Banded Iron Formations, Pyritic Black Shale, and Gold Deposits: a Re-Evaluation

Total Page:16

File Type:pdf, Size:1020Kb

Banded Iron Formations, Pyritic Black Shale, and Gold Deposits: a Re-Evaluation i Banded iron formations, pyritic black shale, and gold deposits: A re-evaluation by Jeffrey Alan Steadman B.S., M.S. (Geology) Submitted in fulfillment of the requirements for the degree of Doctor of Philosophy October 2015 ii iii Declaration of originality This thesis contains no material which has been accepted for the award of any other degree or diploma in any tertiary institution and, to the best of my knowledge and belief, contains no copy or paraphrase of material previously published or written by another person, except where due referenceis made in the text of the thesis, nor does the thesis contain any material that infringes copyright. Signaru,e Date: 6- (Q·- JS Authorityof access This thesis may be made available for loan and limited copying in accordance with the Copyright Act of 1968. Signatme Date: 6 -/0-/J: Statement regarding published work The publishers of the papers comprising Chapters 2, 3, 4, and 5 hold the copyright for those contents; access to those materials should be sought from the journals Precambrian Research and Economic Geology. The remaining non-published content of the thesis may be made available for loan and limited copying in accordance with the Copyright Act of 1968. Signatme Date: b --/&J�/s iv Statement of co-authorship The following people and institutions contributed to the publication of work undertaken as part of this thesis: 1. Jeffrey A Steadman (CODES [ARC Centre of Excellence in Ore Deposits], University of Tasmania) 2. Ross R Large (CODES, University of Tasmania) 3. Sebastien Meffre (CODES, University of Tasmania) 4. Stuart W Bull (CODES, University of Tasmania) 5. Garry J Davidson (CODES, University of Tasmania) 6. Paul H Olin (CODES, University of Tasmania) 7. Jay Thompson (CODES, University of Tasmania) 8. Leonid Danyushevsky (CODES, University of Tasmania) 9. Daniel D. Gregory (CODES, University of Tasmania) 10. Ivan Belousov (CODES, University of Tasmania) 11. Elena Lounejeva (CODES, University of Tasmania) 12. Trevor R. Ireland (Research School of Earth Sciences [RSES], Australian National University) 13. Peter Holden (RSES, Australian National University) Paper details and authors’ roles Paper 1 (Located in Chapter 2) Age, origin, and significance of nodular sulfides in 2680 Ma carbonaceous black shale of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia Jeffrey A Steadman (candidate), Ross R Large, Sebastien Meffre, and Stuart W Bull Candidate was the primary author and with author 2, author 3 and author 4 contributed to the idea, its formalisation and development Author 2 and author 3 assisted with refinement and presentation Authors 2 and 4 offered assistance in the field Author 3 provided assistance in the laboratory Paper 2 (Located in Chapter 3) Paragenesis and composition of sulfides, oxides, and silicates in the Randalls BIF-hosted gold deposits, Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia: Implications for the timing of ore deposit formation and constraints on possible gold sources Jeffrey A Steadman (candidate), Ross R Large, Garry J Davidson, Stuart W Bull, Jay Thompson, Trevor R. Ireland, and Peter Holden Candidate was the primary author and with author 2, author 3, author 4, author 5, author 6, and author 7 contributed to the idea, its formalisation and development Authors 2, 3, and 4 assisted with refinement and presentation Authors 2 and 4 provided assistance in the field Authors 5, 6, and 7 assisted in the laboratory v Paper 3 (Located in Chapter 4) Syn-sedimentary, diagenetic, and metamorphic pyrite,pyrrhotite, and marcasite at the Homestake BIF-hosted gold deposit, South Dakota, USA: Insights on ore genesis from LA-ICP-MS trace element and sulfur isotope studies JeffreyA Steadman (candidate), Ross R Large, Trevor R. Ireland, and Peter Holden Candidate was the primary author and with author 2, author 3, and author 4 contributed to the idea, its formalisation and development Author 2 and Stuart W Bull (secondary advisor) assisted with refinement and presentation Authors 3 and 4 assisted in the laboratory (SHRIMP S isotopes) Paper 4 (Located in Chapter 5) Syn-sedimentary to early diagenetic gold in black shale-hosted pyrite nodules at the Golden Mile deposit, Kalgoorlie, WesternAustralia JeffreyA Steadman (candidate), Ross R Large, Sebastien Meffre,Paul H Olin, Leonid V Danyushevsky, Daniel D Gregory, Ivan Belousov, Elena Lounejeva, Trevor R Ireland, and Peter Holden Candidate was the primary author and with author 2, author 3, and author 4 contributed to the idea, its formalisation and development Authors 2, 3, 4, and 5 assisted with refinement and presentation Authors 4, 6, 7, 8, 9, and 10 assisted in the laboratory We the undersigned agree with the above stated 'proportion of work undertaken' for each of the above published (or submitted) peer-reviewed manuscripts contributing to this thesis: Signed: Signed: Ross R Large Leonid Danyushevsky Supervisor Head of Discipline, Earth Science School of Physical Sciences School of Physical Sciences University ofTasmania University ofTasmania Date: Date: vi Acknowledgements For the work at Lucky Bay (Chapter 2) and Randalls (Chapter 3), I would like to thank Chris Cairns (former Managing Director, Integra Mining Pty Ltd.) and Terry Brown (former General Manger for Project Development, Integra Mining) for permission to carry out these projects. Special thanks to Karsten Gömann and Sandrin Feig (Central Science Laboratory [CSL], University of Tasmania) for help with the SEMs and the microprobe. Thanks also to Christine Cook (CSL, University of Tasmania) for analyzing sulfide separates for S isotope measurements. Leonid Danyushevsky, Sarah Gilbert, and Sebastien Meffre are thanked for their input, suggestions, and expertise with the laser ablation system at CODES. And last, but not least: many thanks to all the fieldies and geologists at Mt. Monger field station; I could not have done this work without you! The project at Homestake (Chapter 4) was graciously supported by the staff at SURF (Sanford Underground Research Facility) in Lead, South Dakota. Special thanks to Jaret Heise (Science Director, SURF) for permission to carry out research on the archived drill core and for logistical support. Discussions with former Homestake geologists Tom Trancynger, John Scheetz, and Kathy Hart were of immense value. We are also indebted to Prof. Colin Paterson (South Dakota School of Mines and Technology) for his expertise on Homestake geology and his hospitality. The lead author is also grateful to Mark Fahrenbach at the South Dakota Geological Survey and the legendary Black Hills field geologist Jack Redden for a productive one-day field excursion around the north-central Black Hills. The laser staff at CODES were indispensible to the success of this project; thanks especially to Leonid Danyushevsky, Sarah Gilbert, Sebastien Meffre, Marcel Guillong, and Ian Little. François Robert is thanked for providing permission to publish this work on behalf of Barrick Mining Company. Finally, we wish to thank the Editor of Economic Geology, Larry Meinert, and associate editor Paul Spry, plus reviewers John Ridley and Robert Frei for their critical suggestions. These greatly improved the quality of this manuscript. For the work on the Golden Mile (Chapter 5), I wish to thank the Editor of Economic Geology, Larry Meinert, and reviewers Neil Phillips, Iain Pitcairn, Cam McCuaig, Katy Evans, Shaun Barker, and an anonymous reviewer from Economic Geology, all of whom provided valuable comments and criticisms that have greatly helped in improving the final version of this manuscript. Thanks also to Drs. Karsten Goëmann and Sandrin Feig (CSL, UTas) for their assistance with the Hitachi SU70 FESEM. SDG. When I was nearing the end of my Master’s degree and had plans for doing a PhD, I had no intention of leaving the United States. However, a good word about CODES was put in by my Master’s advisor, Paul Spry (himself not only Australian but Tasmanian - Lindisfarne born and raised!), so I applied for a scholarship. Four short years later, here I am at the end of it all. The biggest thanks go to my primary supervisor Ross Large, whose fountain of ideas, insight, and optimism is never-ending. I was pretty wet behind the ears when I got to Hobart, and I am oh-so- grateful that he stuck with me to the end. Running a close second to Ross are my secondary supervisors, Stuart Bull and Garry Davidson, who provided chapter feedback and support when Ross was busy or away (which was more often than I preferred!). I also want to thank Sebastien Meffre, because he was like a fourth supervisor to me, though his name was never on any official university paperwork as such. So much of my laser work (particularly vii the Pb isotope studies with sulfides) would never have made it as far as it did with his guidance and expertise. Merci beaucoup. I would be remiss in not tipping my figurative hat to all the students and staff who have come and gone in my four years here as a student; all of them provided a helping hand, a word of encouragement, or constructive criticism at various times in various places. Paul George (digital graffiti) and June Pongratz (CODES thesis designer extraordinare) were invaluable in navigating all things Adobe-related. June was especially indispensible in finalizing this printed work. viii ix Abstract Banded iron formations (BIF) are predominantly Precambrian sedimentary rocks composed of alternating layers of iron-rich minerals (commonly hematite and magnetite, but also siderite, chlorite,
Recommended publications
  • Fundamental Flotation Behaviors of Chalcopyrite and Galena Using O-Isopropyl-N-Ethyl Thionocarbamate As a Collector
    minerals Article Fundamental Flotation Behaviors of Chalcopyrite and Galena Using O-Isopropyl-N-Ethyl Thionocarbamate as a Collector Yongjie Bu ID , Yuehua Hu *, Wei Sun *, Zhiyong Gao ID and Runqing Liu School of Mineral Processing and Bioengineering, Central South University, Changsha 410083, China; [email protected] (Y.B.); [email protected] (Z.G.); [email protected] (R.L.) * Correspondence: [email protected] (Y.H.); [email protected] (W.S.); Tel.: +86-731-8830-482 (Y.H.); +86-0731-8883-6873 (W.S.) Received: 31 January 2018; Accepted: 12 March 2018; Published: 13 March 2018 Abstract: Copper and lead are two important and widely used metals in industry. Chalcopyrite (CuFeS2) is associated with galena (PbS) in ore, and it has been a research hotspot in separating galena from chalcopyrite by flotation. In this study, the flotation behaviors of chalcopyrite and galena were studied through flotation tests, adsorption measurements, solution chemistry calculation, Fourier transform infrared spectroscopy (FTIR) and molecular dynamics (MD) simulations. The results show that the floatability of chalcopyrite is better than that of galena in the presence of O-isopropyl-N-ethyl thionocarbamate (IPETC), and the recovery difference between chalcopyrite and galena is about 20% when IPETC is 7 × 10−4 mol/L at pH 9.5, while the floatability difference between the two minerals is significant. Competitive adsorption of OH− and IPETC on mineral surfaces leads to lower floatability of galena than that of chalcopyrite. IPETC is able to remove the hydration layer on mineral surfaces and then adsorb on active sites. The floatability of minerals is enhanced with the increase of their hydrophobicity.
    [Show full text]
  • A Review of Flotation Separation of Mg Carbonates (Dolomite and Magnesite)
    minerals Review A Review of Flotation Separation of Mg Carbonates (Dolomite and Magnesite) Darius G. Wonyen 1,†, Varney Kromah 1,†, Borbor Gibson 1,† ID , Solomon Nah 1,† and Saeed Chehreh Chelgani 1,2,* ID 1 Department of Geology and Mining Engineering, Faculty of Engineering, University of Liberia, P.O. Box 9020 Monrovia, Liberia; [email protected] (D.G.W.); [email protected] (Y.K.); [email protected] (B.G.); [email protected] (S.N.) 2 Department of Electrical Engineering and Computer Science, University of Michigan, Ann Arbor, MI 48109, USA * Correspondence: [email protected]; Tel.: +1-41-6830-9356 † These authors contributed equally to the study. Received: 24 July 2018; Accepted: 13 August 2018; Published: 15 August 2018 Abstract: It is well documented that flotation has high economic viability for the beneficiation of valuable minerals when their main ore bodies contain magnesium (Mg) carbonates such as dolomite and magnesite. Flotation separation of Mg carbonates from their associated valuable minerals (AVMs) presents several challenges, and Mg carbonates have high levels of adverse effects on separation efficiency. These complexities can be attributed to various reasons: Mg carbonates are naturally hydrophilic, soluble, and exhibit similar surface characteristics as their AVMs. This study presents a compilation of various parameters, including zeta potential, pH, particle size, reagents (collectors, depressant, and modifiers), and bio-flotation, which were examined in several investigations into separating Mg carbonates from their AVMs by froth flotation. Keywords: dolomite; magnesite; flotation; bio-flotation 1. Introduction Magnesium (Mg) carbonates (salt-type minerals) are typical gangue phases associated with several valuable minerals, and have complicated processing [1,2].
    [Show full text]
  • Overview of Tungsten Indicator Minerals Scheelite and Wolframite with Examples from the Sisson W-Mo Deposit, Canada
    Overview of tungsten indicator minerals scheelite and wolframite with examples from the Sisson W-Mo deposit, Canada M. Beth McClenaghan1, M.A. Parkhill2, A.A. Seaman3, A.G. Pronk3, M. McCurdy1 & D.J. Kontak4 1Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8 (e-mail: [email protected]) 2New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 50, Bathurst, New Brunswick, Canada E2A 3Z1 3New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 6000, Fredericton, New Brunswick, Canada E3B 5H1 4Department of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada P3E 2C6 These short course notes provide an overview of published lit- Table 1. List of regional surveys and case studies conducted around erature on the use of scheelite and wolframite as indicator min- the world in which scheelite and/or wolframite in surficial sediments erals for W, Mo, and Au exploration. The use of scheelite and have been used as indicator minerals. wolframite in stream sediments is well documented for mineral Mineral Media Location Source of Information exploration but less so for using glacial sediments (Table 1). scheelite stream sediments Pakistan Asrarullah (1982) wolframite stream sediments Burma ESCAP Scretariat (1982) The Geological Survey of Canada has recently conducted a scheelite, wolframite stream sediments USA Theobald & Thompson (1960) glacial till and stream sediment indicator mineral case study scheelite stream sediments, soil Thailand Silakul (1986) around the Sisson W-Mo deposit in eastern Canada. scheelite stream sediments Greenland Hallenstein et al. (1981) Preliminary indicator mineral results from this ongoing study scheelite stream sediments Spain Fernández-Turiel et al.
    [Show full text]
  • A Column Leaching Model of Low-Grade Chalcopyrite Ore: Mineral Preferences and Chemical Reactivity
    minerals Article A Column Leaching Model of Low-Grade Chalcopyrite Ore: Mineral Preferences and Chemical Reactivity Heike Bostelmann and Gordon Southam * School of Earth and Environmental Sciences, The University of Queensland, St Lucia 4072, Australia; [email protected] * Correspondence: [email protected]; Tel.: +61-07-3365-8505 Received: 16 November 2020; Accepted: 8 December 2020; Published: 17 December 2020 Abstract: Bioleaching models to examine copper extraction from low-grade chalcopyrite ores were set up to identify the influence of pyrite on leaching efficacy. A combination of scanning electron microscopy and geochemical analysis showed that extraction was marginally enhanced by the addition of pyrite when using a combination of Leptospirillum ferrooxidans, an iron oxidiser, Acidithiobacillus thiooxidans, a sulphur oxidising species and Acidithiobacillus ferrooxidans, an iron and sulphur oxidiser. Extensive biofilms formed on the pyrite surfaces (>106 cells/mm2) but were severely limited on chalcopyrite, possessing approximately the same number of cells as quartz grains, an internal non-nutrient control “substrate” (with ca. 2 103 cells/mm2). The presence of dissolved copper did × not inhibit the growth of this consortium. Indirect “bioleaching” of chalcopyrite appears to be limited by proton activity at the chalcopyrite surface. Keywords: bioleaching; chalcopyrite; pyrite; low-grade ore 1. Introduction Economic processing of chalcopyrite ores through bioleaching, i.e., the mobilisation of metals from ore by microorganisms, has not been as successful as secondary copper sulphide leaching operations [1]. This chalcopyrite “problem” needs to be solved, as it is the dominant copper mineral in many low-grade copper deposits. This has resulted in large quantities of low-grade waste material being stockpiled or discarded in mining operations, as they are not economic to process, though they do contain massive quantities of metals (i.e., copper) simply due to their combined volume [1–3].
    [Show full text]
  • Abstract in PDF Format
    PGM Associations in Copper-Rich Sulphide Ore of the Oktyabr Deposit, Talnakh Deposit Group, Russia Olga A. Yakovleva1, Sergey M. Kozyrev1 and Oleg I. Oleshkevich2 1Institute Gipronickel JS, St. Petersburg, Russia 2Mining and Metallurgical Company “Noril’sk Nickel” JS, Noril’sk, Russia e-mail: [email protected] The PGM assemblages of the Cu-rich 6%; the Ni content ranges 0.8 to 1.3%, and the ratio sulphide ores occurring in the western exocontact Cu/S = 0.1-0.2. zone of the Talnakh intrusion and the Kharaelakh Pyrrhotite-chalcopyrite ore occurs at the massive orebody have been studied. Eleven ore top of ore horizons. The ore-mineral content ranges samples, weighing 20 to 200 kg, were processed 50 to 60%, and pyrrhotite amount is <15%. The ore using gravity and flotation-gravity techniques. As a grades 1.1 to 1.3% Ni, and the ratio Cu/S = 0.35- result, the gravity concentrates were obtained from 0.7. the ores and flotation products. In the gravity Chalcopyrite ore occurs at the top and on concentrates, more than 20,000 PGM grains were the flanks of the orebodies. The concentration of found and identified, using light microscopy and sulphides ranges 50 to 60%, and pyrrhotite amount EPMA. The textural and chemical characteristics of is <1%; the Ni content ranges 1.3 to 3.4%, and the PGM were documented, as well as the PGM ratio Cu/S = 0.8-0.9. distribution in different size fractions. Also, the The ore types are distinctly distinguished balance of Pt, Pd and Au distribution in ores and by the PGE content which directly depends on the process products and the PGM mass portions in chalcopyrite quantity, but not on the total sulphide various ore types were calculated.
    [Show full text]
  • 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]
  • Depositional Setting of Algoma-Type Banded Iron Formation Blandine Gourcerol, P Thurston, D Kontak, O Côté-Mantha, J Biczok
    Depositional Setting of Algoma-type Banded Iron Formation Blandine Gourcerol, P Thurston, D Kontak, O Côté-Mantha, J Biczok To cite this version: Blandine Gourcerol, P Thurston, D Kontak, O Côté-Mantha, J Biczok. Depositional Setting of Algoma-type Banded Iron Formation. Precambrian Research, Elsevier, 2016. hal-02283951 HAL Id: hal-02283951 https://hal-brgm.archives-ouvertes.fr/hal-02283951 Submitted on 11 Sep 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Depositional Setting of Algoma-type Banded Iron Formation B. Gourcerol, P.C. Thurston, D.J. Kontak, O. Côté-Mantha, J. Biczok PII: S0301-9268(16)30108-5 DOI: http://dx.doi.org/10.1016/j.precamres.2016.04.019 Reference: PRECAM 4501 To appear in: Precambrian Research Received Date: 26 September 2015 Revised Date: 21 January 2016 Accepted Date: 30 April 2016 Please cite this article as: B. Gourcerol, P.C. Thurston, D.J. Kontak, O. Côté-Mantha, J. Biczok, Depositional Setting of Algoma-type Banded Iron Formation, Precambrian Research (2016), doi: http://dx.doi.org/10.1016/j.precamres. 2016.04.019 This is a PDF file of an unedited manuscript that has been accepted for publication.
    [Show full text]
  • Minerals and Mineral Products in Our Bedroom Bed Hematite
    Minerals and Mineral Products in our Bedroom Make-Up Kit Muscovite Bed Talc Hematite: hinges, handles, Mica mattress springs Hematite: for color Chromite: chrome plating Bismuth Radio Barite Copper: wiring Plastic Pail Quartz: clock Mica Gold: connections Cassiterite: solder Toilet Bowl / Tub Closet Feldspar: porcelain Chromite: chrome plating Pyrolusite: coloring Hematite: hinges, handles (steel) Chromite: plumbing fixtures Quartz : mirror on door Copper: tubing Desk Toothpaste Hematite: hinges, handles (steel) Apatite: teeth Chromite: chrome plating Fluorite: toothpaste Mirror Rutile: to color false Hematite: handle, frame teeth yellow Chromite: plating Gold: fillings Gold: plating Cinnabar: fillings Quartz: mirror Towels Table Lamp Sphalerite: dyes Brass (an alloy of copper and Chromite: dyes zinc): base Quartz: bulb Water Pipe/Faucet/Shower bulb Wolframite: lamp filament Brass Copper: wiring Iron Nickel Minerals and Mineral Products in our Bedroom Chrome: stainless steel Bathroom Cleaner Department of Environment and Natural Resources Borax: abrasive, cleaner, and antiseptic MINES AND GEOSCIENCES BUREAU Deodorant Spray Can Cassiterite Chromite Copper Carpet Quartz Sphalerite: dyes Telephone Chromite: dyes Drinking Glasses Copper: wiring Sulfur: foam padding Quartz Chromite: plating Gold: red color Clock Silver: electronics Pentlandite: spring Graphite: batteries Refrigerator Quartz: glass, time keeper Hematite Television Chromite: stainless steel Chromite: plating Computer Galena Wolframite: monitor Wolframite: monitor Copper Copper:
    [Show full text]
  • Structure and Mineralization of Precambrian Rocks in the Galena-Roub Aix District, Black Hills, South Dakota
    Structure and Mineralization of Precambrian Rocks in the \ Galena-Roubaix District, Black Hills, South Dakota ( By R. W. BAYLEY » CONTRIBUTIONS TO ECONOMIC GEOLOGY V ' GEOLOGICAL SURVEY BULLETIN 1312-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 55 cents (paper cover) CONTENTS Page Abstract_ ____-_-_----_-----__--_-----_--_--.. El Introduction _________________________________ 1 Field methods_______-_____-_____-_____-__--_ 2 General geology.___-__--__-_--__-_--___._-_--_. 3 Stratigraphy. ___________________---__--__-__-.. 4 Metabasalt and chert.______-__-__-_____-_. 4 Graphitic schist and cherty ferruginous schist. 5 Metagraywacke, schist, and slate_ ___________ 6 Structure. ___________.-______-_-__-_-_-_-___-. 6 Distribution of gold. 7 Diamond drilling. __ 9 Magnetic survey. __ 10 Summary________ 14 References. -. ______ 15 ILLUSTEATIONS Page PLATE 1. Geologic map of the Galena-Roubaix district, Lawrence County, Black Hills, South Dakota.________________ In pocket FIGURE 1. Generalized geologic map of the northern Black Hills____-___ E2 2. Magnetic survey in the vicinity of U.S. Geological Survey diamond-drill hole 1__________________________________ 13 TABLE Page TABLIS 1. Results of core-sample analyses, U.S. Geological Survey diamond-drill hole 1, Galena-Roubaix district.____________ Ell ra CONTRIBUTIONS TO ECONOMIC GEOLOGY STRUCTURE AND MINERALIZATION OF PRECAMBRIAN ROCKS IN THE GALENA-ROUB AIX DISTRICT, BLACK HILLS, SOUTH DAKOTA ByK.W.BAYLEY ABSTRACT The Galena-Roubaix district is underlain chiefly by tightly folded and mod­ erately metamorphosed sedimentary and volcanic rocks of Precambrian age.
    [Show full text]
  • Modeling the Shape of Ions in Pyrite-Type Crystals
    Crystals 2014, 4, 390-403; doi:10.3390/cryst4030390 OPEN ACCESS crystals ISSN 2073-4352 www.mdpi.com/journal/crystals Article Modeling the Shape of Ions in Pyrite-Type Crystals Mario Birkholz IHP, Im Technologiepark 25, 15236 Frankfurt (Oder), Germany; E-Mail: [email protected]; Tel.: +49-335-56250 Received: 13 April 2014; in revised form: 22 August 2014 / Accepted: 26 August 2014 / Published: 3 September 2014 Abstract: The geometrical shape of ions in crystals and the concept of ionic radii are re-considered. The re-investigation is motivated by the fact that a spherical modelling is justified for p valence shell ions on cubic lattice sites only. For the majority of point groups, however, the ionic radius must be assumed to be an anisotropic quantity. An appropriate modelling of p valence ions then has to be performed by ellipsoids. The approach is tested for pyrite-structured dichalcogenides MX2, with chalcogen ions X = O, S, Se and Te. The latter are found to exhibit the shape of ellipsoids being compressed along the <111> symmetry axes, with two radii r|| and describing their spatial extension. Based on this ansatz, accurate interatomic M–X distances can be derived and a consistent geometrical model emerges for pyrite-structured compounds. Remarkably, the volumes of chalcogen ions are found to vary only little in different MX2 compounds, suggesting the ionic volume rather than the ionic radius to behave as a crystal-chemical constant. Keywords: ionic radius; ionic shape; bonding distance; ionic volume; pyrite-type compounds; di-chalcogenides; di-oxides; di-sulfides; di-selenides; di-tellurides 1.
    [Show full text]
  • Pyrite Roasting, an Alternative to Sulphur Burning
    The Southern African Institute of Mining and Metallurgy Sulphur and Sulphuric Acid Conference 2009 M Runkel and P Sturm PYRITE ROASTING, AN ALTERNATIVE TO SULPHUR BURNING M Runkel and P Sturm Outotec GmbH, Oberursel GERMANY Abstract The roasting of sulphide ores and concentrates is often the first step in the production of metals or chemicals. In many processes, the production of sulphuric acid is viewed as a by-product, while in some plants production is an important economic factor. Regardless of the purpose, a pyrite roasting plant consists of mainly three plant sections: roasting, gas cleaning and sulphuric acid. With the addition of air, the pyrite concentrates are transformed into solid oxides and gaseous sulphur dioxide at temperatures of 600 - 1000° C. After cleaning and cooling, the sulphur dioxide in the roasting gas is further processed to sulphuric acid. Two types of reactors are used depending on the application: stationary or circulating fluid bed . For over 60 years, Outotec has progressively been developing the principle of fluidised bed technology in several different reactor types for a multitude of process applications. The versatility of the fluidised bed reactor system has manifested itself in the treatment of minerals, including solid fuels, and for metallurgical processes both in the ferrous and non-ferrous fields. Process applications have included roasting, calcining, combustion and charring of coals, as well as off-gas treatment. This paper provides a summary of the pyrite roasting technology currently used along with a simple cost comparison of pyrite roasting and sulphur burning processes. Introduction Pyrite roasting and sulphur burning plants are built for the production of sulphuric acid.
    [Show full text]