Specialty Metals in Canada

Total Page:16

File Type:pdf, Size:1020Kb

Specialty Metals in Canada Specialty Metals In Canada G.J. Simandl, E.A. Prussin, and N. Brown British Columbia Geological Survey Open File 2012-7 Ministry of Energy and Mines Recommended citation: Simandl, G.J., Prussin, E.A., and Brown, N., 2012. Specialty Metals In Canada. British Columbia Geological Survey Open File 2012-7. Cover Photo: ++ Eudialyte [Na4(Ca,Ce)2(Fe ,Mn,Y)ZrSi8O22(OH,Cl)2], a rare earth element-bearing mineral (pink). Other major constituents are feld- spar (white and gray), sodic amphibole (dark green) and mosandrite and/or agrellite (graysh-buff). Sample from the Specimen Pit (Trench 1 of the Matamec Explorations Inc.), Kipawa, Quebec. Canadian quarter for scale. British Columbia Ministry of Energy and Mines Specialty Metals in Canada Simandl, G. J.1,2, Prussin, E.A.1 and Brown, N.1 1British Columbia Geological Survey, Ministry of Energy and Mines, Victoria, B.C. 2School of Earth and Ocean Sciences, University of Victoria, Victoria, B.C. Abstract Specialty metals (SMs) are critical for the development of green technologies, essential raw materials for high technology industries, and deemed strategic for national security by the USA and several European countries. More than one thousand Ta, Nb, Zr, Hf, Li, REE and Be occurrences are known in Canada. Only two Canadian SM deposits are being mined, the ferroniobium producing St. Honoré carbonatite (Niobec) and the Cs- and Ta- producing Bernic Lake deposit (Tanco Mine). Several Ta, Nb, REE and Li prospects are reaching pre-feasibility or feasibility stages. Examples are: Crevier Township, Nb-Ta (QC); Aley Carbonatite, Nb (BC); Blue River, Ta-Nb (BC); Nechalacho, REE (NT); Strange Lake, REE (QC); Kipawa, REE (QC); LaCorne Township, Li (QC); and Wabouchi (also known as Lac des Montagnes) Li (QC). Ontario has the greatest number of occurrences (373), followed by Quebec (195), NWT (115), British Columbia (108), Newfoundland (86), and the remaining provinces, Yukon and Nunavut (220, combined). These occurrences can be described as anomalies (140), showings (563), prospects (204), developed prospects (109), past producers (23), current producers (8), Li-bearing oilfield brines (48), and oil sands by- products (2). Geologically, the occurrences can be grouped into 14 categories: carbonatite/syenite-related; peralkaline intrusion-related; pegmatite/granite/aplite; REE ± P veins; placer/paleoplacer; sedimentary phosphates; REE- enriched Iron oxide copper gold ore (IOCG); sandstone-hosted xenotime; REE as uranium by-products; skarns; greisen/veins; Li-bearing brines; oils sands by-products; and other/unknown. Canada has excellent geological potential to supply SMs worldwide. British Columbia Geological Survey Open File 2012-7 1 British Columbia Ministry of Energy and Mines Introduction (LREE) and heavy (HREE) categories. Traditional definition of LREEs The terms “specialty metal” (SM) and includes La, Ce, Pr, Nd, Sm, Eu and Gd “rare metal” are synonymous. They and the term HREEs covers Tb, Dy, refer to uncommon, nonferrous metals Ho, Er, Tm, Yb and Lu. More recently, used in quantities of typically less than industry defined LREEs as La-Eu and 150000 tonnes/year or derived from HREEs as Gd-Lu series. Y is also geographically restricted areas. The commonly considered an HREE, based term SM was adopted by the Targeted on its geological association and Geoscience Initiative-4 (TGI-4) chemical properties. Sc is not grouped program and will be used throughout either with LREEs or HREEs. this paper. Examples of SMs include: Promethium (Pm) does not occur in tantalum (Ta); niobium (Nb); zirconium nature. Germanium (Ge), gallium (Ga) (Zr); hafnium (Hf); lithium (Li); and vanadium (V) are also classified as beryllium (Be), and rare earth elements SMs, but they are excluded from this (REE). According to the International study because they are not covered Union of Pure and Applied Chemistry under the mandate of the Specialty (IUPA) the term “rare earth Metals component of the TGI-4 element” (REE) encompasses yttrium program (Simandl, 2010b). (Y), scandium (Sc) and the lanthanide The tonnage and value of specialty series: lanthanum (La), cerium (Ce), metals mined worldwide is minor praseodymium (Pr), neodymium (Nd), compared to common industrial metals promethium (Pm), samarium (Sm), such as iron, copper, nickel, zinc, and europium (Eu), gadolinium (Gd), lead. Nonetheless, high technology terbium (Tb), dysprosium (Dy), industries need a secure supply of SMs holmium (Ho), erbium (Er), thulium at competitive prices. Although other (Tm), ytterbium (Yb) and lutetium materials can substitute for several (Lu). This definition is used herein. SMs, they are typically more expensive REEs are further subdivided into light or less effective. For example: British Columbia Geological Survey Open File 2012-7 2 British Columbia Ministry of Energy and Mines palladium and ultra-stable zeolite can have a SM specified either as a primary replace REE’s used as catalysts; or secondary commodity. In these cases andalusite, chromite, and kyanite can territorial geologists felt very strongly substitute for zircon in refractories; and that based on the deposit type, Zn-Carbon and Ni-Cd can be used in geological settings, and similarity with batteries instead of Li. Many countries other occurrences that SMs have been consider several SMs essential for probably overlooked or not reported. national security as highlighted in the In the following we discuss the 2010 “Review of Critical Raw global sources and production of Materials for Europe”, spearheaded by specialty metals, describe the the European Commission. Table 1 geological setting of Canadian deposits describes the prices, uses, and market and occurrences, and consider applied information for selected SMs. mineralogical and metallurgical aspects. The inventory presented on the accompanying map (Fig. 1) and in Global sources and Table 2 is current as of Fall, 2011. It is production of specialty based mainly on provincial and territorial databases, and documents metals occurrences and deposits that have at Rare Earth Elements least one specialty metal listed as a Global production for 2011 is estimated commodity. The provincial data were between 100000 and 140000 tonnes of collected, merged, examined, and contained REOs. China currently classified using 14 deposit categories controls the REE market by using a based on the association between the system of mining, separation and mineralization and the host rock. The smelting, and export quotas. The high resulting compilation was sent for technology industry and governments verification to provincial and territorial of industrialized countries are geologists. Six data entries in Yukon concerned about China’s control of the Territory (#s 1, 2, 3, 4, 5 and 6) do not market and recent volatility of REO British Columbia Geological Survey Open File 2012-7 3 British Columbia Ministry of Energy and Mines prices (Simandl, 2010a). More than fertilizer production (Simandl et al., 556 REE exploration projects are active 2011a, b, c). Other potential sources worldwide. Of these, 296 are include seafloor occurrences, which grassroots (no drilling), 157 have have recently received attention (Kato limited drilling, 66 are in the advanced et al., 2011). exploration stage, 26 are in the pre- feasibility stage, 7 are at the feasibility Niobium stage, and 4 are under construction The global Nb supply for 2011 is (Intierra, 2012). New drilling results estimated at 63000 tonnes of contained were announced from 54 projects; 19 Nb (Papp, 2012a). Brazil (58000 are in Canada and 12 are in Australia tonnes) and Canada (4 400 tonnes) are (Intierra, 2012). Under the market the main producing countries. conditions that follow the law of supply Niobium is traded mostly in the form of and demand (without production quotas ferroniobium and as niobium alloys and or the governmental interferences), only metal. Most Nb is used in steel (75%) the best of the above primary REE and superalloys (25%). For 2011, the deposits will reach the production stage value of US consumption is expected to and remain economically viable over an be about $400 million, as measured by extended period of time. The quality of the value of imports (Papp, 2012a). a REE deposit is determined by World Nb reserves were reported to be mineralogy (Simandl, 2010a), grade, 3 million tonnes of contained Nb (Papp, HREE-LREE ratio, tonnage, depth and 2012a). shape of the ore zone, proven and simple metallurgy, infrastructure, and Tantalum environmental constraints plus the Global Ta supply for 2011 is estimated availability of labour. at 790 tonnes of contained Ta (Papp, High potential exists for recovery of 2012b). According to Mining Journal substantial tonnage of REE as a by- (2012), approximately 40% is being product of uranium and/or phosphate recovered from tin slags. The remainder British Columbia Geological Survey Open File 2012-7 4 British Columbia Ministry of Energy and Mines is divided equally between primary Ta Canada and Australia or to the mines and secondary concentrates, development of currently sub-economic which consist largely of columbite, deposits. struverrite, and recycled materials. The main producers are: Mibra mine in Zirconium/Hafnium Nazareno (Brazil), with a capacity of Global production of zirconium 181 tonnes Ta2O5/year; Kenticha mine concentrates for 2011 is estimated at (Ethiopia), producing 200000 lb of more than 1.4 million tonnes of Ta2O5/year; and Lovozero (Russia) contained Zr. Substantial increase in producing 120000 lb/year (Mining demand since 2010
Recommended publications
  • 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]
  • 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
    [Show full text]
  • The Mineral Industry of Burundi in 2016
    2016 Minerals Yearbook BURUNDI [ADVANCE RELEASE] U.S. Department of the Interior January 2020 U.S. Geological Survey The Mineral Industry of Burundi By Thomas R. Yager In 2016, the production of mineral commodities—notably can be found in previous editions of the U.S. Geological Survey gold, tantalum, tin, and tungsten—represented only a minor Minerals Yearbook, volume III, Area Reports—International— part of the economy of Burundi (United Nations Economic Africa, which are available at https://www.usgs.gov/centers/ Commission for Africa, 2017). The legislative framework for nmic/africa-and-middle-east. the mineral sector in Burundi is provided by the Mining Code of Burundi (law No. 1/21 of October 15, 2013). The legislative Reference Cited framework for the petroleum sector is provided by the Mining United Nations Economic Commission for Africa, 2017, Burundi, in African and Petroleum Act of 1976. Data on mineral production are statistical yearbook 2017: United Nations Economic Commission for Africa, in table 1. Table 2 is a list of major mineral industry facilities. p. 113–117. (Accessed November 7, 2018, at https://www.uneca.org/sites/ More-extensive coverage of the mineral industry of Burundi default/files/PublicationFiles/asyb-2017.pdf.) TABLE 1 BURUNDI: PRODUCTION OF MINERAL COMMODITIES1 (Metric tons, gross weight, unless otherwise specified) Commodity2 2012 2013 2014 2015 2016 METALS Gold, mine, Au contente kilograms 500 400 500 500 500 Niobium and tantalum, mine, columbite-tantalite concentrate: Gross weight do. 258,578 73,518 105,547 53,093 r 31,687 Nb contente do. 51,000 14,000 21,000 10,000 r 6,200 Ta contente do.
    [Show full text]
  • Jadar Lithium Mine,Serbia
    2021 Jadar Lithium Mine, Serbia A Raw Deal ICT metal mining case study Author Zvezdan Kalmar, CEKOR Editing Emily Gray Design Milan Trivic Cover SN040288, Depositphotos Acknowledgements Association Protect Jadar and Rađevina Center for Ecology and Sustainable Development (Centar za ekologiju i održivi razvoj – CEKOR) is an environmental and development organisation. Apart from monitoring international financial institutions’ activities in Serbia, CEKOR is working on issues in the areas of transport, waste, biodiversity, genetically modified organisms (GMO) and making the city of Subotica sustainable. CEKOR is a member of CEE Bankwatch Network. Coalition for Sustainable Mining, Serbia (Koalicija za održivo rudarstvo u Srbiji – KORS) is an organisation that promotes the application of the strictest social and environmental standards for mining and mineral use in Serbia. CEE Bankwatch Network is the largest network of grassroots, environmental and human rights groups in central and eastern Europe. It monitors public finance institutions that are responsible for hundreds of billions of investments across the globe. Together with local communities and other NGOs Bankwatch works to expose their influence and provide a counterbalance to their unchecked power. About ICT and the mining-related work of CEE Bankwatch Network CEE Bankwatch Network has been monitoring mining projects in Europe and abroad for years. Bankwatch cooperates with the Make ICT Fair consortium, which seeks to reform the information and communication technology (ICT) manufacture and minerals supply chains and to improve the lives of workers and those impacted along different stages of the ICT supply chain. Our long-term cooperation with groups monitoring the impact of mining on people and environment as well as with communities directly affected by mines or smelters strengthens our conviction that the many negative impacts of mining must finally come under the proper scrutiny.
    [Show full text]
  • Session 1 Sources and Availability of Materials for Lithium Batteries
    Session 1: Sources and Availability of Materials for Lithium Batteries Session 1 Sources and Availability of Materials for Lithium Batteries Adrian Griffin Managing Director, Lithium Australia NL ABSTRACT Lithium, as a feedstock for the battery industry, originates from two primary sources: hard-rock (generally spodumene and petalite), and brines. Brine processing results in the direct production of lithium chemicals, whereas the output from hard-rock production is tradeable mineral concentrates that require downstream processing prior to delivery, as refined chemicals, into the battery market. The processors of the concentrates, the 'converters', are the major constraint in a supply chain blessed with abundant mineral feed. The battery industry must overcome the constraints imposed by the converters, and this can be achieved through the application of the Sileach™ process, which produces lithium chemicals from concentrates direct, without the need for roasting. The cathode chemistries of the most efficient lithium batteries have a common thread – a high dependence on cobalt. Battery manufacturers consume around 40% of the current production of cobalt, a by-product of the nickel and copper industries. This means cobalt is at a tipping point – production will not keep up with demand. In the short term, the solution lies in developing alternative cathode compositions, while in the longer term recycling may be the answer. Lithium Australia NL is researching the application of its Sileach™ process to waste batteries to achieve a high-grade, low-cost source of battery materials and, in so doing, ease the supply constraints on cathode metals. To ensure that the battery industry is sustainable, better utilisation of mineral resources, more efficient processing technology, an active battery reprocessing capacity and less reliance on cobalt as a cathode material are all necessary.
    [Show full text]
  • Alphab Etical Index
    ALPHAB ETICAL INDEX Names of authors are printed in SMALLCAPITALS, subjects in lower-case roman, and localities in italics; book reviews are placed at the end. ABDUL-SAMAD, F. A., THOMAS, J. H., WILLIAMS, P. A., BLASI, A., tetrahedral A1 in alkali feldspar, 465 and SYMES, R. F., lanarkite, 499 BORTNIKOV, N. S., see BRESKOVSKA, V. V., 357 AEGEAN SEA, Santorini I., iron oxide mineralogy, 89 Boulangerite, 360 Aegirine, Scotland, in trachyte, 399 BRAITHWAITE, R. S. W., and COOPER, B. V., childrenite, /~kKERBLOM, G. V., see WILSON, M. R., 233 119 ALDERTON, D. H. M., see RANKIN, A. H., 179 Braunite, mineralogy and genesis, 506 Allanite, Scotland, 445 BRESKOVSKA, V. V., MOZGOVA, N. N., BORTNIKOV, N. S., Aluminosilicate-sodalites, X-ray study, 459 GORSHKOV, A. I., and TSEPIN, A. I., ardaite, 357 Amphibole, microstructures and phase transformations, BROOKS, R. R., see WATTERS, W. A., 510 395; Greenland, 283 BULGARIA, Madjarovo deposit, ardaite, 357 Andradite, in banded iron-formation assemblage, 127 ANGUS, N. S., AND KANARIS-SOTIRIOU, R., autometa- Calcite, atomic arrangement on twin boundaries, 265 somatic gneisses, 411 CANADA, SASKATCHEWAN, uranium occurrences in Cree Anthophyllite, asbestiform, morphology and alteration, Lake Zone, 163 77 CANTERFORD, J. H., see HILL, R. J., 453 Aragonite, atomic arrangements on twin boundaries, Carbonatite, evolution and nomenclature, 13 265 CARPENTER, M. A., amphibole microstructures, 395 Ardaite, Bulgaria, new mineral, 357 Cassiterite, SW England, U content, 211 Arfvedsonite, Scotland, in trachyte, 399 Cebollite, in kimberlite, correction, 274 ARVlN, M., pumpellyite in basic igneous rocks, 427 CHANNEL ISLANDS, Guernsey, meladiorite layers, 301; ASCENSION ISLAND, RE-rich eudialyte, 421 Jersey, wollastonite and epistilbite, 504; mineralization A TKINS, F.
    [Show full text]
  • Petrology of Nepheline Syenite Pegmatites in the Oslo Rift, Norway: Zr and Ti Mineral Assemblages in Miaskitic and Agpaitic Pegmatites in the Larvik Plutonic Complex
    MINERALOGIA, 44, No 3-4: 61-98, (2013) DOI: 10.2478/mipo-2013-0007 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Petrology of nepheline syenite pegmatites in the Oslo Rift, Norway: Zr and Ti mineral assemblages in miaskitic and agpaitic pegmatites in the Larvik Plutonic Complex Tom ANDERSEN1*, Muriel ERAMBERT1, Alf Olav LARSEN2, Rune S. SELBEKK3 1 Department of Geosciences, University of Oslo, PO Box 1047 Blindern, N-0316 Oslo Norway; e-mail: [email protected] 2 Statoil ASA, Hydroveien 67, N-3908 Porsgrunn, Norway 3 Natural History Museum, University of Oslo, Sars gate 1, N-0562 Oslo, Norway * Corresponding author Received: December, 2010 Received in revised form: May 15, 2012 Accepted: June 1, 2012 Available online: November 5, 2012 Abstract. Agpaitic nepheline syenites have complex, Na-Ca-Zr-Ti minerals as the main hosts for zirconium and titanium, rather than zircon and titanite, which are characteristic for miaskitic rocks. The transition from a miaskitic to an agpaitic crystallization regime in silica-undersaturated magma has traditionally been related to increasing peralkalinity of the magma, but halogen and water contents are also important parameters. The Larvik Plutonic Complex (LPC) in the Permian Oslo Rift, Norway consists of intrusions of hypersolvus monzonite (larvikite), nepheline monzonite (lardalite) and nepheline syenite. Pegmatites ranging in composition from miaskitic syenite with or without nepheline to mildly agpaitic nepheline syenite are the latest products of magmatic differentiation in the complex. The pegmatites can be grouped in (at least) four distinct suites from their magmatic Ti and Zr silicate mineral assemblages.
    [Show full text]
  • The Challenges of Li Determination in Minerals: a Comparison of Stoichiometrically Determined Li by EPMA with Direct Measurement by LA-ICP-MS and Handheld LIBS
    The challenges of Li determination in minerals: A comparison of stoichiometrically determined Li by EPMA with direct measurement by LA-ICP-MS and handheld LIBS Robin Armstrong (NHM) THE TEAM & ACKNOWLEDGEMENTS • This work was carried out as part of the WP2 of the FAME project • The “analysts”: John Spratt & Yannick Buret (NHM) and Andrew Somers (SciAps) • The “mineralogists”: Fernando Noronha &Violeta Ramos (UP), Mario Machado Leite (LNEG), Jens Anderson, Beth Simmons & Gavyn Rollinson (CSM), Chris Stanley, Alla Dolgopolova, Reimar Seltmann & Mike Rumsey* (NHM) • Literature mineral data is taken from Mindat, Webmineral and DHZ • Robin Armstrong ([email protected]) INTRODUCTION • The analytical problems of Li • Whole Rock analysis (WR) • Examples and is it safe to make mineralogical assumptions on the base of WR • Li Mineral analysis • Li-minerals overview • Li-minerals examined • EPMA • LA-ICP-MS • LIBS • Summary and thoughts for the future LITHIUM ORES ARE POTENTIALLY COMPLEX 50mm • Li-bearing phases identified: • Lepidolite, Amblygonite-Montebrasite Li = 1.17 wt% group, Lithiophosphate(tr) and Petalite WHOLE ROCK ANALYSIS (Li ASSAYS) • Li is not that straight forward to analyse in whole rock • Its low mass means that there are low fluorescence yields and long wave-length characteristic radiation rule out lab-based XRF and pXRF • We cannot use conventional fluxes as these are generally Li- based • We can use “older” non Li fluxes such as Na2O2 but then there maybe contamination issues in the instruments • We can use multi-acid digests (HF+HNO3+HClO4 digestion with HCl-leach) (FAME used the ALS ME-MS61) however there may still be contamination issues and potentially incomplete digestion.
    [Show full text]
  • Tin, Tungsten, and Tantalum Deposits of South Dakota
    TIN, TUNGSTEN, AND TANTALUM DEPOSITS OF SOUTH DAKOTA. By FRANK L. HESS. INTRODUCTION. Many articles have been written 011 the tin deposits of the Black Hills, and an excellent paper by J. D. Irving a on the tungsten deposits at Lead was published in 1901. Nothing is known to have been pub­ lished on the tungsten deposits of the southern Black Hills, but several articles have been written on the deposits of tantalum. Nearly all the papers on these different deposits, however, are a num­ ber of years old, and later developments have given several of the deposits an aspect somewhat different from their appearance at the time they were described. It therefore seems well to give a brief account of observations made by the writer during a short reconnais­ sance trip in September, 1908, together with such reviews of the his­ tory and the literature of the region as may seem advisable. All the known deposits of tin, tungsten, and tantalum in South Dakota occur in the Black Hills, in Lawrence and Pennington coun­ ties, in the southwestern part of the State. Although designated as "hills," these elevations reach a height of 7,216 feet in Harney Peak, 500 feet above the highest of the Appalachians (Mount Mitchell, 6,711 feet) and almost a thousand feet above the highest of the White Mountains (Mount Washington, 6,279 feet). They are about 60 to 75 miles long by 50 miles wide, the longer axis lying nearly north and south. There is a considerable diversity of topography in the different parts of the area to be considered.
    [Show full text]
  • Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia
    minerals Article Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia Lia Kogarko 1,* and Troels F. D. Nielsen 2 1 Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 119991 Moscow, Russia 2 Geological Survey of Denmark and Greenland, 1350 Copenhagen, Denmark; [email protected] * Correspondence: [email protected] Received: 23 September 2020; Accepted: 16 November 2020; Published: 20 November 2020 Abstract: Lovozero complex, the world’s largest layered peralkaline intrusive complex hosts gigantic deposits of Zr-, Hf-, Nb-, LREE-, and HREE-rich Eudialyte Group of Mineral (EGM). The petrographic relations of EGM change with time and advancing crystallization up from Phase II (differentiated complex) to Phase III (eudialyte complex). EGM is anhedral interstitial in all of Phase II which indicates that EGM nucleated late relative to the main rock-forming and liquidus minerals of Phase II. Saturation in remaining bulk melt with components needed for nucleation of EGM was reached after the crystallization about 85 vol. % of the intrusion. Early euhedral and idiomorphic EGM of Phase III crystalized in a large convective volume of melt together with other liquidus minerals and was affected by layering processes and formation of EGM ore. Consequently, a prerequisite for the formation of the ore deposit is saturation of the alkaline bulk magma with EGM. It follows that the potential for EGM ores in Lovozero is restricted to the parts of the complex that hosts cumulus EGM. Phase II with only anhedral and interstitial EGM is not promising for this type of ore.
    [Show full text]
  • Lithium 2017
    2017 Minerals Yearbook LITHIUM [ADVANCE RELEASE] U.S. Department of the Interior September 2020 U.S. Geological Survey Lithium By Brian W. Jaskula Domestic survey data and tables were prepared by Annie Hwang, statistical assistant. In the United States, one lithium brine operation with an cobalt oxide and 2,160 kg of lithium-nickel-cobalt-aluminum associated lithium carbonate plant operated in Silver Peak, oxide (Defense Logistics Agency Strategic Materials, 2017). At NV. Domestic and imported lithium carbonate, lithium yearend 2017, the NDS held 540 kg of lithium-cobalt oxide and chloride, and lithium hydroxide were consumed directly 1,620 kg of lithium-nickel-cobalt-aluminum oxide. in industrial applications and used as raw materials for downstream lithium compounds. In 2017, lithium consumption Production in the United States was estimated to be equivalent to The U.S. Geological Survey (USGS) collected domestic 3,000 metric tons (t) of elemental lithium (table 1) [16,000 t production data for lithium from a voluntary canvass of the of lithium carbonate equivalent (LCE)], primarily owing to only U.S. lithium carbonate producer, Rockwood Lithium Inc. demand for lithium-based battery, ceramic and glass, grease, (a subsidiary of Albemarle Corp. of Charlotte, NC). Production pharmaceutical, and polymer products. In 2017, the gross weight and stock data collected from Rockwood Lithium were withheld of lithium compounds imported into the United States increased from publication to avoid disclosing company proprietary data. by 7% and the gross weight of exports increased by 29% from The company’s 6,000-metric-ton-per-year (t/yr) Silver Peak those in 2016.
    [Show full text]
  • Report on the Sonora Lithium Project
    Report on the Sonora Lithium Project (Pursuant to National Instrument 43-101 of the Canadian Securities Administrators) Huasabas - Bacadehuachi Area (Map Sheet H1209) Sonora, Mexico o o centered at: 29 46’29”N, 109 6’14”W For 330 – 808 – 4th Avenue S. W. Calgary, Alberta Canada T2P 3E8 Tel. +1-403-237-6122 By Carl G. Verley, P. Geo. Martin F. Vidal, Lic. Geo. Geological Consultant Vice-President, Exploration Amerlin Exploration Services Ltd. Bacanora Minerals Ltd. 2150 – 1851 Savage Road Calle Uno # 312 Richmond, B.C. Canada V6V 1R1 Hermosillo, Mexico Tel. +1-604-821-1088 Tel. +52-662-210-0767 Ellen MacNeill, P.Geo. Geological Consultant RR5, Site25, C16 Prince Albert, SK Canada S6V 5R3 Tel. +1-306-922-6886 Dated: September 5, 2012. Bacanora Minerals Ltd. Report on the Sonora Lithium Project, Sonora, Mexico Date and Signature Page Date Dated Effective: September 5, 2012. Signatures Carl G. Verley, P.Geo. ____________________ Martin F. Vidal, Lic. Geo. Ellen MacNeill, P.Geo. Amerlin Exploration Services Ltd. - Consulting mineral exploration geologists ii Bacanora Minerals Ltd. Report on the Sonora Lithium Project, Sonora, Mexico Table of Contents 1.0 Summary ................................................................................................................................... 1 2.0 Introduction ............................................................................................................................... 3 3.0 Reliance on Other Experts .......................................................................................................
    [Show full text]