Cobalt Resources in Europe and the Potential for New Discoveries
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Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
2. Obszary O Niekorzystnych Warunkach Gospodarowania (Halina Klimczak)
Autorzy: Halina Klimczak – rozdziały I, II, VI; Halina Klimczak, Katarzyna Galant, Marta K=ciak – rozdział III; Halina Klimczak, Katarzyna Galant – rozdział IV; Ewa Krzywicka-Blum, Halina Klimczak, Andrzej Klimczak – rozdział V Opiniodawca prof. dr hab. Janusz Gołaski Redaktor merytoryczny dr hab. inb. Andrzej Borkowski Opracowanie redakcyjne dr Ewa Jaworska Korekta: mgr Elbbieta Winiarska-Grabosz, Janina Szydłowska Łamanie Teresa Alicja Chmura Projekt okładki Stanisław Rogowski Publikacja finansowana przez Ministerstwo Nauki i Szkolnictwa Wybszego Grant badawczy nr 4 T12E 021 28 Monografie LIII © Copyright by Uniwersytet Przyrodniczy we Wrocławiu, Wrocław 2008 ISBN 978-83-60574-25-6 WYDAWNICTWO UNIWERSYTETU PRZYRODNICZEGO WE WROCŁAWIU Redaktor Naczelny – prof. dr hab. Andrzej Kotecki ul. Sopocka 23, 50–344 Wrocław, tel. 071 328–12–77 e-mail: [email protected] Nakład 100 + 16 egz. Ark. druk. 9,75 Druk i oprawa: Wydawnictwo Tekst Sp. z o.o. ul. Kossaka 72, 85-307 Bydgoszcz SPIS TREUCI WstBp (Halina Klimczak) ..................................................................................................... 7 1. Charakterystyka warunków gospodarowania w województwie dolnoVl=skim (Halina Klimczak) ..................................................................................................... 9 1.1. Podział na regiony funkcjonalne i fizjograficzny ........................................................... 9 1.2. Warunki przyrodnicze i społeczne produkcji rolniczej ................................................ 11 1.2.1. Ukształtowanie -
New Siberian Islands Archipelago)
Detrital zircon ages and provenance of the Upper Paleozoic successions of Kotel’ny Island (New Siberian Islands archipelago) Victoria B. Ershova1,*, Andrei V. Prokopiev2, Andrei K. Khudoley1, Nikolay N. Sobolev3, and Eugeny O. Petrov3 1INSTITUTE OF EARTH SCIENCE, ST. PETERSBURG STATE UNIVERSITY, UNIVERSITETSKAYA NAB. 7/9, ST. PETERSBURG 199034, RUSSIA 2DIAMOND AND PRECIOUS METAL GEOLOGY INSTITUTE, SIBERIAN BRANCH, RUSSIAN ACADEMY OF SCIENCES, LENIN PROSPECT 39, YAKUTSK 677980, RUSSIA 3RUSSIAN GEOLOGICAL RESEARCH INSTITUTE (VSEGEI), SREDNIY PROSPECT 74, ST. PETERSBURG 199106, RUSSIA ABSTRACT Plate-tectonic models for the Paleozoic evolution of the Arctic are numerous and diverse. Our detrital zircon provenance study of Upper Paleozoic sandstones from Kotel’ny Island (New Siberian Island archipelago) provides new data on the provenance of clastic sediments and crustal affinity of the New Siberian Islands. Upper Devonian–Lower Carboniferous deposits yield detrital zircon populations that are consistent with the age of magmatic and metamorphic rocks within the Grenvillian-Sveconorwegian, Timanian, and Caledonian orogenic belts, but not with the Siberian craton. The Kolmogorov-Smirnov test reveals a strong similarity between detrital zircon populations within Devonian–Permian clastics of the New Siberian Islands, Wrangel Island (and possibly Chukotka), and the Severnaya Zemlya Archipelago. These results suggest that the New Siberian Islands, along with Wrangel Island and the Severnaya Zemlya Archipelago, were located along the northern margin of Laurentia-Baltica in the Late Devonian–Mississippian and possibly made up a single tectonic block. Detrital zircon populations from the Permian clastics record a dramatic shift to a Uralian provenance. The data and results presented here provide vital information to aid Paleozoic tectonic reconstructions of the Arctic region prior to opening of the Mesozoic oceanic basins. -
Covered Cinnabar Deposit of El the Polymetallic Pyritic Lenses at the Base of The
LEIDSE GEOLOGISCHE MEDEDELINGEN, Deel 52, 1-7-1981 Aflevering 1, pp. 23-56, Framework and evolution of Hercynian mineralization in the Iberian Meseta BY L.J. G. Schermerhorn Abstract The Hercynian cycle, starting in Late Precambrian times and terminated at the end ofthe Palaeozoic, is associated in the Iberian Peninsula with the the deposition of a wide variety of metallic and nonmetallic mineral resources. The most famous of these are the base-metal sulphides of Iberian Pyrite Belt (Rio Tinto and other deposits), tin and tungsten (Panasqueira), and mercury (Almadén). The of the the accumulation of depositional stage Hercynian cycle saw syngenetic mineral deposits, resulting from the interplay of palaeogeographical, sedimentary and volcanic controls. During and after the following orogenic stage, epigenetic minerals originated through magmaticactivity, mostly as direct deposits from magmatic-derived fluids and also indirectly through thermal activation of existing rock. In both stages felsic magmatismwas the dominant agent of mineralization, both for the moreimportant volcanogenic and for the plutonic mineral deposits. Framework and evolution of Hercynian mineralization are defined by the geotectonic intraplate — not plate-margin - setting ofthe Meseta and by its palaeogeographicaland structural developmentduring the cycle, modified by regional and local factors, foremost among which are volcanic and plutonic heat and mass transfer. the Metallogeneticprovinces and epochs are distinguished, metallotects outlined, and possible sources for -
A Template for an Improved Rock-Based Subdivision of the Pre-Cryogenian Timescale
Downloaded from http://jgs.lyellcollection.org/ by guest on September 28, 2021 Perspective Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2020-222 A template for an improved rock-based subdivision of the pre-Cryogenian timescale Graham A. Shields1*, Robin A. Strachan2, Susannah M. Porter3, Galen P. Halverson4, Francis A. Macdonald3, Kenneth A. Plumb5, Carlos J. de Alvarenga6, Dhiraj M. Banerjee7, Andrey Bekker8, Wouter Bleeker9, Alexander Brasier10, Partha P. Chakraborty7, Alan S. Collins11, Kent Condie12, Kaushik Das13, David A. D. Evans14, Richard Ernst15,16, Anthony E. Fallick17, Hartwig Frimmel18, Reinhardt Fuck6, Paul F. Hoffman19,20, Balz S. Kamber21, Anton B. Kuznetsov22, Ross N. Mitchell23, Daniel G. Poiré24, Simon W. Poulton25, Robert Riding26, Mukund Sharma27, Craig Storey2, Eva Stueeken28, Rosalie Tostevin29, Elizabeth Turner30, Shuhai Xiao31, Shuanhong Zhang32, Ying Zhou1 and Maoyan Zhu33 1 Department of Earth Sciences, University College London, London, UK 2 School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, UK 3 Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA, USA 4 Department of Earth and Planetary Sciences, McGill University, Montreal, Canada 5 Geoscience Australia (retired), Canberra, Australia 6 Instituto de Geociências, Universidade de Brasília, Brasilia, Brazil 7 Department of Geology, University of Delhi, Delhi, India 8 Department of Earth and Planetary Sciences, University of California, Riverside, -
Cobalt Mineral Ecology
American Mineralogist, Volume 102, pages 108–116, 2017 Cobalt mineral ecology ROBERT M. HAZEN1,*, GRETHE HYSTAD2, JOSHUA J. GOLDEN3, DANIEL R. HUMMER1, CHAO LIU1, ROBERT T. DOWNS3, SHAUNNA M. MORRISON3, JOLYON RALPH4, AND EDWARD S. GREW5 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Northwest, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. 4Mindat.org, 128 Mullards Close, Mitcham, Surrey CR4 4FD, U.K. 5School of Earth and Climate Sciences, University of Maine, Orono, Maine 04469, U.S.A. ABSTRACT Minerals containing cobalt as an essential element display systematic trends in their diversity and distribution. We employ data for 66 approved Co mineral species (as tabulated by the official mineral list of the International Mineralogical Association, http://rruff.info/ima, as of 1 March 2016), represent- ing 3554 mineral species-locality pairs (www.mindat.org and other sources, as of 1 March 2016). We find that cobalt-containing mineral species, for which 20% are known at only one locality and more than half are known from five or fewer localities, conform to a Large Number of Rare Events (LNRE) distribution. Our model predicts that at least 81 Co minerals exist in Earth’s crust today, indicating that at least 15 species have yet to be discovered—a minimum estimate because it assumes that new minerals will be found only using the same methods as in the past. Numerous additional cobalt miner- als likely await discovery using micro-analytical methods. -
Budowa Geologiczna Górotworu W Dostępnych Sztolniach Rejonu Krobicy–Przecznicy
Dzieje górnictwa – element europejskiego dziedzictwa kultury, 4 pod red. P.P. Zagożdżona i M. Madziarza, Wrocław 2012 kartowanie geologiczne, górnictwo cyny, górnictwo kobaltu, kamienickie pasmo łupkowe, Krobica, Gierczyn, Przecznica Paweł P. ZAGOŻDŻON * Katarzyna D. ZAGOŻDŻON * BUDOWA GEOLOGICZNA GÓROTWORU W DOSTĘPNYCH SZTOLNIACH REJONU KROBICY–PRZECZNICY W artykule przedstawiono wyniki badań geologicznych przeprowadzonych w latach 2010–11 na obszarze dawnych kopalń rud Sn i Co w rejonie Krobicy, Gierczyna i Przecznicy. Ukazano szczegółowe mapy geolog- iczne sztolni Leopold i Rungenschen w Krobicy, sztolni kopalni St. Carol w Kotlinie oraz sztolni upadowej kopalni Anna Maria w Przecznicy. Ponadto przedstawiono uproszczone plany niewielkiego wyrobiska na polu kopalni Hudsrücken w Kotlinie i sztolni Fryderyk Wilhelm koło Przecznicy. W sztolniach udokumentowano obecność szeregu odmian łupków krystalicznych, a także rzadkiej odmi- any skalnej – granatytu. Stwierdzono obecność licznych skupień granatów, polimetalicznej mineralizacji siarczkowej oraz nacieków żelazistych, manganowych i prawdopodobnie kalcytowych. Opisano szereg zjawisk tektonicznych – stref uskokowych różnej skali i deformacji ciągłych Opisane stanowiska będą elementem podziemnej trasy turystycznej w sztolniach Leopold i Rungensche. Niektóre inne wyrobiska mogą stanowić interesujące obiekty wielodyscyplinarnych badań naukowych. 1. Wstęp W sezonach badawczych 2010–11 przeprowadzono prace ternowe w sześciu histo- rycznych obiektach podziemnych. Były to sztolnie Rungenschen i -
Tectonic Regimes in the Baltic Shield During the Last 1200 Ma • a Review
Tectonic regimes in the Baltic Shield during the last 1200 Ma • A review Sven Åke Larsson ' ', Bva-L^na Tuliborq- 1 Department of Geology Chalmers University of Technology/Göteborij U^vjrsivy 2 Terralogica AB November 1993 TECTONIC REGIMES IN THE BALTIC SHIELD DURING THE LAST 1200 Ma - A REVIEW Sven Åke Larsson12, Eva-Lena Tullborg2 1 Department of Geology, Chalmers University of Technology/Göteborg University 2 Terralogica AB November 1993 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author(s) and do not necessarily coincide with those of the client. Information on SKB technical reports from 1977-1978 (TR 121), 1979 (TR 79-28), 1980 (TR 80-26), 1981 (TR 81-17), 1982 (TR 82-28), 1983 (TR 83-77), 1984 (TR 85-01), 1985 (TR 85-20), 1986 (TR 86-31), 1987 (TR 87-33), 1988 (TR 88-32),. 1989 (TR 89-40), 1990 (TR 90-46), 1991 (TR 91-64) and 1992 (TR 92-46) is available through SKB. ) TECTONIC REGIMES IN THE BALTIC SHIELD DURING THE LAST 1200 Ma - A REVIEW by Sven Åke Larson and Eva-Lena Tullborg Department of Geology, Chalmers University of Technology / Göteborg University & Terralogica AB Gråbo, November, 1993 Keywords: Baltic shield, Tectonicregimes. Upper Protero/.oic, Phanerozoic, Mag- matism. Sedimentation. Erosion. Metamorphism, Continental drift. Stress regimes. , ABSTRACT 1 his report is a review about tectonic regimes in the Baltic (Fennoscandian) Shield from the Sveeonorwegian (1.2 Ga ago) to the present. It also covers what is known about palaeostress during this period, which was chosen to include both orogenic and anorogenic events. -
Uchwała Nr XXV/327/20 Z Dnia 26 Listopada 2020 R
DZIENNIK URZĘDOWY WOJEWÓDZTWA DOLNOŚLĄSKIEGO Wrocław, dnia 14 grudnia 2020 r. Poz. 6963 UCHWAŁA NR XXV/327/20 RADY MIEJSKIEJ GMINY MIRSK z dnia 26 listopada 2020 r. w sprawie wyznaczenie obszaru, wielkości i granic aglomeracji Mirsk Na podstawie art. 87 ust. 1 i 4 ustawy z dnia 20 lipca 2017 r. Prawo wodne (t.j. Dz. U. z 2020 r. poz. 310 ze zm.) w związku z § 3 i 4 Rozporządzenia Ministra Gospodarki Wodnej i Żeglugi Śródlądowej z dnia 27 lipca 2018 r. w sprawie sposobu wyznaczania obszaru i granic aglomeracji (Dz. U. z 2018 r. poz. 1586) Rada Miejska Gminy Mirsk uchwala, co następuje: § 1. Wyznacza się aglomerację Mirsk o równoważnej liczbie mieszkańców wynoszącej 6110 RLM z oczyszczalnią ścieków w Mirsku. § 2. Integralną częścią uchwały jest opis wielkości i obszaru aglomeracji zawierający podstawowe informacje dotyczące charakterystyki aglomeracji, stanowiący załącznik nr 1 do uchwały oraz mapa aglomeracji określająca jej granice i położenie w stosunku do najważniejszych obiektów infrastruktury i obszarów chronionych, stanowiąca załącznik nr 2 do uchwały. § 3. Niniejsza uchwała była poprzedzona rozporządzeniem Wojewody Dolnośląskiego z dnia 20 września 2005 r. w sprawie wyznaczenia aglomeracji: Bielawa, Bolków, Brzeg Dolny, Chełmsko Śląskie, Krośnice, Lubawka, Lubomierz, Lwówek Śląski, Malczyce, Mirsk, Olszyna, Piechowice, Stara Kamienica, Syców, Świerzawa, Wądroże Wielkie, Złotoryja (Dz. Urz. Woj. Doln. Nr 198, poz. 3339 ze zm.), które traci moc z dniem wejścia niniejszej uchwały zgodnie z art. 565 ust. 2 ustawy z dnia 20 lipca 2017 r. Prawo wodne (t.j. Dz. U. z 2020 r. poz. 310 ze zm.). § 4. Wykonanie Uchwały powierza się Burmistrzowi Miasta i Gminy Mirsk. -
Download the Scanned
THE AMERICAN MINER.{LOGIST, VOL. 55, SEPTEMBER-OCTOBER, 1970 NEW MINERAL NAN4ES Polarite A. D GnNrrrv, T. L EvsrrcNrEVA, N. V. Tnoxnve, eno L. N. Vver.,sov (1969) polarite, Pd(Pb, Bi) a new mineral from copper-nickel sulfide ores.Zap. Vses.Mined. Obslrch. 98, 708-715 [in Russian]. The mineral was previouslv described but not named by cabri and rraill labstr- Amer. Mineral.52, 1579-1580(1967)lElectronprobeanalyseson3samples(av.of 16, 10,and15 points) gave Pd,32.1,34.2,32 8; Pb 35.2, 38.3,34 0; Bi 31.6, 99.1,334; sum 98 9, 102.8, 100.2 percent corresponding to Pcl (Pb, Bi), ranging from pd1.6 (pb04? Bi0.60)to pdro (PboogBio rs). X-ray powder daLa are close to those of synthetic PbBi. The strongest lines (26 given) are 2 65 (10)(004),2.25 (5)(331),2.16 (9)(124),1.638(5)(144). These are indexed on an orthorhombic cell with a7 l9l, D 8 693, c 10.681A. single crystal study could not be made. In polished section, white with 1'ellowish tint, birefringence not observed. Under crossed polars anisotropic with slight color effects from gray to pale brown Maximum reflectance is given at 16 wave lengths (t140 740 nm) 56.8 percent at 460 nm; 59.2 at 540; 59.6 at 580; 6I.2 at 660. Microhardness (kg/mmr) was measured on 3 grains: 205,232, av 217;168- 199, av 180; 205-232, av 219. The mineral occurs in vein ores of the'r'alnakh deposit amidst chalcopyrite, talnekhite, and cubanite, in grains up to 0.3 mm, intergro.wn with pdspb, Cupd6 (Sn, pb): (stannopal- ladinite), nickeloan platinum, sphalerite, and native Ag The name is for the occurence in the Polar urals. -
Ages of Detrital Zircons
Elsevier Editorial System(tm) for Precambrian Research Manuscript Draft Manuscript Number: Title: AGES OF DETRITAL ZIRCONS (U/Pb, LA-ICP-MS) FROM THE LATEST NEOPROTEROZOIC - MIDDLE CAMBRIAN(?) ASHA GROUP AND EARLY DEVONIAN TAKATY FORMATION, THE SOUTH- WESTERN URALS: A TEST OF AN AUSTRALIA-BALTICA CONNECTION WITHIN RODINIA Article Type: SI:Precambrian Supercontinents Keywords: Urals, Detrital Zircon, Rodinia, Ediacaran, Baltica Corresponding Author: Prof. Nikolay Borisovich Kuznetsov, Ph.D. Corresponding Author's Institution: Geological Institute of Russian Academy of Science First Author: Nikolay B Kuznetsov, Ph.D. Order of Authors: Nikolay B Kuznetsov, Ph.D.; Josef G Meert, Ph.D.; Tatiana V Romanyuk, Ph.D. Abstract: Results from U/Pb-dating of detrital zircons (dZr) from sandstones of the Basu and Kukkarauk Fms. (Asha Group) of Ediacaran-Middle Cambrian(?) age along with the results obtained from the Early Devonian Takaty Fm. are presented. The age of the Asha Group is traditionally labeled as Upper Vendian in the Russian stratigraphic chart that overlaps with the Ediacaran in the International stratigraphic chart. The dZr whose ages fall within the age-interval of (500-750 Ma) are common in the Basu and Kukkarauk Fm. These ages are typical for crystalline complexes in the Pre- Uralides-Timanides orogen. The identification of zircons with this age range agrees with commonly adopted interpretations for the depositional origin of the Asha Group as a molasse resulting from the erosion of that orogenic belt. Based on the estimates of the youngest ages of dZr along with the tentative identification of inarticulate brachiopods in the Kukkarauk Fm., it appears that the upper part of the Asha Group may extend into the Middle Cambrian.