Materiais 2017

Total Page:16

File Type:pdf, Size:1020Kb

Materiais 2017 MATERIAIS 2017 XVIII Congresso da Sociedade Portuguesa dos Materiais VIII International Symposium on Materials An International Conference … Exploring the Latest Progress in Materials Development … Bringing Science Solutions to the World 9-12 April, 2017 University of Aveiro, Aveiro, Portugal Table of Contents Foreword iii Sponsorship iv Organization of Materiais 2017 v Conference Program Program Digest vii Detailed Conference Program viii Numbered List of Posters xxvi Abstracts Plenary Talks 1 Keynote Talks 4 Invited Talks 8 Regular Talks 18 Sattelite Event on Materials for Energy 19 Symposium A - Functional Materials 36 Symposium B - Structural Materials 92 Symposium C - Processing Technologies 117 Symposium D - Characterization and Modelling 152 Posters 175 Symposium A - Functional Materials 176 Symposium B - Structural Materials 289 Symposium C - Processing Technologies 323 Symposium D - Characterization and Modelling 364 ii MATERIAIS 2017, XVIII Congresso da Sociedade Portuguesa de Materiais and VIII International Symposium on Materials, will take place in Aveiro, Portugal, from 9 – 12 April 2017. MATERIAIS 2017, aiming to explore the latest Progress in Materials Development and to bring Science Solutions to the World, provides the ideal forum for scientists, developers, engineers and companies to share their latest breakthroughs, achievements and views in the field of Materials. MATERIAIS 2017 will be hosted by the University of Aveiro in the beautiful city of Aveiro, and in one of the oldest nations in the world, Portugal. It will cover all areas of Materials from Functional Materials, Structural Materials and Processing Technologies to Characterization and Modelling. MATERIAIS 2017 continues the famous MATERIAIS conferences organized every two years by the Portuguese Materials Society (SPM), and is the eighteenth National and the eighth International Materials Conference, since the inaugural one, held in Lisbon in 1983. MATERIAIS returns to Aveiro, after two former editions (1995 and 2005), and follows the last meeting in Porto (MATERIAIS 2015). During the 3 days, MATERIAIS 2017 will encompass schools, scientific talks, debate sessions on cutting edge technologies, and a show case event of applications based on scientific development. We will award for the second time the SPM Career and Recognition Award (Prémio SPM de Carreira e Reconhecimento) that aims to recognize, encourage and promote the excellency of research and development activities in the area of Materials in Portugal. We will also commemorate the 40th Anniversary of the Department of Materials and Ceramics Engineering (DEMaC) of the University of Aveiro. Finally we are very pleased to welcome Materiais 2017 guest society, SOCIEMAT (Sociedade Espanola de Materiales), The Spanish Materials Society. We anticipate that MATERIAIS 2017 will be a very well attended international meeting, with excellent technical and scientific interaction. We look forward to seeing you in Aveiro in April 2017. Paula M. Vilarinho (MATERIAIS 2017 Chair) iii Sponsorship iv Organization of Materiais 2017 CONFERENCE CHAIR Paula M. Vilarinho (Department of Materials and Ceramic Engineering, University of Aveiro) Organizing Committee Ana Luisa Daniel (Chemistry Department, University of Aveiro) Ana Maria Rocha Senos (Department of Materials and Ceramic Engineering, University of Aveiro) João Tedim (Department of Materials and Ceramic Engineering, University of Aveiro) Maria Elizabete Costa (Department of Materials and Ceramic Engineering, University of Aveiro) Maria Paula Seabra (Department of Materials and Ceramic Engineering, University of Aveiro,) Oleksandr Tkach (Department of Materials and Ceramic Engineering, University of Aveiro) Paula Celeste da Silva Ferreira (Department of Materials and Ceramic Engineering, University of Aveiro) Rob Pullar (Department of Materials and Ceramic Engineering, University of Aveiro) Rui Ramos Ferreira e Silva (Department of Materials and Ceramic Engineering, University of Aveiro) Victor Fernando Santos Neto (Department of Mechanical Engineering, University of Aveiro) Scientific Committee Albano Cavaleiro (Department of Mechanical Engineering, University of Coimbra) Ascensão Lopes (Faculty of Engineering of UP – FEUP, University of Oporto) Helena Florindo (iMed, University of Lisbon) João Celestino Rocha (Chemistry Department, University of Aveiro) Jorge Frade (Department of Materials and Ceramic Engineering, University of Aveiro) Leonard Francis (The International Iberian Nanotechnology Laboratory – INL) Luis Gil (Direção Geral de Energia e Geologia, DGEG) Manuel Vieira (Faculty of Engineering of UP – FEUP, University of Oporto) Maria Helena Fernandes (Department of Materials and Ceramic Engineering, University of Aveiro) Paloma Fernandes (Universidad Complutense de Madrid and SOCIEMAT) Paulo Ferreira (Materials Science and Engineering Program, University of Texas at Austin, USA) Pedro Granja (Faculty of Engineering of UP – FEUP, University of Oporto) Sandra Carvalho (Centre of Physics, University of Minho) v The scientific and technical program of the meeting includes the following topics: Symposium A - Functional Materials A1 - Bio-inspired materials and materials for healthcare applications A2 - Magnetic, electric, multiferroic, and plasmonic functional materials A3 - Materials for energy (talks are separated into Energy Satellite Event), environment and sustainable materials A4 - Carbon based materials Symposium B - Structural Materials B1 - Advances in ceramics, concrete, building materials B2 - Advances in metals and alloys B3 - Advances in polymers B4 - Advances in composites and hybrid materials Symposium C - Processing Technologies C1 - Processing using laser/plasma/electric field technologies C2 - Additive manufacturing C3 - Coatings and interfaces C4 – Recycling Symposium D - Characterization and Modelling D1 - Physical, chemical and structural characterization D2 - Mechanical characterization (including at nanoscale) D3 - Advanced characterization using microscopy techniques D4 - Materials modelling (advanced atomistic algorithms, computer simulations) vi Time Sunday, April 9 Monday, April 10 Tuesday, April 11 Wednesday, April 12 SAEM SABio 1. Plenary speakers 2. Key note speakers 3. Invited Spekers 08:30 Registration Registration 08:45 SAEM Opening Materiais 2017 Opening 09:00 Invited Invited Invited - Ian Reaney (Plenary 1) - Chris Bowen (Keynote 1) - Patricia Carvalho (Invited 1) Bus from UA 09:15 Keynote 1 Keynote 2 Keynote 3 Talk 5 Talk 6 Talk 7 - Paolo Bartolo (Plenary 2) - Jonathan Knowles (Keynote 2) - João Gomes (Invited 2) 09:30 SABio Opening A2 Talk 8 C3 Talk 1 A4 Talk 1 - Angus Kingon (Plenary 3) - Lenny Koh (Keynote 3) - Daniel Marinha (Invited 3) Lecture 2.1 Plenary 1 09:45 A2 Talk 1 A1 Talk 24 A3 Talk 1 A2 Talk 9 C3 Talk 2 A4 Talk 2 - Angus Kingon (Invited 4) 10:00 Lecture 1.1 A2 Talk 2 A1 Talk 25 A3 Talk 2 A2 Talk 10 C3 Talk 3 A4 Talk 3 - James Raju (Invited 5) 10:15 - David Maestre (Invited 6) Coffee Break Coffee Break Coffee Break 10:30 Discussions and - Raul Arenal (Invited 7) 10:45 Lecture 1.2 Coffee Break Energy A1 Talk 1 Invited Invited Invited C2 Talk 1 A3 Talk 3 A2 Talk 11 C3 Talk 4 A4 Talk 4 11:00 Invited 1 A1 Talk 2 Talk 1 Talk 2 Talk 4 C2 Talk 2 A3 Talk 4 A2 Talk 12 C3 Talk 5 A4 Talk 5 - Brain Korgel (En. Invited 1) 11:15 En. Talk 1 A1 Talk 3 D3 Talk 1 B4 Talk 1 A2 Talk 3 C2 Talk 3 A3 Talk 5 A2 Talk 13 C3 Talk 6 D4 Talk 8 - Ibrahim Gulyurtlu (En. Invited 2) 11:30 Lecture 1.3 En. Talk 2 A1 Talk 4 D3 Talk 2 B4 Talk 2 A2 Talk 4 C2 Talk 4 C4 Talk 1 A2 Talk 14 C3 Talk 7 B1 Talk 1 Lecture 2.2 11:45 En. Talk 3 A1 Talk 5 D3 Talk 3 B4 Talk 3 A2 Talk 5 C2 Talk 5 C4 Talk 2 A2 Talk 15 C3 Talk 8 B1 Talk 2 12:00 En. Talk 4 A1 Talk 6 D1 Talk 1 B4 Talk 4 A2 Talk 6 C2 Talk 6 C4 Talk 3 A2 Talk 16 C3 Talk 9 B1 Talk 3 12:15 Lecture 1.4 En. Talk 5 A1 Talk 7 D1 Talk 2 B4 Talk 5 A2 Talk 7 C2 Talk 7 C4 Talk 4 A2 Talk 17 C3 Talk 10 B1 Talk 4 12:30 En. Talk 6 A1 Talk 8 B4 Talk 6 D4 Talk 7 C3 Talk 11 B1 Talk 5 Topics: 12:45 En. Talk 7 Symposium A - En. Materials for energy 13:00 Functional A1 Bio-inspired materials and materials for healthcare applications Lunch 13:15 Lunch Lunch Materials A2 Magnetic, electric, multiferroic, and plasmonic functional materials 13:30 Lunch A3 Materials for environment and sustainable materials 13:45 A4 Carbon based materials 14:00 Rector of UA Talk 14:15 Lecture 1.5 A1 Talk 9 Invited B4 Talk 7 Plenary 2 14:30 En. Talk 8 A1 Talk 10 Talk 3 B4 Talk 8 Plenary 3 vii Lecture 2.3 14:45 En. Talk 9 A1 Talk 11 C1 Talk 1 B4 Talk 9 Symposium B - B1 Advances in ceramics, concrete, building materials 15:00 Lecture 1.6 Conference Registration En. Talk 10 A1 Talk 12 C1 Talk 2 B4 Talk 10 Structural B2 Advances in metals and alloys 40 Years Anniversary of DEMaC 15:15 En. Talk 11 A1 Talk 13 C1 Talk 3 B2 Talk 1 Materials B3 Advances in polymers Special Session - Invited Talks 15:30 En. Talk 12 A1 Talk 14 C1 Talk 4 B2 Talk 2 B4 Advances in composites and hybrid materials Discussion and Debate on Additive Manufacturing 15:45 En. Talk 13 A1 Talk 15 C1 Talk 5 B2 Talk 3 Coffee Break Concluding 16:00 En. Talk 14 A1 Talk 16 C1 Talk 6 B2 Talk 4 Remarks Lecture 2.4 16:15 En. Talk 15 A1 Talk 17 C1 Talk 7 B2 Talk 5 16:30 A1 Talk 18 C1 Talk 8 B2 Talk 6 Symposium C - C1 Processing using laser/plasma/electric field technologies Coffee Break 40 Years Anniversary of DEMaC 16:45 Coffee Break Processing C2 Additive manufacturing Round Table 17:00 Energy Technologies C3 Coatings and interfaces Guided tour to 17:15 Q & A session Invited 2 A1 Talk 19 D4 Talk 1 D2 Talk 1 C4 Recycling Museu da Vista 17:30 and Discussions En.
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]
  • 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]
  • Rare Earth Elements in Planetary Crusts: Insights from Chemically Evolved Igneous Suites on Earth and the Moon
    minerals Article Rare Earth Elements in Planetary Crusts: Insights from Chemically Evolved Igneous Suites on Earth and the Moon Claire L. McLeod 1,* and Barry J. Shaulis 2 1 Department of Geology and Environmental Earth Sciences, 203 Shideler Hall, Miami University, Oxford, OH 45056, USA 2 Department of Geosciences, Trace Element and Radiogenic Isotope Lab (TRaIL), University of Arkansas, Fayetteville, AR 72701, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-513-529-9662 Received: 5 July 2018; Accepted: 8 October 2018; Published: 16 October 2018 Abstract: The abundance of the rare earth elements (REEs) in Earth’s crust has become the intense focus of study in recent years due to the increasing societal demand for REEs, their increasing utilization in modern-day technology, and the geopolitics associated with their global distribution. Within the context of chemically evolved igneous suites, 122 REE deposits have been identified as being associated with intrusive dike, granitic pegmatites, carbonatites, and alkaline igneous rocks, including A-type granites and undersaturated rocks. These REE resource minerals are not unlimited and with a 5–10% growth in global demand for REEs per annum, consideration of other potential REE sources and their geological and chemical associations is warranted. The Earth’s moon is a planetary object that underwent silicate-metal differentiation early during its history. Following ~99% solidification of a primordial lunar magma ocean, residual liquids were enriched in potassium, REE, and phosphorus (KREEP). While this reservoir has not been directly sampled, its chemical signature has been identified in several lunar lithologies and the Procellarum KREEP Terrane (PKT) on the lunar nearside has an estimated volume of KREEP-rich lithologies at depth of 2.2 × 108 km3.
    [Show full text]
  • EMD Uranium (Nuclear Minerals) Committee
    EMD Uranium (Nuclear Minerals) Committee EMD Uranium (Nuclear Minerals) Mid-Year Committee Report Michael D. Campbell, P.G., P.H., Chair December 12, 2011 Vice-Chairs: Robert Odell, P.G., (Vice-Chair: Industry), Consultant, Casper, WY Steven N. Sibray, P.G., (Vice-Chair: University), University of Nebraska, Lincoln, NE Robert W. Gregory, P.G., (Vice-Chair: Government), Wyoming State Geological Survey, Laramie, WY Advisory Committee: Henry M. Wise, P.G., Eagle-SWS, La Porte, TX Bruce Handley, P.G., Environmental & Mining Consultant, Houston, TX James Conca, Ph.D., P.G., Director, Carlsbad Research Center, New Mexico State U., Carlsbad, NM Fares M Howari, Ph.D., University of Texas of the Permian Basin, Odessa, TX Hal Moore, Moore Petroleum Corporation, Norman, OK Douglas C. Peters, P.G., Consultant, Golden, CO Arthur R. Renfro, P.G., Senior Geological Consultant, Cheyenne, WY Karl S. Osvald, P.G., Senior Geologist, U.S. BLM, Casper WY Jerry Spetseris, P.G., Consultant, Austin, TX Committee Activities During the past 6 months, the Uranium Committee continued to monitor the expansion of the nuclear power industry and associated uranium exploration and development in the U.S. and overseas. New power-plant construction has begun and the country is returning to full confidence in nuclear power as the Fukushima incident is placed in perspective. India, Africa and South America have recently emerged as serious exploration targets with numerous projects offering considerable merit in terms of size, grade, and mineability. During the period, the Chairman traveled to Columbus, Ohio to make a presentation to members of the Ohio Geological Society on the status of the uranium and nuclear industry in general (More).
    [Show full text]
  • Materiais 2017
    MATERIAIS 2017 XVIII Congresso da Sociedade Portuguesa dos Materiais VIII International Symposium on Materials An International Conference … Exploring the Latest Progress in Materials Development … Bringing Science Solutions to the World 9-12 April, 2017 University of Aveiro, Aveiro, Portugal Table of Contents Foreword iii Sponsorship iv Organization of Materiais 2017 v Conference Program Program Digest vii Detailed Conference Program viii Numbered List of Posters xxvi Abstracts Plenary Talks 1 Keynote Talks 4 Invited Talks 8 Regular Talks 18 Sattelite Event on Materials for Energy 19 Symposium A - Functional Materials 36 Symposium B - Structural Materials 92 Symposium C - Processing Technologies 117 Symposium D - Characterization and Modelling 152 Posters 175 Symposium A - Functional Materials 176 Symposium B - Structural Materials 289 Symposium C - Processing Technologies 323 Symposium D - Characterization and Modelling 364 ii MATERIAIS 2017, XVIII Congresso da Sociedade Portuguesa de Materiais and VIII International Symposium on Materials, will take place in Aveiro, Portugal, from 9 – 12 April 2017. MATERIAIS 2017, aiming to explore the latest Progress in Materials Development and to bring Science Solutions to the World, provides the ideal forum for scientists, developers, engineers and companies to share their latest breakthroughs, achievements and views in the field of Materials. MATERIAIS 2017 will be hosted by the University of Aveiro in the beautiful city of Aveiro, and in one of the oldest nations in the world, Portugal. It will cover all areas of Materials from Functional Materials, Structural Materials and Processing Technologies to Characterization and Modelling. MATERIAIS 2017 continues the famous MATERIAIS conferences organized every two years by the Portuguese Materials Society (SPM), and is the eighteenth National and the eighth International Materials Conference, since the inaugural one, held in Lisbon in 1983.
    [Show full text]
  • O, a New Mineral of the Titanite Group from the Piława Górna Pegmatite, the Góry Sowie Block, Southwestern Poland
    Mineralogical Magazine, June 2017, Vol. 81(3), pp. 591–610 Żabińskiite, ideally Ca(Al0.5Ta 0.5)(SiO4)O, a new mineral of the titanite group from the Piława Górna pegmatite, the Góry Sowie Block, southwestern Poland 1,* 2 3 3 4 ADAM PIECZKA ,FRANK C. HAWTHORNE ,CHI MA ,GEORGE R. ROSSMAN ,ELIGIUSZ SZEŁĘG , 5 5 6 6 7 ADAM SZUSZKIEWICZ ,KRZYSZTOF TURNIAK ,KRZYSZTOF NEJBERT ,SŁAWOMIR S. ILNICKI ,PHILIPPE BUFFAT AND 7 BOGDAN RUTKOWSKI 1 AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, 30-059 Kraków, Mickiewicza 30, Poland 2 Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada 3 Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, 91125-2500, California, USA 4 University of Silesia, Faculty of Earth Sciences, Department of Geochemistry, Mineralogy and Petrography, 41-200 Sosnowiec, Bedzin̨ ská 60, Poland 5 University of Wrocław, Institute of Geological Sciences, 50-204 Wrocław, M. Borna 9, Poland 6 University of Warsaw, Faculty of Geology, Institute of Geochemistry, Mineralogy and Petrology, 02-089 Warszawa, Żwirki and Wigury 93, Poland 7 AGH University of Science and Technology, International Centre of Electron Microscopy for Materials Science, Department of Physical and Powder Metallurgy, 30-059 Kraków, Mickiewicza 30, Poland [Received 7 January 2016; Accepted 21 April 2016; Associate Editor: Ed Grew] ABSTRACT Ż ́ ł abinskiite, ideally Ca(Al0.5Ta0.5)(SiO4)O, was found in a Variscan granitic pegmatite at Pi awa Górna, Lower Silesia, SW Poland. The mineral occurs along with (Al,Ta,Nb)- and (Al,F)-bearing titanites, a pyrochlore-supergroup mineral and a K-mica in compositionally inhomogeneous aggregates, ∼120 μm× 70 μm in size, in a fractured crystal of zircon intergrown with polycrase-(Y) and euxenite-(Y).
    [Show full text]
  • A Glossary of Uranium- and Thorium-Bearing Minerals
    GEOLOGICAL SURVEY CIRCULAR 74 April 1950 A GLOSSARY OF URANIUM­ AND THORIUM-BEARING MINERALS By Judith Weiss Frondel and Michael F1eischer UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director WASHINGTON. D. C. Free on application to the Director, Geological Survey, Washington 25, D. C. A GLOSSAR-Y OF URANIUM- AND THORIUM-BEARING MINERALS By Judith Weiss Fronde! and Michael Fleischer CONTENTS Introduction ••oooooooooo••••••oo•-•oo•••oo••••••••••oooo•oo••oooooo••oo•oo•oo•oooo••oooooooo•oo• 1 .A. Uranium and thorium minerals oooo oo oo ......................... oo .... oo oo oo oo oo oooooo oo 2 B. Minerals with minor amounts of uranium and thorium 000000000000000000000000.... 10 C. Minerals that should be tested for uranium and thorium ...... 00 .. 00000000000000 14 D. Minerals that are non-uranium- or non-thorium­ bearing, but that have been reported to contain impurities or intergrowths of uranium, thorium, or rare-earth minerals oooooo•oo ............ oo ... oo .. oooooo'""""oo" .. 0000 16 Index oo ...... oooooo•oo••••oo•oooo•oo•oooo•·~· .. •oooo•oooooooooooo•oooooo•oooooo•oooo••oo•••oooo••• 18 INTRODUCTION The U. S. ·Geological Survey has for some time been making a systematic survey of da~ pertaining to uranium and thorium minerals and to those minerals that contain trace1 or more of uranium and thorium. This survey consists of collecting authoritative chemical, optical, and X-ray diffraction data from the literature and of adding to these data, where inadequate, by work in the laboratory. The results will he reported from time to time, and the authors welcome in- formation on additional data and names.
    [Show full text]
  • Minerals Found in Michigan Listed by County
    Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee,
    [Show full text]
  • The Pegmatite Dyke at Rømteland
    The pegmatite dyke at Rømteland. A c/e^ci/ii/on of the mme^a/F and a ck/FcuFFlon of the mineral paragenesis, especially within the system (Fe, Mn)O-TiO2-Y2O3-(Nb, Ta)205-Si02 By Thor L. Sverdrup Contents lntro^uction 125 Magnetite 161 125 162 Description of the area 127 162 6etelM!NstionB 128 163 History 129 Orangite 163 Description of the pegmatite .... 130 Palygorskite 164 Temperature of formation of the Plagioclase 164 pegmatite 134 p^rite 166 Magmatic origin; supporting Quartz 166 odBervation3 142 3amalBliite 167 OeBci'lption ot tlie mineral 143 Spessartite 168 143 3pkene 169 147 169 153 170 Apatite 156 170 Bastnåsite 156 Uraninite 170 Lei-yl 157 Clarkeite 171 Liotite 157 171 Oalcite 158 l<2B3olite 171 Chalcopyrite 158 a-uranophane 171 158 ?ircon 171 Chlorite (Daphnite) 158 Mineral paragenesis at Rømteland 173 Columbite 158 The two adjacent four component 159 system with the oxides: (Fe, Luxenite 159 Mn)O-Y2O3-(Nb, Ta)2O5-TiOé> ?luolite 160 SiO2 181 Nematite 160 161 Sammendrag 191 Ilmenite 161 195 Introduction. The pegmatite described is located at Rømteland, about 7 km W of Vigeland, Vest-Agder county, southern Norway. Field investigations were made in the summers of 1955 and 1956, and v the laboratory work was done under the direction of Professor Dr. Tom F. W. Barth and Dr. H. Neumann. The pe^matite is BUllouncie6 by a hornblende bearing quartz monzonite which Barth (1945) has called farsundite. Major (1939) believes the quartz monzonite to be a magmatic rock which during its emplacement has torn loose pieces of the sur rounding gneiss and partly assimilated these.
    [Show full text]
  • Euxenite-(Y) (Y, Ca, Ce, U, Th)(Nb, Ta, Ti)2O6 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic; Typically Metamict
    Euxenite-(Y) (Y, Ca, Ce, U, Th)(Nb, Ta, Ti)2O6 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic; typically metamict. Point Group: 2/m 2/m 2/m. As stout prismatic crystals, to 10 cm, may be flattened k [100] or [010]; commonly in parallel, subparallel, or radiating aggregates; compact massive. Twinning: Common on {201}; rare on {101} or {013}. Physical Properties: Fracture: Conchoidal to subconchoidal. Tenacity: Brittle. Hardness = 5.5–6.5 VHN = 633–692 (50 g load). D(meas.) = 5.3–5.9 D(calc.) = [5.16] Radioactive. Optical Properties: Opaque, translucent on thin edges. Color: Black, brownish black, greenish black; brown to yellow-brown in transmitted light. Streak: Yellowish, grayish, or reddish brown. Luster: Brilliant submetallic, waxy to resinous on fractures. Optical Class: Isotropic. n = 2.06–2.24 R1–R2: (470) 13.7–15.6, (546) 13.0–15.6, (589) 12.5–15.0, (650) 12.4–15.0 Cell Data: Space Group: P cmn (synthetic YNbTiO6). a = 5.5528(6) b = 14.6432(20) c = 5.1953(7) Z = 4 X-ray Powder Pattern: Risør, Norway; after heating at 1200 ◦C. 2.99 (100), 3.66 (40), 2.95 (40), 2.60 (30), 1.830 (30), 1.727 (30), 2.78 (25) Chemistry: (1) (1) (1) UO3 0.04 SnO2 0.12 MnO 0.59 Nb2O5 41.43 UO2 0.67 PbO 0.37 Ta2O5 3.84 Al2O3 0.13 MgO 0.13 SiO2 0.07 Ce2O3 4.34 CaO 4.86 + TiO2 16.39 (Y, Er)2O3 18.22 H2O 1.90 − ThO2 4.95 Fe2O3 1.32 H2O 0.06 ZrO2 0.04 FeO 0.77 Total 100.24 (1) Lyndoch Township, Ontario, Canada.
    [Show full text]
  • Minerals in a Computer
    MINERALS IN TYPICAL COMPUTERS Computer Component Element/Compound Mineral Source of Element Monitor Phosphorescent Coating - Transition Metals: ZnS - Zinc Sulfide Zn, S Sulfur, Hemmimorphite, Zincite Smithsonite, Franklenite Ag - Silver Ag Ag, Pyrargyrite, Cerargyrite Cl - Chlorine Cl Halite Al - Aluminum Al Bauxite Cu - Copper Cu Chalcopyrite, Boronite, Enargite, Cuprite, Malachite, Azurite, Chrysocolla, Chalcocite Au - Gold Au Gold Y2O2S - Yittrium Sulfate Y Eu - Europium Eu (KF, MgF2): Mn Potasium-Magnesium Floride: K, F, Mg, Mn Alunite, Orthoclase, Nephelite, Leucite, Manganese Apophullite; Flourite, Cryolite, Vesuvianite; Lepidolite: Dolomite, Magnesite, Espomite, Spinel, Olivine, Pyrope, Biotite, Talc (Zn,Cd)S - Zinc Cadmium Sulfate Cd Zn2SiO4:O4: Mn, As - ZincSilicate, Manganese, Arsenic As Realgar, Orpiment, Niccolite, Cobalite, Arsenopyrite, Tetrahedrite Gd2O2S: Tb - Gadolinium Sulfate: Tebrium Gd, Tb Y2SiO12:Ce - Yitrium Silicate: Cerium Ce Monzanite, Orthite CRT Glass: Pb - Lead Pb Galena, Cerussite, Anglesite, Pyromorphite SiO2 Si Quartz Plastic Case, Keyboard Thermoplastic - Polypropylene, PVC CaCO2 - additive Ca Calcite, Gypsum, Apatite, Aragonite TiO2 - White Pigment Ti Rutile, Ilmenite, Titanite Amonium Polyphosphate P Apetite, Pyromorphite, Wavellite __________________________________________________________________________________________________________ National Mining Association - 101 Constitution Ave. NW Suite 500 East - Washington, DC 20001 - Phone (202) 463-2600 - Fax (202) 463-2666 Liquid Crystal Display (LCD)
    [Show full text]
  • NIOBIAN TITANITE from the HURON CLAIM PEGMATITE, SOUTHEASTERN MANITOBA* Is
    Canadian Mineralogist Vol. 19, pp. 549-552 (1981) NIOBIAN TITANITE FROM THE HURON CLAIM PEGMATITE, SOUTHEASTERN MANITOBA* V I B.J. PAULt, P. CERNY AND R. CHAPMAN Department of Earth Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2 J.R. HINTHORNE Department of Geology, Central Washington University, Ellensburg, Washington 98926, U.S.A. ABsTRAcT indiquant toutefois une Iegere substitution d'Al a Si, qui ameliore probablement la distribution locale Niobian titanite occurs in the Be,Nb-Ta,Ti, des charges sur les octaedres a Nb-Ta. Les peg­ REE,Y,Zr,Th,U -bearing Huron Claim pegmatite, in matites a titanite sont generalement pauvres en the Winnipeg River pegmatite district of south­ Nb et Ta; par contre, c'est dans les pegmatites eastern Manitoba. The titanite is found in vuggy enrichies en ces elements que pr6dominent les albite and quartz, separate from other Nb,Ta­ oxydes de (Nb, Ta, Ti), ce qui expliquerait la bearing minerals. The Nb205 content is the highest rarete des titanites riches en Nb et Ta. ever found in this species ( 6.5 wt. % ) , and the combined (Nb,Ta).05 content (10.2 wt. %) is sec­ (Traduit par la Redaction) ond only to that of the tantalian titanite from Cra­ Mots-ctes: niobium, tantale, titanite, chimie cristal­ veggia (Clark 1974). Normalization to l:(RIV+Rv1) line, pegmatite, Manitoba. = 8 yields reasonable formulae for both Huron Claim and Craveggia titanites but with slight AI INTRODUCTION substitution for Si, which may improve local charge distribution at Nb,Ta-populated octahedra. Titanite­ The possibility of appreciable substitution of bearing pegmatites are usually low in Nb and Ta, Nb and Ta for Ti in the structure of titanite, and complex Nb,Ta,Ti-bearing oxide minerals predominate in pegmatites enriched in these ele­ frequently advocated on crystallochemical ments, suggesting a scarcity of Nb,Ta-rich titanites.
    [Show full text]