Metallic Minerals

Total Page:16

File Type:pdf, Size:1020Kb

Metallic Minerals Electronic Capture, 2011 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Department of Mines, Natural Resources and Environment MANIT~BA MINERAL RESOURCES DIVISION MRD Educational Series 78/2 Minerals of Manitoba Volume II: Metallic minerals by K.A. Phillips Ph.D., P. Eng. Winnipeg 1979 1 Minerals of Manitoba Volume II: Metallic Minerals Foreword ...................................................................................... 3 Iron oxide minerals ............................................................................ 9 Copper-zinc ore-suites ........................................................................ 20 Nickel-copper ore-suites ...................................................................... 30 Gold ore-suites ................................................................................ 40 References .................................................................................... 59 Indexed Mineral Table ........................................................................ 64 Maps .......................................................................................... 68 Cover plates: Top left - Gold in limonitic veinlets cutting vein quartz (Elbow Lake) Top right - Pyrrhotite accompanied by large black hornblende crystals and cut by small chalcopyrite veinlet (Dumbarton mine) Bottom left - Chalcopyrite ore with graphitic gangue material (Mandy mine) Bottom right - Sphalerite ore with minor pyrite and white plagioclase (Chisel Lake Mine) 2 Foreword This publication is the third in an educational Canada highway at Falcon Lake. The numerous series intended to introduce the general public to rock-dumps to be found on the surface at old mine­ the rocks and minerals of Manitoba. The first, sites and near abandoned shafts are of great interest entitled Common Rocks in Manitoba (1975), to rockhounds and mineral collectors. I n thus introduced the layman to the principal rocks likely describing both the operational and worked out to be encountered. The rock-forming, pegmatitic mines of the province, as well as many exploration and non-metallic minerals were then described in shafts, much information is incidentally given the first volume of Minerals of Manitoba (1978), about the history of mining in Manitoba. The main with details of their occurrences throughout the purpose is, however, to describe Manitoba's rocks province. This paved the way for the present and minerals to the general public, while volume which, in describing Manitoba's metallic references to source documents are given at r1inerals, gives examples from widespread out­ frequent intervals for the benefit of readers who crops, orebodies and mineral deposits, some as far may be interested in greater geological detail. north as Lynn Lake, and others near the Trans- 3 Colo.... Plates 1. Octahedra of magnetite in chlorite schist cut by quartz veinlets (Museum) .... 18 2. Specularite crystals on magnetite-hematite groundmass (Museum) ............ 18 3. Oolitic hematite (Museum) ...................................................... 18 4. Spherulitic hematite (turgite) with interstitial calcite (Black Island) ............. 18 5. Botryoidal goethite, showing radiating fibrous structure (Museum) ............ 18 6. Weathered limonitic surface of pyrrhotite-rich andesite (Bird River area) ...... 18 7. Typical structure of limonitic gossan (Museum) ................................. 19 8. Polished slab of chromite ore showing banding (Bird River Sill) ............... 19 9. Cubic and distorted pyritohedral crystals of pyrite (Anderson Lake Mine) ..... 19 10. Botryoidal pyrite with vein quartz (Dumbarton mine) .......................... 19 11. Large pyrite crystals in pyrrhotite-chalcopyrite groundmass (Osborne Lake Mine) 19 12. Radiating prisms of marcasite (Museum) ........................................ 19 13. Large crystals of pyrite surrounded by chalcopyrite in pyrrhotitic groundmass (Stall Lake Mine) ................................................................. 28 14. Pyrrhotite with sphalerite, chalcopyrite and pyrite (Sherridon mine) ........... 28 15. Chalcopyrite ore with graphitic gangue material (Mandy mine) ................ 28 16. Sphalerite ore with minor pyrite and white plagioclase (Chisel Lake Mine) .... 28 17. Massive, fine-grained pyrite, veined by sphalerite (FUn Flon Mine) ............ 28 18. Galena crystals, showing cubic form and cleavage (Museum) .................. 28 19. Galena with pyrite and chalcopyrite, in vein cutting andesite (Chisel Lake Mine) 29 20. Chalcopyrite in chlorite schist (Flin Flon Mine) ................................. 29 21. Argillaceous host-rock showing pyrrhotitic and pyrite-chalco pyrite-rich bands (White Lake Mine) ............................................................... 29 22. Pyrite crystals and cu bic aggregates, partially oxidized to rusty brown goethite (Baker Patton deposit) ........................................................... 29 23. Pseudomorphic pyrrhotite in chalcopyrite groundmass (Anderson Lake Mine) 29 24. Pyrrhotite with chlorite-biotite gangue, accompanied by chalcopyrite and large pyrite crystals (Stall Lake Mine) ................................................. 29 25. Pyrite-chalcopyrite ore with minor magnetite (Stall Lake Mine) ................ 38 26. Large aggregates of fine-grained pyrite in chalcopyrite-pyrrhotite-pyrite ground- ground- mass (Osborne Lake Mine) .................................................... " 38 27. Large pyrite crystals surrounded by pyrrhotite in chalcopyrite ore (Ruttan Mine) 38 28. Polished slab showing pyrite-pyrrhotite interbanded with dark hematitic gangue material (Ruttan Mine) .......................................................... 38 29. Pyrrhotite accompanied by vein quartz with pink feldspar (Lynn Lake Mine) .. 38 4 30. Pyrrhotite accompanied by large black hornblende crystals and cut by small chalcopyrite vein let (Dumbarton mine) ......................................... 38 31. High-grade pentlandite ore with much pyrrhotite and chalcopyrite (Lynn LakE Mine) ............................................................................ 39 32. Gersdorffite crystals with plagioclase (Museum) ................................ 39 33. Specimen of massive nickeline (Museum) ....................................... 39 34. Chalcopyrite-rich ore with minor pyrrhotite and small amphibole crystals; gab­gab- broic gangue (Lynn Lake Mine) ................................................. 39 35. Serpentinite with minor pyrrhotite (Pipe Mine) ................................. 39 36. Massive pyrrhotite ore crossed by pyrite veinlet and containing insets of magnetite (Pipe Mine) ........................................................... 39 37. Biotite schist containing fine-grained pyrrhotite (Thompson Mine) ............. 50 38. Pegmatitic feldspar accompanied by pyrrhotite with biotite (Thompson Mine) 50 39. Coarse breccia-ore showing large biotite-quartz fragment in pyrrhotite-pyrite­pyrrhotite-pyrite- biotite groundmass (Thompson Mine) .......................................... 50 40. Polished slab of pyrrhotite breccia-ore showing black gangue fragments (Thompson Mine) ............................................................... 50 41. Pyrrhotite and minor chalcopyrite associated with large hornblende crystals (Dumbarton mine) ............................................................... 50 42. Free gold in quartz (San Antonio mine) ........................................ 50 43. Gold in limonitic veinlets cutting vein quartz (Elbow Lake) .................... 51 44. Arsenopyrite crystals accompanied by quartz prisms (Museum) ................ 51 45. Arsenopyrite crystals with quartz (Museum) .................................... 51 46. Bluish black, platy molybdenite (Barren Lake) .................................. 51 47. Gold-bearing pyrite in quartz (San Antonio mine) .............................. 51 48. Gold-bearing chalcopyrite in blue quartz (Cryderman property) ............... 51 Blaek and White Plates A Banded iron formation showing magnetite and quartz bands (Knee Lake) ....... 9 B Hematite in the form known as kidney-ore (Museum) ........................... 10 C White pseudomorphs of serpentine after olivine in black chromite groundmass (Bird River Sill) ..................................................................... 10 D Pyrite with vein quartz; network structure due to leaching (Ruttan Mine) .......... 21 E Polished slab showing banding in pyrite-chalcopyrite ore (North Star mine) ...... 21 F Bands of fine-grained pyrrhotite in andesite (Dumbarton mine) .................. 30 5 Photography All photographs were taken by Peter R. Beech of the Manitoba Government's Information Services. Museum specimens were kindly lent by Dr. G.E. Lammers, Chief Curator of the Manitoba Museum of Man and Nature. Others were from the collection of the Mineral Resources Division. Colour separations by Litho Color Services Ltd. Maps A West Hawk and Falcon Lakes area ................................................. 69 B Bird River Cat Lake area ......................................................... 70 C Rice Lake Beresford Lake area ................................................... 71 D Black Island,
Recommended publications
  • LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, and COBALT ARSENIDE and SULFIDE ORE FORMATION Nicholas Allin
    Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2019 EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION Nicholas Allin Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geotechnical Engineering Commons EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION by Nicholas C. Allin A thesis submitted in partial fulfillment of the requirements for the degree of Masters in Geoscience: Geology Option Montana Technological University 2019 ii Abstract Experiments were conducted to determine the relative rates of reduction of aqueous sulfate and aqueous arsenite (As(OH)3,aq) using foils of copper, nickel, or cobalt as the reductant, at temperatures of 150ºC to 300ºC. At the highest temperature of 300°C, very limited sulfate reduction was observed with cobalt foil, but sulfate was reduced to sulfide by copper foil (precipitation of Cu2S (chalcocite)) and partly reduced by nickel foil (precipitation of NiS2 (vaesite) + NiSO4·xH2O). In the 300ºC arsenite reduction experiments, Cu3As (domeykite), Ni5As2, or CoAs (langisite) formed. In experiments where both sulfate and arsenite were present, some produced minerals were sulfarsenides, which contained both sulfide and arsenide, i.e. cobaltite (CoAsS). These experiments also produced large (~10 µm along longest axis) euhedral crystals of metal-sulfide that were either imbedded or grown upon a matrix of fine-grained metal-arsenides, or, in the case of cobalt, metal-sulfarsenide. Some experimental results did not show clear mineral formation, but instead demonstrated metal-arsenic alloying at the foil edges.
    [Show full text]
  • 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
    [Show full text]
  • Rediscovery of the Elements — a Historical Sketch of the Discoveries
    REDISCOVERY OF THE ELEMENTS — A HISTORICAL SKETCH OF THE DISCOVERIES TABLE OF CONTENTS incantations. The ancient Greeks were the first to Introduction ........................1 address the question of what these principles 1. The Ancients .....................3 might be. Water was the obvious basic 2. The Alchemists ...................9 essence, and Aristotle expanded the Greek 3. The Miners ......................14 philosophy to encompass a obscure mixture of 4. Lavoisier and Phlogiston ...........23 four elements — fire, earth, water, and air — 5. Halogens from Salts ...............30 as being responsible for the makeup of all 6. Humphry Davy and the Voltaic Pile ..35 materials of the earth. As late as 1777, scien- 7. Using Davy's Metals ..............41 tific texts embraced these four elements, even 8. Platinum and the Noble Metals ......46 though a over-whelming body of evidence 9. The Periodic Table ................52 pointed out many contradictions. It was taking 10. The Bunsen Burner Shows its Colors 57 thousands of years for mankind to evolve his 11. The Rare Earths .................61 thinking from Principles — which were 12. The Inert Gases .................68 ethereal notions describing the perceptions of 13. The Radioactive Elements .........73 this material world — to Elements — real, 14. Moseley and Atomic Numbers .....81 concrete basic stuff of this universe. 15. The Artificial Elements ...........85 The alchemists, who devoted untold Epilogue ..........................94 grueling hours to transmute metals into gold, Figs. 1-3. Mendeleev's Periodic Tables 95-97 believed that in addition to the four Aristo- Fig. 4. Brauner's 1902 Periodic Table ...98 telian elements, two principles gave rise to all Fig. 5. Periodic Table, 1925 ...........99 natural substances: mercury and sulfur.
    [Show full text]
  • Polymetallic Mineralization in Ediacaran Sediments in the Żarki-Kotowice Area, Poland
    MINERALOGIA, 43, No 3-4: 199-212 (2012) DOI: 10.2478/v10002-012-0008-0 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Polymetallic mineralization in Ediacaran sediments in the Żarki-Kotowice area, Poland Łukasz KARWOWSKI1*, Marek MARKOWIAK2 1University of Silesia, Faculty of Earth Sciences, ul. Będzińska 60, 41-200 Sosnowiec, Poland; e-mail: [email protected] 2Polish Geological Institute - Research and Development Unit, Upper Silesian Branch, ul. Królowej Jadwigi 1, 41-200 Sosnowiec, Poland; e-mail: [email protected] * Corresponding author Received: September 5, 2012 Received in revised form: February 20, 2013 Accepted: March 17, 2013 Available online: March 30, 2013 Abstract. In one small mineral vein in core from borehole 144-Ż in the Żarki-Kotowice area, almost all of the ore minerals known from related deposits in the vicinity occur. Some of the minerals in the vein described in this paper, namely, nickeline, hessite, native silver and minerals of the cobaltite-gersdorffite group, have not previously been reported from elsewhere in the Kraków-Lubliniec tectonic zone. The identified minerals are chalcopyrite, pyrite, marcasite, sphalerite, Co-rich pyrite, tennantite, tetrahedrite, bornite, galena, magnetite, hematite, cassiterite, pyrrhotite, wolframite (ferberite), scheelite, molybdenite, nickeline, minerals of the cobaltite- gersdorffite group, carrollite, hessite and native silver. Moreover, native bismuth, bismuthinite, a Cu- and Ag-rich sulfosalt of Bi (cuprobismutite) and Ni-rich pyrite also occur in the vein. We suggest that, the ore mineralization from the borehole probably reflects post-magmatic hydrothermal activity related to an unseen granitic intrusion located under the Mesozoic sediments in the Żarki-Pilica area.
    [Show full text]
  • Discussion Paper on Mineral Groups by E. H. Nickel
    Discussion Paper on Mineral Groups by E. H. Nickel INTRODUCTION There are two aspects to the compilation of mineral groups. One is the criteria to be used in defining a group. In a recent meeting of the CCM in Melbourne, it was generally agreed that the main criteria defining a group are that it should comprise at least two species, and that the species comprising the group should be isostructural, as indicated by similarity of space group and unit-cell parameters. An important additional consideration is the need to develop an arrangement of the groups in a way that makes it relatively easy to find the group to which a particular mineral species should be consigned. There are many ways in which mineral groups can be classified, and I have looked at four different possibilities with the aim of initiating discussion on this topic. To illustrate the four different classification systems, I have applied them to the sulfide and sulfosalt minerals. The four systems, demonstrated below, are as follows: I) Alphabetical; II) Hey’s chemical classification; III) A combination of Hey’s chemical classification and Smith’s structural formulae; and IV) Strunz’s chemical-structural classification. Comments and suggestions are welcomed. I) SULFIDE AND SULFOSALT GROUPS ALPHABETICAL LISTING Argyrodite Group: Orthorhombic, Pna21 (33). Argyrodite structure type Arsenopyrite Group: Monoclinic, P21/c (14). Related to marcasite structure. Berthierite Group: Orthorhombic, Pnam (62). Berthierite structure type. Bournonite Group: Orthorhombic, Pn21m (31). Bournonite structure type Bowieite Group: Orthorhombic, Pbcn (60). Bowieite structure type. Braggite Group: Tetragonal, P42/m (84). Braggite structure type. Brezinaite Group: Monoclinic, I2/m (12).
    [Show full text]
  • Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1
    Nickeline NiAs c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Commonly in granular aggregates, reniform masses with radial structure, and reticulated and arborescent growths. Rarely as distorted, horizontally striated, {1011} terminated crystals, to 1.5 cm. Twinning: On {1011} producing fourlings; possibly on {3141}. Physical Properties: Fracture: Conchoidal. Tenacity: Brittle. Hardness = 5–5.5 VHN = n.d. D(meas.) = 7.784 D(calc.) = 7.834 Optical Properties: Opaque. Color: Pale copper-red, tarnishes gray to blackish; white with strong yellowish pink hue in reflected light. Streak: Pale brownish black. Luster: Metallic. Pleochroism: Strong; whitish, yellow-pink to pale brownish pink. Anisotropism: Very strong, pale greenish yellow to slate-gray in air. R1–R2: (400) 39.2–45.4, (420) 38.0–44.2, (440) 36.8–43.5, (460) 36.2–43.2, (480) 37.2–44.3, (500) 39.6–46.4, (520) 42.3–48.6, (540) 45.3–50.7, (560) 48.2–52.8, (580) 51.0–54.8, (600) 53.7–56.7, (620) 55.9–58.4, (640) 57.8–59.9, (660) 59.4–61.3, (680) 61.0–62.5, (700) 62.2–63.6 Cell Data: Space Group: P 63/mmc. a = 3.621(1) c = 5.042(1) Z = 2 X-ray Powder Pattern: Unknown locality. 2.66 (100), 1.961 (90), 1.811 (80), 1.071 (40), 1.328 (30), 1.033 (30), 0.821 (30) Chemistry: (1) (2) Ni 43.2 43.93 Co 0.4 Fe 0.2 As 55.9 56.07 Sb 0.1 S 0.1 Total 99.9 100.00 (1) J´achymov, Czech Republic; by electron microprobe, corresponds to (Ni0.98Co0.01 Fe0.01)Σ=1.00As1.00.
    [Show full text]
  • 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.
    [Show full text]
  • Standing Strong Manitoba Operations at [email protected] 2013/2014 Annual Update on Vale in Manitoba Or 204-778-2326
    About the Jasyn paints animals and Artist landscapes, but has also worked in a variety of areas such as abstract Born Jasyn expressionism, surrealism and Bighetty of the sculpture. He is known in Thompson Mathias Colomb for painting murals on buildings. Cree First In 2005, he painted a mural on the Nation, Jasyn side of the Surface Dry building at was adopted into the Lucas family Vale’s Thompson Operations to help of Thompson, Manitoba before commemorate the 50th anniversary his first birthday. His father, Jack of the year of discovery of the Lucas, worked at Vale and retired in Thompson ore body. 2010. Jasyn grew up in Thompson Although he was a featured artist and graduated from R.D. Parker at the 2010 Winter Olympics Collegiate. He moved to North in Vancouver and has sold his Vancouver in 1999 where he works around the world, Jasyn graduated from Capilano College continues to work out of Thompson, with a Diploma in Studio Art. Manitoba. He travels, putting on art In 2007, Jasyn returned to Thompson shows across the country, but his and decided to dedicate his time main goal is to further develop his to a career as a visual artist and skills and use technology to have a painter. He works mainly with stronger international presence. acrylic on canvas, both hand-painted For further information visit applications and airbrush, finding www.jasynlucas.ca. a balance in both traditional and contemporary applications. For more detailed information, please visit our website www.vale.com/canada or contact Ryan Land, Manager, Corporate Affairs and Organizational Development, Standing Strong Manitoba Operations at [email protected] 2013/2014 Annual Update on Vale in Manitoba or 204-778-2326.
    [Show full text]
  • Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba
    Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province
    [Show full text]
  • Copper Cliff, Ontario, January, 1969 Number 10 Inco Triangle January, 1969
    VOLUME 28 COPPER CLIFF, ONTARIO, JANUARY, 1969 NUMBER 10 INCO TRIANGLE JANUARY, 1969 senger car and consumer products Highway 17 Commuters Were Puzzled industries in 1968 maintained the demand for decorative nickel plating, despite lower per-unit CMAKi,F consumption. Nickel plating of plastics is being more widely in- Published for all employees of The troduced into the automotive in- International Nickel Company of dustry and is expected to aid in Canada Limited counteracting competition to nickel D. M. Dunbar, Editor from colored coatings and non- D. J. Wing, Assistant Editor metallic materials. Editorial Office, Copper Cliff, Ont. In summary, the demand for Authorized as second class mail by the nickel continues to grow, and Post Office Department, Ottawa, and for so does the industry's production payment of postage in cash. capability. We are still in a period Material contained in Inco Triangle of tight supply, but established should not be reprinted unless permission has been obtained from The International nickel producers and new com- Nickel Company of Canada, Limited, panies entering the industry are Copper Cliff, Ontario. making large capital expenditures to alter this situation. They are expanding their existing facilities, developing new mines and build- Inco Leads World's ing new plants and conducting an unprecedented search in many Nickel Industry in parts of the globe for new nickel deposits. Meeting Challenges A challenging course for which production, research and explora- Expanding tion must all be geared up to new highs, has been charted for the nickel industry by the pressure of Markets world demand, International Nickel president Albert P.
    [Show full text]
  • Nickel: the Stuff of Legends
    Nickel: The Stuff of Legends by Frank J. Verderber* Chemist (BSGS / ASCT) Columbia Manufacturing Inc. Westfi eld, MA USA A legend is defi ned by Merriam Webster as: “a story After many years of high tech employ, and a few coming down from the past.” Nickel is a legend, stops at other peripheral enterprises, my skills found and one that hails from the origins of the universe. place in the world of consumer goods, specifi cally It drives the engines of exploding stars and is the pri- the manufacture of “chrome-bright” metal furniture. mary reason for the existence of iron. In retrospect, My employer, a durable and all-American corpora- this story of nickel will not reiterate the fi ne articles tion, Columbia Manufacturing, Inc, of Westfield, completed by academics and engineers, who for so Massachusetts, took me in, and from there began many years have kept vigil over fi nishing apparatus an odyssey of intrigue and discovery, much different and tanks of green solutions. They paid their dues than my mind could have ever imagined. Our wares, and embraced the world of fi nishing - men such as covered in nickel and chromium, give scholarly impe- George Dupernell, who wrote a fi ne piece in 1959, tus to our end-users, by virtue of holding the posterior which has since been reprinted in the 2006 volume of of students and academics. Columbia is the second Plating & Surface Finishing. Oh, I wince to recount largest manufacturer of metal chairs and tables, for the story of Adams and Watts and all the celebrated universities, public and private schools.
    [Show full text]
  • TEXTURES and COMPOSITIONAL VARIABILITY in GERSDORFFITE from the CRESCENCIA Ni–(Co–U) SHOWING, CENTRAL PYRENEES, SPAIN: PRIMARY DEPOSITION OR RE-EQUILIBRATION?
    1513 The Canadian Mineralogist Vol. 44, pp. 1513-1528 (2006) TEXTURES AND COMPOSITIONAL VARIABILITY IN GERSDORFFITE FROM THE CRESCENCIA Ni–(Co–U) SHOWING, CENTRAL PYRENEES, SPAIN: PRIMARY DEPOSITION OR RE-EQUILIBRATION? ISABEL FANLO§ AND IGNACIO SUBÍAS Cristalografía y Mineralogía, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, C/ Pedro Cerbuna 12, E–50009 Zaragoza, Spain FERNANDO GERVILLA Instituto Andaluz de Ciencias de la Tierra y Departamento de Mineralogía y Petrología, Facultad de Ciencias, C.S.I.C.–Universidad de Granada, E–18002 Granada, Spain JOSE MANUEL Cristalografía y Mineralogía, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, C/ Pedro Cerbuna 12, E–50009 Zaragoza, Spain ABSTRACT At the Crescencia showing in the Pyrenees, Spain, three stages of mineral deposition can be distinguished: stage I: nickeline and pararammelsbergite, stage II: gersdorffi te, and stage III: uraninite. Gersdorffi te has been subdivided into seven groups on the basis of textural and compositional criteria. Some of these groups of gersdorffi te clearly show disequilibrium processes that may have been induced by secondary reactions associated with a re-equilibration of the system during cooling. Formation and subsequent growth of gersdorffi te nuclei on the nickeline (0001) surface, self-organization, or a coupled dissolution-and-repre- cipitation moving interface through pararammelsbergite or nickeline are some of the processes invoked during the re-equilibra- tion. Thus, the compositional variations found in the seven groups of gersdorffi te are likely due to intermediate steps during the bulk of the replacement and re-equilibration processes at low temperature, rather than a direct precipitation from the ore-forming fl uids under different conditions.
    [Show full text]