Minerals of Manitoba
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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 -
Contributions to the Mineralogy of Maryland. by II
JOHNS HOPKINS UNIVERSITY CI RCULARS Publis/ied wit/i t/ze approbation ofthe Board of Trustees VoL. YIIJ.—No. 75.1 BALTIMORE, SEPTEMBER, 1889. [PRICE, 10 CENTS. SCIENTIFIC NOTES. Contributions to the Mineralogy of Maryland. By II. Mica Schist. No new minerals. It is doubtful whether all the schists of the Baltimore area are not sufficiently feldspathic to be regarded as GEORGE H. WILLIAMS. gneisses. Since the publication of the “Notes on the Minerals occurring in the III. Crystalline Limestone. In addition to the species, calcite, phlogo- Neighborhood of Baltimore” in 1887, a number of additions have been pite, brown tourmaline, tremolite, pyrite, and iron hydroxide, already made to our knowledge of mineral occurrences both in this district and in recorded as occurring in the crystalline limestones and dolomites of Balti- more distant parts of the State. I have therefore thought it worth while more county, we may now enumerate the following: Quartz, very common to publish a preliminary record of the principal of these, which may serve in rounded grey nodules known to the quarrymen as “flint;” much rarer as an appendix to the above-mentioned pamphlet. in well-formed limpid crystals. Mr. Tidy, for many years salesman for the I shall mention first the new minerals found within the Baltimore Beaver Dam marble company, told me of a remarkable druse of quartz neighborhood—the 625 square miles embraced within the limits of the crystals accidentally found by the breaking of a marble step. He described University Field Club map, to which alone reference was made in the the crystals as resembling tbe glass prisms frequently suspended from chan- “Notes “—and subsequently speak of such species a.s have come to my notice deliers. -
The Rutile Deposits of the Eastern United States
THE RUTILE DEPOSITS OF THE EASTERN UNITED STATES. By THOMAS L. WATSON. INTRODUCTION. The titanium-bearing minerals comprise more than 60 distinct species, grouped under a variety of mineral and chemical forms, chiefly as oxides, titanates, titano-silicates, silicates, columbates, and iantalates. These minerals are widely distributed in a variety of associations and in such quantity as to make titanium a relatively abundant element. Clarke* estimates the. amount of titanium in the solid crust of the earth to be 0.44 per cent, equivalent in oxide to 0.73 per cent, the element thus standing in the ninth place in the scale of abundance, next to potassium. Most of the titanium-bearing minerals, however, are rare and are only of scientific interest. The largest concentrations of the element are as oxide (rutile), as iron titanate (ilmenite), and in iron ferrate (magnetite) as intergrown ilmenite. Of these three forms the prin cipal source of the element at present is rutile. The known workable deposits of rutile, however, are extremely few and widely sepa rated, and as the demand for titanium has greatly increased in the last few years it has been necessary for some uses to turn to ilmenite or highly titaniferous magnetites. This paper briefly summarizes present knowledge of the geology of the rutile deposits in the eastern United States and for the sake of comparison discusses several foreign deposits, each of which has produced some rutile. Of the known deposits in the United, States only those in Virginia are of commercial importance. These have been made the subject of a special report 2 by the Virginia Geological Survey, which was preceded by a preliminary paper on the rutile deposits of Amherst and Nelson counties.3 1 Clarke, F. -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
New Minerals Approved Bythe Ima Commission on New
NEW MINERALS APPROVED BY THE IMA COMMISSION ON NEW MINERALS AND MINERAL NAMES ALLABOGDANITE, (Fe,Ni)l Allabogdanite, a mineral dimorphous with barringerite, was discovered in the Onello iron meteorite (Ni-rich ataxite) found in 1997 in the alluvium of the Bol'shoy Dolguchan River, a tributary of the Onello River, Aldan River basin, South Yakutia (Republic of Sakha- Yakutia), Russia. The mineral occurs as light straw-yellow, with strong metallic luster, lamellar crystals up to 0.0 I x 0.1 x 0.4 rnrn, typically twinned, in plessite. Associated minerals are nickel phosphide, schreibersite, awaruite and graphite (Britvin e.a., 2002b). Name: in honour of Alia Nikolaevna BOG DAN OVA (1947-2004), Russian crys- tallographer, for her contribution to the study of new minerals; Geological Institute of Kola Science Center of Russian Academy of Sciences, Apatity. fMA No.: 2000-038. TS: PU 1/18632. ALLOCHALCOSELITE, Cu+Cu~+PbOZ(Se03)P5 Allochalcoselite was found in the fumarole products of the Second cinder cone, Northern Breakthrought of the Tolbachik Main Fracture Eruption (1975-1976), Tolbachik Volcano, Kamchatka, Russia. It occurs as transparent dark brown pris- matic crystals up to 0.1 mm long. Associated minerals are cotunnite, sofiite, ilin- skite, georgbokiite and burn site (Vergasova e.a., 2005). Name: for the chemical composition: presence of selenium and different oxidation states of copper, from the Greek aA.Ao~(different) and xaAxo~ (copper). fMA No.: 2004-025. TS: no reliable information. ALSAKHAROVITE-Zn, NaSrKZn(Ti,Nb)JSi401ZJz(0,OH)4·7HzO photo 1 Labuntsovite group Alsakharovite-Zn was discovered in the Pegmatite #45, Lepkhe-Nel'm MI. -
The Seven Crystal Systems
Learning Series: Basic Rockhound Knowledge The Seven Crystal Systems The seven crystal systems are a method of classifying crystals according to their atomic lattice or structure. The atomic lattice is a three dimensional network of atoms that are arranged in a symmetrical pattern. The shape of the lattice determines not only which crystal system the stone belongs to, but all of its physical properties and appearance. In some crystal healing practices the axial symmetry of a crystal is believed to directly influence its metaphysical properties. For example crystals in the Cubic System are believed to be grounding, because the cube is a symbol of the element Earth. There are seven crystal systems or groups, each of which has a distinct atomic lattice. Here we have outlined the basic atomic structure of the seven systems, along with some common examples of each system. Cubic System Also known as the isometric system. All three axes are of equal length and intersect at right angles. Based on a square inner structure. Crystal shapes include: Cube (diamond, fluorite, pyrite) Octahedron (diamond, fluorite, magnetite) Rhombic dodecahedron (garnet, lapis lazuli rarely crystallises) Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Cubic Crystals: Diamond Fluorite Garnet Spinel Gold Pyrite Silver Tetragonal System Two axes are of equal length and are in the same plane, the main axis is either longer or shorter, and all three intersect at right angles. Based on a rectangular inner structure. Crystal shapes include: Four-sided prisms and pyramids Trapezohedrons Eight-sided and double pyramids Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Tetragonal Crystals: Anatase Apophyllite Chalcopyrite Rutile Scapolite Scheelite Wulfenite Zircon Hexagonal System Three out of the four axes are in one plane, of the same length, and intersect each other at angles of 60 degrees. -
Scandium Mineralization Associated with Hydrothermal Lazulite-Quartz Veins in the Lower Austroalpine Grobgneis Complex, Eastern Alps, Austria
Bernhard, F. (2001): Scandium mineralization associated with hydrothermal lazulite-quartz veins in the Lower Austroalpine Grobgneis complex, Eastern Alps, Austria. In: Piestrzynski A. et al. (eds.): Mineral Deposits at the Beginning of the 21st Century. Proceedings of the joint sixth biennial SGA-SEG meeting. Kraków, Poland. A.A.Balkema Publishers, 935-938. Scandium mineralization associated with hydrothermal lazulite-quartz veins in the Lower Austroalpine Grobgneis complex, Eastern Alps, Austria F. Bernhard Institut für Technische Geologie und Angewandte Mineralogie, Technische Universität Graz, Rechbauerstraße 12, A-8010 Graz, Austria ABSTRACT: Lazulite (MgAl2(PO4)2(OH)2)-quartz veins within the Lower Austroalpine Grobgneis complex, Austria, have Sc-contents up to 200 ppm. The predominant Sc-carrier is pretulite, ScPO4, and this phase oc- curs as a wide-spread accessory mineral. Vein formation took place at temperatures of 300-500° C and low pressure during Permo-Triassic extensional tectonics and fluid flow. Mg-enriched alteration zones suggest that vein material was not derived from the immediate host rocks. Eo-Alpine metamorphism and deformation overprinted the veins to varying degrees. Despite the low tonnage of the Sc-rich veins, this new type of Sc- mineralization may point to larger Sc-accumulations in similar phosphate-rich hydrothermal environments. 1 INTRODUCTION The long-known lazulite (MgAl2(PO4)2(OH)2)- quartz veins in northeastern Styria and southern Scandium is a moderately abundant transition ele- Lower Austria contain significant Sc-enrichments in ment with an average content ca. 7 ppm in the upper the form of pretulite, ScPO4 (Bernhard et al. 1998b). and ca. 25 ppm in the lower continental crust (We- This contribution gives data on the geology, miner- depohl 1995). -
Compositional Asymmetry in Replacement Tourmaline – an Example from the Tauern Window, Eastern Alps
Geological Volume 4 Number 2 Mater ials August 12, 2002 Researc h Compositional asymmetry in replacement tourmaline – An example from the Tauern Window, Eastern Alps Darrell J. Henry1, Barbara L. Dutrow2 and Jane Selverstone3 1, 2Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70808, USA 1<[email protected]>, 2<[email protected]>, 3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA 3<[email protected] > Abstract Tourmaline, partially replacing pre-existing tourmaline from a tectonically-dismembered tourmalinite vein, has developed distinctive compositional asymmetry that reflects influx of reac- tive fluids. The tourmalinite clast, enclosed in a quartzite from the Tauern Window, Eastern Alps, experienced a clockwise P-T-t path with maximal burial depths of 35-40 km (10-11 kbar), peak temperatures of ~550°C and major deformation preceding peak thermal conditions. The primary tourmaline of the tourmalinite clast, generation-1, is texturally and compositionally heterogeneous, ranging from schorl to dravite [Mg / (Mg + Fe) = 0.27 - 0.61] with highly-variable Al consistent X X with combinations of the Al(NaR)-1 and AlO(R(OH))-1 exchange vectors, where represents X-site vacancy and R is Fe2+ + Mn + Mg. Generation-2 tourmaline is manifest as distinctive compo- sitionally-asymmetric bands of colorless foitite (zone 1) and blue schorl (zone 2) replacing genera- tion-1 tourmaline. Replacement takes place along a scalloped margin and advances preferentially towards the analogous pole (-c) of generation-1 tourmaline. The two zones of generation-2 range from foitite to schorl with a restricted ratio of Mg / (Mg + Fe) of 0.32 - 0.41, but with variable X, X Al, Na and R predominantly reflecting Al(NaR)-1. -
'Uravesmountain Artd-·
/' ;~~ . - . :-.--... -~~;~-'. ' ) ;;. :,~~., . -'uravesMountain artd-· . ',MagrudetMine·, " . WiIkes_ Lmeolll~Gee"'.- .··~-SOUth~(JeolegicalSoc~~ OOidebOOk;NWIlber~3B- - April- 23-25, 1999 -. GRAVES MOUNTAIN AND MAGRUDER MINE Compiled and Edited by: Marc V. Hurst and Cornelis Winkler III - GUIDEBOOK NtTMBER 38 Prepared for the Annual Field Trip of the Southeastern Geological Society April 23-25, 1999 Published by the Southeastern Geological Society P.O. Box 1634 Tallahassee, Florida 32302 TABLE OF CONTENTS LOCATIONS OF GRAVES MOUNTAIN AND MAGRUDERMINE...................................... 1 INTRODUCTION TO GRAVES MOUNTAIN by John S. Whatley, JM. Huber Corporation.................................................................3 PHOSPHATE MINERALS OF GRAVES MOUNTAIN, GEORGIA by Henry BatWood............. .............................................................................................5 GRAVES MOUNTAIN, SLATE BELT, GEORGIA GEOLOGY by Gilles O. Allard, University of Georgia.................................................................... 11 GEOLOGY AND ECONOMIC POTENTIAL OF THE MAGRUDER MINE AND VICINITY by Norman L. Bryan ..................................................................................................... 17 \ \ \ \ \ \ \ \ \ \ Magruder Mme ~\ \ ,\(". ~\1- "'..,.. \9 \'> <'\'ci0;: \ I I I I l-s £-''d C!.'s., "I~ ~ \«\ (>\~ o I' I \ i-20 \ \ I \ \ I \ \ \ \ ~ \ '\ '\ '\ LOCATIONS OF GRAVES MOUNTAIN AND MAGRUDER MINE 2 J 5 ! ! I Scole in Hites Ap,.it 15. 1'J'J'J INTRODUCTION TO GRAVES MOUNTAIN by John S. -
GEMSTONES by Donald W
GEMSTONES By Donald W. Olson Domestic survey data and tables were prepared by Christine K. Pisut, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. Gemstones have fascinated humans since prehistoric times. sustaining economically viable deposits (U.S. International They have been valued as treasured objects throughout history Trade Commission, 1997, p. 23). by all societies in all parts of the world. The first stones known The total value of natural gemstones produced in the United to have been used for making jewelry include amber, amethyst, States during 2001 was estimated to be at least $15.1 million coral, diamond, emerald, garnet, jade, jasper, lapis lazuli, pearl, (table 3). The production value was 12% less than the rock crystal, ruby, serpentine, and turquoise. These stones preceding year. The production decrease was mostly because served as status symbols for the wealthy. Today, gems are not the 2001 shell harvest was 13% less than in 2000. worn to demonstrate wealth as much as they are for pleasure or The estimate of 2001 U.S. gemstone production was based on in appreciation of their beauty (Schumann, 1998, p. 8). In this a survey of more than 200 domestic gemstone producers report, the terms “gem” and “gemstone” mean any mineral or conducted by the USGS. The survey provided a foundation for organic material (such as amber, pearl, and petrified wood) projecting the scope and level of domestic gemstone production used for personal adornment, display, or object of art because it during the year. However, the USGS survey did not represent possesses beauty, durability, and rarity. -
Paula Celeste Da Novel Microporous Silicates and Mesoporous MCM Silva Ferreira Materials Derivatised with Inorganic and Organometallic Complexes
Universidade de Aveiro Departamento de Quimica 0 @ 2000 qso 5a"s Paula Celeste da Novel microporous silicates and mesoporous MCM Silva Ferreira materials derivatised with inorganic and organometallic complexes Dissertação apresentada à Universidade de Aveiro para cumprimento dos requisitos necessários a obtenção do grau de Doutor em Quirnica, realizada sob orientação científica do Doutor João Carlos Matias Celestino Gomes da Rocha, Professor CatedrBtico do Departamento de Quirnica da Universidade de Aveiro. o Júri Presidente: Doutor Casimiro Adrião Pio Professor Catedrático da Universidade de Aveiro Vogais: Doutor Carlos José Rodrigues Crispim Romão Professor Catedrático do Instituto de Tecnologia Química e Biológica da Universidade Nova de Lisboa Doutor João Carlos Matias Celestino Gomes da Rocha Professor Catedrático da Universidade de Aveiro Doutora Maria Filipa Gomes Ribeiro Professora Associada do Departamento de Engenharia Química do Instituto Superior Técnico, da Universidade Técnica de Lisboa Doutora Ana Maria Vieira Silva Viana Cavaleiro Professora Associada da Universidade de Aveiro Doutora Isabel Maria de Sousa Gonçalves Professora Auxiliar da Universidade de Aveiro Doutor Michael William Anderson Full Professor, Department of Chemistry, Institute of Science and Technology, University of Manchester acknowledgements I would like to express my sincere gratitude to my supervisor Prof. Dr. João Rocha for giving me the opportunity to work with him and for sharing with me some of his knowledge. I also acknowledge his continuous help, specially, in the solid state NMR experiments and in the correction of this thesis. I would like to thank Prof. Dr. Isabel Gonçalves for her indispensable help, advice and guidance in the derivatisation of mesoporous MCM rnaterials with organometallic and inorganic complexes. -
Visual Guide to Gemstones.Docx
Visual Guide to Gemstones & Minerals This gemstones glossary provides a wealth of information about gemstones and minerals plus the different types of stones that are used in jewellery making. A ABALONE – with Paua and Red illustrated below: Gemstone Physical Composition: Abalones are members of the Gastropoda class of mollusks that have one- piece shells. Abalone shells have a dichroic, tortoise shell like appearance. They are a source of mother of pearl. Gemstone Physical Characteristics: Gemstone Colour Variations: The Paua shell is part of the abalone family, but has deeper colors of blue, green, and purple. Gemstone Sources: Australia, Japan and the United States. Gemstone Hardness: Gemstone History: Gemstone Uses: Gemstone Care: Gemstone Therapeutic Properties: The mother of pearl is used for the treatment of high blood pressure, dizziness, and heart palpitations Birthstone: n/a Marriage: n/a Zodiac Sign: n/a. AGATE – with Branded, Blue Lace, Condor, Dendritic, Fire, Green, Honey Brush, Moss, Polka Dot, Red, Rossette and Scottish Agates illustrated below: Gemstone Physical Composition: Agate is a member of the Chalcedony or Quartz family characterised by its fineness of grain, brightness of colour, and dramatic banding. It consists of amorphous or cryptocrystalline silica alongside the aforementioned mineral Chalcedony. They are typically associated with volcanic rocks or ancient lavas where they occur as nodules forming from solutions of silica at relatively shallow depths and low temperatures. They are extremely sensitive to the physical and chemical conditions around them forming in concentric layers and filling cavities in a host rock. The results are round bands similar to the rings in tree trunks, whilst also appearing as eyes, scallops, or as landscapes with dendrites that look like trees.