35Th International Geological Congress
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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 -
New Mineral Names*,†
American Mineralogist, Volume 106, pages 1360–1364, 2021 New Mineral Names*,† Dmitriy I. Belakovskiy1, and Yulia Uvarova2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2CSIRO Mineral Resources, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia In this issue This New Mineral Names has entries for 11 new species, including 7 minerals of jahnsite group: jahnsite- (NaMnMg), jahnsite-(NaMnMn), jahnsite-(CaMnZn), jahnsite-(MnMnFe), jahnsite-(MnMnMg), jahnsite- (MnMnZn), and whiteite-(MnMnMg); lasnierite, manganflurlite (with a new data for flurlite), tewite, and wumuite. Lasnierite* the LA-ICP-MS analysis, but their concentrations were below detec- B. Rondeau, B. Devouard, D. Jacob, P. Roussel, N. Stephant, C. Boulet, tion limits. The empirical formula is (Ca0.59Sr0.37)Ʃ0.96(Mg1.42Fe0.54)Ʃ1.96 V. Mollé, M. Corre, E. Fritsch, C. Ferraris, and G.C. Parodi (2019) Al0.87(P2.99Si0.01)Ʃ3.00(O11.41F0.59)Ʃ12 based on 12 (O+F) pfu. The strongest lines of the calculated powder X-ray diffraction pattern are [dcalc Å (I%calc; Lasnierite, (Ca,Sr)(Mg,Fe)2Al(PO4)3, a new phosphate accompany- ing lazulite from Mt. Ibity, Madagascar: an example of structural hkl)]: 4.421 (83; 040), 3.802 (63, 131), 3.706 (100; 022), 3.305 (99; 141), characterization from dynamic refinement of precession electron 2.890 (90; 211), 2.781 (69; 221), 2.772 (67; 061), 2.601 (97; 023). It diffraction data on submicrometer sample. European Journal of was not possible to perform powder nor single-crystal X-ray diffraction Mineralogy, 31(2), 379–388. -
Gatehouseite Mn (PO4)2(OH)4
2+ Gatehouseite Mn5 (PO4)2(OH)4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. As bladelike crystals, with prominent {001}, {110}, {102}, elongated along [010], to 100 µm, in radiating to divergent groups and overgrowths on arsenoclasite. Twinning: On {001}, contact twins. Physical Properties: Cleavage: On {010}, distinct. Fracture: Splintery. Hardness = ∼4 D(meas.) = n.d. D(calc.) = 3.74 Optical Properties: Transparent. Color: Pale brownish orange to yellow or pale yellow. Streak: Pale yellow. Luster: Adamantine. Optical Class: Biaxial. Pleochroism: Distinct; brown to nearly colorless. Orientation: Parallel extinction; length-slow. α = 1.74(1) β = n.d. γ = 1.76(1) 2V(meas.) = n.d. Cell Data: Space Group: P 212121 (probable). a = 9.097(2) b = 5.693(2) c = 18.002(10) Z=4 X-ray Powder Pattern: Iron Monarch quarry, Australia. 2.90 (100), 2.702 (80), 2.853 (70), 2.802 (50), 2.022 (15), 1.608 (15), 4.483 (10) Chemistry: (1) (2) (3) SO3 0.10 P2O5 22.18 23.05 26.65 As2O5 3.58 3.32 V2O5 0.38 Al2O3 0.10 FeO 0.19 0.32 MnO 64.42 63.34 66.59 CuO 0.03 0.04 ZnO 0.03 PbO 0.05 0.05 H2O [6.44] [6.43] 6.76 Total [97.40] [96.65] 100.00 (1) Iron Monarch quarry, Australia; by electron microprobe, total Mn as MnO, total Fe as FeO, H2O calculated for 4(OH); corresponds to Mn5.09Fe0.01Al0.01[(P0.87As0.08V0.01)Σ=0.96O4]2(OH)4. -
Thirty-Seventh List of New Mineral Names. Part 1" A-L
Thirty-seventh list of new mineral names. Part 1" A-L A. M. CLARK Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK AND V. D. C. DALTRYt Department of Geology and Mineralogy, University of Natal, Private Bag XO1, Scottsville, Pietermaritzburg 3209, South Africa THE present list is divided into two sections; the pegmatites at Mount Alluaiv, Lovozero section M-Z will follow in the next issue. Those Complex, Kola Peninsula, Russia. names representing valid species, accredited by the Na19(Ca,Mn)6(Ti,Nb)3Si26074C1.H20. Trigonal, IMA Commission on New Minerals and Mineral space group R3m, a 14.046, c 60.60 A, Z = 6. Names, are shown in bold type. Dmeas' 2.76, Dc~ac. 2.78 g/cm3, co 1.618, ~ 1.626. Named for the locality. Abenakiite-(Ce). A.M. McDonald, G.Y. Chat and Altisite. A.P. Khomyakov, G.N. Nechelyustov, G. J.D. Grice. 1994. Can. Min. 32, 843. Poudrette Ferraris and G. Ivalgi, 1994. Zap. Vses. Min. Quarry, Mont Saint-Hilaire, Quebec, Canada. Obschch., 123, 82 [Russian]. Frpm peralkaline Na26REE(SiO3)6(P04)6(C03)6(S02)O. Trigonal, pegmatites at Oleny Stream, SE Khibina alkaline a 16.018, c 19.761 A, Z = 3. Named after the massif, Kola Peninsula, Russia. Monoclinic, a Abenaki Indian tribe. 10.37, b 16.32, c 9.16 ,~, l~ 105.6 ~ Z= 2. Named Abswurmbachite. T. Reinecke, E. Tillmanns and for the chemical elements A1, Ti and Si. H.-J. Bernhardt, 1991. Neues Jahrb. Min. Abh., Ankangite. M. Xiong, Z.-S. -
Design Rules for Discovering 2D Materials from 3D Crystals
Design Rules for Discovering 2D Materials from 3D Crystals by Eleanor Lyons Brightbill Collaborators: Tyler W. Farnsworth, Adam H. Woomer, Patrick C. O'Brien, Kaci L. Kuntz Senior Honors Thesis Chemistry University of North Carolina at Chapel Hill April 7th, 2016 Approved: ___________________________ Dr Scott Warren, Thesis Advisor Dr Wei You, Reader Dr. Todd Austell, Reader Abstract Two-dimensional (2D) materials are championed as potential components for novel technologies due to the extreme change in properties that often accompanies a transition from the bulk to a quantum-confined state. While the incredible properties of existing 2D materials have been investigated for numerous applications, the current library of stable 2D materials is limited to a relatively small number of material systems, and attempts to identify novel 2D materials have found only a small subset of potential 2D material precursors. Here I present a rigorous, yet simple, set of criteria to identify 3D crystals that may be exfoliated into stable 2D sheets and apply these criteria to a database of naturally occurring layered minerals. These design rules harness two fundamental properties of crystals—Mohs hardness and melting point—to enable a rapid and effective approach to identify candidates for exfoliation. It is shown that, in layered systems, Mohs hardness is a predictor of inter-layer (out-of-plane) bond strength while melting point is a measure of intra-layer (in-plane) bond strength. This concept is demonstrated by using liquid exfoliation to produce novel 2D materials from layered minerals that have a Mohs hardness less than 3, with relative success of exfoliation (such as yield and flake size) dependent on melting point. -
Shigaite Namn Al3(SO4)
2+ • Shigaite NaMn6 Al3(SO4)2(OH)18 12H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 3. Hexagonal tabular crystals, to 2 cm, may be in groups; as thin films and fracture coatings. Twinning: On {0001}. Physical Properties: Cleavage: On {0001}, perfect. Tenacity: Moderately flexible. Hardness = ∼2 D(meas.) = 2.32 D(calc.) = 2.35 Optical Properties: Semitransparent. Color: Pale yellow, bright yellow, golden yellow, burnt orange; brownish yellow if included, brown to black if altered. Streak: Very pale yellow to white. Luster: Vitreous to dull. Optical Class: Uniaxial (–). Pleochroism: Distinct; O = yellow; E = very pale yellow. Absorption: O > E. ω = 1.546 = n.d. Cell Data: Space Group: R3. a = 9.51–9.52 c = 32.83–33.074 Z = 3 X-ray Powder Pattern: Ioi mine, Japan. 10.89 (100), 5.47 (90), 2.457 (90), 3.664 (80), 2.198 (60), 1.944 (60), 4.36 (40) Chemistry: (1) (2) (3) SO3 13.6 12.75 13.95 Al2O3 15.3 11.8 13.32 Fe2O3 0.9 2.6 MnO 41.7 42.1 37.08 MgO 0.25 Na2O n.d. n.d. 2.70 H2O 28.0 [30.5] 32.95 Total 99.5 [100.0] 100.00 (1) Ioi mine,Japan; by electron microprobe, total Fe as Fe2O3, total Mn as MnO, H2Oby TGA-EGA. (2) Iron Monarch quarry, Australia; by electron microprobe, average of two analyses, • total Fe as Fe2O3, total Mn as MnO, H2O by difference. (3) NaMn6Al3(SO4)2(OH)18 12H2O. Occurrence: A rare secondary mineral in metamorphosed manganese ore deposits. -
Description and Unique Crystal-Structure of Waterhouseite, a New Hydroxy Manganese Phosphate Species from the Iron Monarch Deposit, Middleback Ranges, South Australia
1401 The Canadian Mineralogist Vol. 43, pp. 1401-1410 (2005) DESCRIPTION AND UNIQUE CRYSTAL-STRUCTURE OF WATERHOUSEITE, A NEW HYDROXY MANGANESE PHOSPHATE SPECIES FROM THE IRON MONARCH DEPOSIT, MIDDLEBACK RANGES, SOUTH AUSTRALIA ALLAN PRING§ Department of Mineralogy, South Australian Museum, North Terrace, Adelaide, South Australia 5000, and School of Earth & Environmental Science, University of Adelaide, Adelaide, S.A. 5005, Australia UWE KOLITSCH Institut für Mineralogie und Kristallographie, Geozentrum, Universität Wien, Althanstr. 14, A–1090 Wien, Austria WILLIAM D. BIRCH Department of Mineralogy, Museum of Victoria, GPO Box 666E, Melbourne, Victoria, 3000, Australia ABSTRACT Waterhouseite from the Iron Monarch mine, Iron Knob, South Australia, is a new hydroxy manganese phosphate species that has a unique crystal-structure. The mineral was found in a carbonate-rich zone with gatehouseite, seamanite, rhodochrosite, shigaite, barite, hausmannite and hematite. It occurs as divergent sprays of orange-brown to dark brown bladed crystals up to 1 mm in length but only up to 20 m in thickness. The crystals are transparent with a pearly luster on cleavages, but it is vitreous to pearly on the tabular faces. The mineral is brittle, with a conchoidal fracture and a yellowish brown streak. There is a perfect cleavage on (100) and a probable cleavage on (001). The crystals show the principal forms {100} (dominant), {010}, {011} and {001}. All crystals are twinned on (100) by non-merohedry. The Mohs hardness is estimated to be ~4, and the measured density is 3.55(5) g/cm3 (calculated density is 3.591 g/cm3). Crystals are biaxial negative and length-slow, with ␣ 1.730(3),  ~1.738 and ␥ 1.738(4), but 2V could not be measured. -
Waterhouseite Mn7(PO4)2(OH)8
Waterhouseite Mn7(PO4)2(OH)8 Crystal Data: Monoclinic. Point Group: 2/m. As divergent sprays of bladed crystals to 1.0 mm elongated along [001]. Pseudo-orthorhombic crystals display {100} (dominant), {010}, {011}, and {001}. Twinning: Contact twinning on (100). Physical Properties: Cleavage: Perfect on (100) and probable on (001). Fracture: Splintery to conchoidal. Tenacity: Brittle. Hardness = 4 D(meas.) = 3.55(5) D(calc.) = 3.59 Optical Properties: Transparent. Color: Resinous orange-brown to dark clove-brown. Streak: Yellowish brown. Luster: Vitreous to pearly on cleavage surfaces. Optical Class: Biaxial (-). α =1.730(3) β = ~1.738 γ = 1.738(4) 2V = ~ 0° Orientation: X = b, Y = a, Z = c. Pleochroism: X= pale brown, Y = brown-yellow, Z = pale brown. Absorption: Z = X > Y. Cell Data: Space Group: P21/c. a = 11.364(2) b = 5.570(1) c = 10.455(2) β = 96.61(3)° Z = 2 X-ray Powder Pattern: Iron Monarch mine, Middleback Ranges, Iron Knob, South Australia. 3.621 (100), 4.436 (70), 3.069 (50), 2.941(40), 2.780 (35), 2.890 (20), 2.842 (20) Chemistry: (1) MnO 69.70 ZnO 0.02 P2O5 17.37 As2O5 1.09 V2O5 0.50 H2O [9.49] Total 98.17 (1) Iron Monarch mine, Middleback Ranges, Iron Knob, South Australia; average of 7 electron microprobe analyses supplemented by Raman spectroscopy, H2O calculated from structure analysis; corresponds to Mn7.28[(P1.81As0.07V0.04)O4]1.92(OH)7.81O0.51. Occurrence: In cavities in the carbonate-rich beds of a Precambrian banded iron formation. -
35Th International Geological Congress
............................... 3 NO. 59 QUARTERLY NEWS BULLETIN ~ SEPTEMBER 2 0 1 6 VOLUME ..................... 35TH INTERNATIONAL GEOLOGICAL CONGRESS 27 AUGUST - 4 SEPTEMBER 2016 I CAPE TOWN, SOUTH AFRICA UCT du Toit lecture Pre-IGC field trips Mineral Scene ................................................................................................................................................................................................... GeoBulletin_Expression Form (A4)_OUTLINES CREATED.indd 1 2013/09/13 03:14:51 PM 3535THTH INTERNATIONALINTERNATIONAL GEOLOGICALGEOLOGICAL CONGRESSCONGRESS 2727 AUGUST AUGUST - 4- 4SEPTEMBER SEPTEMBER 2016 2016 | | CAPE CAPE TOWN, TOWN, SOUTH SOUTH AFRICA AFRICA TheThe International International Geological Geological Congress Congress (IGC) (IGC) is isthe the principal principal event event of of the the International International Union Union of of Geological Geological SciencesSciences (IUGS), (IUGS), one one of of the the largest largest and and most most active active non-governmental non-governmental scienti scientificfi organizationsc organizations in inthe the world. world. TheThe IUGS IUGS promotes promotes and and encourages encourages the the study study of of geological geological phenomena, phenomena, especially especially those those of of worldwide worldwide facilitates international and interdisciplinary signisignificance,ficance, and and supports supports and and facilitates international and interdisciplinarycooperation cooperation in inthe the earth earth sciences.sciences. -
IMA–CNMNC Approved Mineral Symbols
Mineralogical Magazine (2021), 85, 291–320 doi:10.1180/mgm.2021.43 Article IMA–CNMNC approved mineral symbols Laurence N. Warr* Institute of Geography and Geology, University of Greifswald, 17487 Greifswald, Germany Abstract Several text symbol lists for common rock-forming minerals have been published over the last 40 years, but no internationally agreed standard has yet been established. This contribution presents the first International Mineralogical Association (IMA) Commission on New Minerals, Nomenclature and Classification (CNMNC) approved collection of 5744 mineral name abbreviations by combining four methods of nomenclature based on the Kretz symbol approach. The collection incorporates 991 previously defined abbreviations for mineral groups and species and presents a further 4753 new symbols that cover all currently listed IMA minerals. Adopting IMA– CNMNC approved symbols is considered a necessary step in standardising abbreviations by employing a system compatible with that used for symbolising the chemical elements. Keywords: nomenclature, mineral names, symbols, abbreviations, groups, species, elements, IMA, CNMNC (Received 28 November 2020; accepted 14 May 2021; Accepted Manuscript published online: 18 May 2021; Associate Editor: Anthony R Kampf) Introduction used collection proposed by Whitney and Evans (2010). Despite the availability of recommended abbreviations for the commonly Using text symbols for abbreviating the scientific names of the studied mineral species, to date < 18% of mineral names recog- chemical elements -
New Data on Minerals
Russian Academy of Science Fersman Mineralogical Museum Volume 39 New Data on Minerals Founded in 1907 Moscow Ocean Pictures Ltd. 2004 ISBN 5900395626 UDC 549 New Data on Minerals. Moscow.: Ocean Pictures, 2004. volume 39, 172 pages, 92 color images. EditorinChief Margarita I. Novgorodova. Publication of Fersman Mineralogical Museum, Russian Academy of Science. Articles of the volume give a new data on komarovite series minerals, jarandolite, kalsilite from Khibiny massif, pres- ents a description of a new occurrence of nikelalumite, followed by articles on gemnetic mineralogy of lamprophyl- lite barytolamprophyllite series minerals from IujaVritemalignite complex of burbankite group and mineral com- position of raremetaluranium, berrillium with emerald deposits in Kuu granite massif of Central Kazakhstan. Another group of article dwells on crystal chemistry and chemical properties of minerals: stacking disorder of zinc sulfide crystals from Black Smoker chimneys, silver forms in galena from Dalnegorsk, tetragonal Cu21S in recent hydrothermal ores of MidAtlantic Ridge, ontogeny of spiralsplit pyrite crystals from Kursk magnetic Anomaly. Museum collection section of the volume consist of articles devoted to Faberge lapidary and nephrite caved sculp- tures from Fersman Mineralogical Museum. The volume is of interest for mineralogists, geochemists, geologists, and to museum curators, collectors and ama- teurs of minerals. EditorinChief Margarita I .Novgorodova, Doctor in Science, Professor EditorinChief of the volume: Elena A.Borisova, Ph.D Editorial Board Moisei D. Dorfman, Doctor in Science Svetlana N. Nenasheva, Ph.D Marianna B. Chistyakova, Ph.D Elena N. Matvienko, Ph.D Мichael Е. Generalov, Ph.D N.A.Sokolova — Secretary Translators: Dmitrii Belakovskii, Yiulia Belovistkaya, Il'ya Kubancev, Victor Zubarev Photo: Michael B. -
Arsenoclasite Mn5 (Aso4)2(OH)4 C 2001-2005 Mineral Data Publishing, Version 1
2+ Arsenoclasite Mn5 (AsO4)2(OH)4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. Crystals rare, to 5 mm; granular or massive. Physical Properties: Cleavage: Perfect on {010}. Hardness = 5–6 D(meas.) = 4.16 D(calc.) = 4.21 Optical Properties: Translucent. Color: Red, dark orange-brown. Optical Class: Biaxial (–). Orientation: X = b; Y = a; Z = c. α = 1.787 β = 1.810 γ = 1.816 2V(meas.) = 53◦260 Cell Data: Space Group: P 212121. a = 18.29(2) b = 5.75(1) c = 9.31(2) Z = 4 X-ray Powder Pattern: L˚angban,Sweden. 2.933 (100), 2.739 (75), 4.55 (70), 2.835 (70), 3.057 (60), 1.631 (50), 4.92 (45) Chemistry: (1) (2) (3) SO3 0.23 P2O5 1.37 As2O5 36.96 34.10 37.04 Al2O3 0.17 FeO trace 0.03 MnO 55.01 55.74 57.16 CuO 0.57 0.05 ZnO 0.11 PbO 0.15 MgO 0.87 BaO 0.11 H2O 5.90 [5.85] 5.80 Total 99.42 [97.80] 100.00 (1) L˚angban, Sweden. (2) Iron Monarch quarry, Australia; by electron microprobe, H2O calculated for 2H2O; corresponding to Mn4.74Al0.02[(As0.90P0.06S0.01)Σ=0.97O4]2(OH)4. (3) Mn5(AsO4)2(OH)4. Occurrence: A rare fissure mineral in a metamorphosed Fe–Mn orebody (L˚angban,Sweden); in a sedimentary Fe–Mn deposit (Iron Monarch quarry, Australia). Association: Sarkinite, adelite, allactite, calcite, dolomite, hausmannite (L˚angban,Sweden); gatehouseite, shigaite, hematite, hausmannite, barite, manganoan ferroan calcite (Iron Monarch quarry, Australia).