIECHTENSTEIN REPUBLIC DENMARK LUXEMBOURG UNION OF SOVIET SOCIALIST DOMINICAN REPUBLIC MADAGASCAR REPUBLICS ECUADOR MALAYSIA UNITED KINGDOM OF GREAT EGYPT, ARAB REPUBLIC OF MALI BRITAIN AND NORTHERN EL SALVADOR MEXICO IRELAND ETHIOPIA MONACO UNITED STATES OF AMERICA FINLAND MOROCCO URUGUAY FRANCE NETHERLANDS VENEZUELA GABON NEW ZEALAND VIET-NAM GERMANY, FEDERAL REPUBLIC OF NIGER YUGOSLAVIA GHANA NIGERIA ZAIRE, REPUBLIC OF GREECE NORWAY ZAMBIA The Agency's Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957, The Headquarters of the Agency are situated in Vienna. Its principal objective is "to accelerate and enlarge the contribution of atomic energy to peace, health and prosperity throughout the world". -
Rosatom: Continuous Nuclear Contamination of the Area Around the Mayak Complex
Greenpeace Justice for Section International People and Planet Case Studies Rosatom: Continuous nuclear contamination of the area around the Mayak complex Russian nuclear corporation Rosatom has been Company activity responsible for a series of nuclear accidents at its Nuclear power and power engineering assets, as well Mayak complex, and victims have been unable to as nuclear power plant (NPP) and facilities of full nuclear secure either justice or remedy in part due to the fuel cycle design and construction.5 Rosatom is also impunity of the state-owned company in Russian responsible for part of the military nuclear activities of courts. Russia, including in Mayak. The company has a range of other businesses, including power generation in its Problem Analysis existing nuclear plants; it has a renewable division with increasing investments in wind; and it has uranium mining The Kyshtym nuclear disaster, caused by the Mayak and nuclear weapon development, amongst others. nuclear complex, was the third worst nuclear disaster in history. Despite this the Mayak nuclear complex, whose Country and location in which core business is reprocessing spent nuclear fuel, remains in the violation occurred operation. Local residents are affected both by the historical contamination and by the emissions from current activities. Ozyorsk, Chelyabinsk Oblast, the Southern Urals region, Today Mayak is run by Rosatom, Russia’s state nuclear Russia corporation. This case illustrates how the Russian state and its flagship company work closely together to continue their Summary of the case operations, despite the negative impacts on both public Rosatom’s Mayak Combine is part of the Russian state health and the environment. -
Karachay Lake Is the Storage of the Radioactive Wastes Under Open Sky
KARACHAY LAKE IS THE STORAGE OF THE RADIOACTIVE WASTES UNDER OPEN SKY Alexey O. Merkushkin Ozyorsk Technological Institute of Moscow Physical Engineering Institute, Russia e-mail: [email protected] [email protected] [email protected] ABSTRACT Lake Karachay is situated at "Mayak" PA site. From October 1951 the lake was used as a storage of technological radioactive waste to stop the waste discharge into the Teclia River. At present time the reservoir contains about 120 min Ci of radionuclides. Lake Karachay presents a serious ecological problem being source of the contamination of the air, grounds and underground water. In this work a review of available sources dealing with Karachay's problem is made. Present and past approaches to this problem are shown. INTRODUCTION parting area of Lakes Ulagach. Tatysh, Malaya Nanoga, Kyzyltash, and sources of the Mishelyak and Techa River Production association “Mayak” is situated in the north (Fig. 2). Since October 1951, PA “Mayak” began to use part of Chelyabinsk region, near towns Kyshtym and Kasli Lake Karachay for the storage of radioactive wastes, in (Fig. 1). “Mayak” was founded at the end of 40-s to produce order to stop the waste discharge into the Techa River. plutonium and convert the nuclear materials for creating the This step was made because there were not enough parity in the field of the nuclear weapons. Activity of PA containers for storage of big amounts of the radioactive “Mayak” (before 60-s) was a source of radioactive wastes. Today Karachay is used for discharge of liquid contamination of the Ural region and, in the first place, of the middle radioactive wastes from radiochemical and northen part of Chelyabinsk region Imperfection of nuclear radioisotope productions of PA “Mayak”. -
Guide to Investment Chelyabinsk Region Pwc Russia ( Provides Industry-Focused Assurance, Advisory, Tax and Legal Services
Guide to Investment Chelyabinsk Region PwC Russia (www.pwc.ru) provides industry-focused assurance, advisory, tax and legal services. Over 2,500 professionals working in PwC offices in Moscow, St Petersburg, Ekaterinburg, Kazan, Novosibirsk, Krasnodar, Yuzhno-Sakhalinsk and Vladikavkaz share their thinking, experience and solutions to develop fresh perspectives and practical advice for our clients. Global PwC network includes over 169,000 employees in 158 countries. PwC first appeared in Russia in 1913 and re-established its presence here in 1989. Since then, PwC has been a leader in providing professional services in Russia. According to the annual rating published in Expert magazine, PwC is the largest audit and consulting firm in Russia (see Expert, 2000-2011). This overview has been prepared in conjunction with and based on the materials provided by the Ministry of Economic Development of Chelyabinsk Region. This publication has been prepared for general guidance on matters of interest only, and does not constitute professional advice. You should not act upon the information contained in this publication without obtaining specific professional advice. No representation or warranty (express or implied) is given as to the accuracy or completeness of the information contained in this publication, and, to the extent permitted by law, PwC network, its members, employees and agents accept no liability, and disclaim all responsibility, for the consequences of you or anyone else acting, or refraining to act, in reliance on the information -
ZINCIAN AEGIRINE-AUGITE and JEFFERSONITE from FRANKLIN, NEW JERSEY Cr.Rrnonofnonnbr Enn Jux Ho, Departmentof Geolog,Icalsciences, H Arsaril [] Niaer Sity Cambrid
THE AMERICAN MINERALOGIST, VOL 51, SEPTEMBER_OCTOBER, 1966 ZINCIAN AEGIRINE-AUGITE AND JEFFERSONITE FROM FRANKLIN, NEW JERSEY Cr.rrnonoFnoNnBr eNn Jux ho, Departmentof Geolog,icalSciences, H arsaril [] niaer sity Cambrid. ge, M as s a chu s e tt s.r Agsrnect A coarsely crystallized dark colored monoclinic pyroxene found abundantly in skarn zones at Franklin and Sterling Hill, New Jersey, has long been known under the name jefiersonite. It has been classed as a diopsidic pyroxene, but four new chemical analyses (with accompanying r-ray and optical data) establish that it comprises highly zincian and manganoan members of a series from aegirine-augite to sodian and ferrian augite. Both Mn2+ and Zn are much in excess of Fe2f, with almost 40 atomic per cent Mn in the B position in one analysis. As Fea+and Na decrease the color changes from reddish brown and mahogany brown to dark olive green and greenish black. The original jefiersonite of Vanuxem and Keating (1822) probably referred to the latter material; the name lacks species or varietal significance and may be set aside. INtnooucuoN Three different types of pyroxene have been found in the so-called skarn zones in the orebodiesat Franklin and Sterling Hill, New Jersey. The most common type is a manganoan and sometimes also zincian variety of diopside. It generally contains NInO in the range from 4 to 10 weight per cent (Table 1, anal. 1 to 5). If little or Lo Zn is present,this material has been called schefierite,following the varietal name originally proposedby Michaelson(1863) for manganoandiopside of similar com- position from Langban, Sweden. -
Analyses of Rocks and Minerals
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director / rf Bulletin 878 ANALYSES OF ROCKS AND MINERALS FROM THE LABORATORY OF THE UNITED STATES GEOLOGICAL SURVEY 1914-36 TABULATED BY ROGER C. WELLS Chief Chemist UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1937 For sale by the Superintendent of Documents, Washington, D. C. ------ Price 15 cents V CONTENTS Page Introduction._____________________________________________________ 1 The elements and their relative abundance.__________________________ 3 Abbreviations used._______________________________________________ 5 Classification.___________________________________________________ 5 Analyses of igneous and crystalline rocks____-_________.._____________ 6 Alaska._____-_____-__________---_-_--___-____-_____-_________ 6 \ Central Alaska________________________________________ 6 Southeastern Alaska___________-_--________________________ 7 Arizona._________--____-_---_-------___-_--------_----_______ 8 Ajo district.-_--_.____---------______--_-_--__---_______ 8 Oatman district____________-___-_-________________________ 9 Miscellaneous rocks....-._...._-............_......_._.... 10 Arkansas.____________________________________________________ 11 Austria._____________________________________________________ 11 California.__,_______________--_-_----______-_-_-_-___________ 11 T ' Ivanpah quadrangle.____-_----__--_____----_--_--__.______ 11 Lassen Peak__________________ ___________________________ 12 Mount Whitney quadrangle________________________________