Synthesis of Two-Dimensional Single-Crystal Berzelianite Nanosheets and Nanoplates with Near-Infrared Optical Absorption†
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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 -
New Occurrence of Kruťaite and Petříčekite at the Former Uranium Mine Slavkovice, Western Moravia, Czech Republic
250 Bull Mineral Petrolog 26, 2, 2018. ISSN 2570-7337 (print); 2570-7345 (online) PŮVODNÍ PRÁCE/ORIGINAL PAPER New occurrence of kruťaite and petříčekite at the former uranium mine Slavkovice, western Moravia, Czech Republic Tomáš FLÉGR1)*, Jiří SeJkora2), Pavel Škácha2,3) and Zdeněk dolníček2) 1)Department of Geology, Masaryk University, Kotlářská 267/2, 611 37 Brno; *e-mail:[email protected] 2)Department of Mineralogy and Petrology, National Museum, Cirkusová 1740, 193 00 Prague 9 3)Mining Museum Příbram, Hynka Kličky place 293, 261 01 Příbram VI Flégr T, SeJkora J, Škácha P, dolníček Z (2018) New occurrence of kruťaite and petříčekite at the former uranium mine Slavkovice, western Moravia, Czech Republic. Bull Mineral Petrolog 26(2): 250-258. ISSN 2570-7337 Abstract Two rare copper diselenides, kruťaite and petříčekite, were found in two museum samples of vein fillings from the uranium mine Slavkovice, western Moravia (Czech Republic). Kruťaite occurs as small isometric isolated euhedral to subhedral zoned crystals enclosed and partly replaced by umangite. Petříčekite forms small elongated or isometric inclusions enclosed by kruťaite and other Cu-selenides. Optical data, Raman spectra and chemical composition of both phases are specified in this paper. Kruťaite contains elevated contents of Co (up to 0.15apfu ) and Ni (up to 0.09 apfu), whereas petříčekite is Ni-Co free and enriched in Fe (up to 0.25 apfu). Both phases seem to be the oldest selenides in the given assemblage, and are associated with umangite, athabascaite, eskebornite, klockmannite, bukovite, urani- nite, chalcopyrite, calcite and hematite. The studied ore assemblage originated at temperature not exceeding ca. -
Tyrrellite (Cu, Co, Ni)3Se4 C 2001-2005 Mineral Data Publishing, Version 1
Tyrrellite (Cu, Co, Ni)3Se4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m 32/m. Rounded grains and subhedral cubes. Physical Properties: Cleavage: {001}, poor. Fracture: Conchoidal. Tenacity: Brittle. Hardness = ∼3.5 VHN = 343–368 (100 g load). D(meas.) = n.d. D(calc.) = 6.6(2) Optical Properties: Opaque. Color: Pale bronze; pale brassy bronze in reflected light. Streak: Black. Luster: Metallic. R: (400) 41.8, (420) 42.6, (440) 43.5, (460) 44.4, (480) 45.0, (500) 45.5, (520) 45.9, (540) 46.3, (560) 46.5, (580) 46.8, (600) 47.0, (620) 47.3, (640) 47.5, (660) 47.6, (680) 47.8, (700) 48.0 Cell Data: Space Group: Fm3m. a = 10.005(4) Z = 8 X-ray Powder Pattern: Ato Bay, Canada. 1.769 (10), 2.501 (9), 2.886 (7), 3.016 (6), 1.926 (6), 5.780 (4), 3.537 (4) Chemistry: (1) (2) Cu 12.7 13.7 Co 17.7 11.6 Ni 6.9 12.0 Se 62.4 62.0 Total 99.7 99.3 (1) Beaverlodge district [sic; Goldfields district], Canada; by electron microprobe, corresponding to Cu1.01Co1.52Ni0.60Se4.00. (2) Hope’s Nose, England; by electron microprobe; corresponding to Cu1.10Ni1.04Co1.00Se4.00. Mineral Group: Linnaeite group. Occurrence: With other selenides, as the youngest hydrothermal replacements and open space fillings in sheared Precambrian rocks, which also contain uraninite deposits (Goldfields district, Canada). Association: Umangite, klockmannite, clausthalite, pyrite, hematite, chalcopyrite, chalcomenite (Ato Bay, Canada); berzelianite, eucairite, crookesite, ferroselite, bukovite, kruˇtaite, athabascaite, calcite, dolomite (Petrovice deposit, Czech Republic). -
Minerals Named After Scientists
Dr. John Andraos, http://www.careerchem.com/NAMED/Minerals.pdf 1 MINERALS NAMED AFTER PEOPLE AND PLACES © Dr. John Andraos, 2003-2011 Department of Chemistry, York University 4700 Keele Street, Toronto, ONTARIO M3J 1P3, CANADA For suggestions, corrections, additional information, and comments please send e-mails to [email protected] http://www.chem.yorku.ca/NAMED/ PEOPLE MINERAL PERSON OR PLACE DESCRIPTION Abelsonite ABELSON, Philip Hauge (1913 - ?) geochemist Abenakiite ABENAKI people, Quebec, Canada Abernathyite ABERNATHY, Jess Mine operator American, b. ? Abswurmbachite ABS-WURMBACH, IRMGARD (1938 - ) mineralogist German, b. ? Adamite ADAM, Gilbert Joseph Zn3(AsO3)2 H2O (1795 - 1881) mineralogist French, b. ? Aegirine AEGIR, Scandinavian god of the sea Afwillite WILLIAMS, Alpheus Fuller (1874 - ?) mine operator DeBeers Consolidated Mines, Kimberley, South Africa Agrellite AGRELL, Stuart O. (? - 1996) mineralogist British, b. ? Agrinierite AGRINIER, Henri (1928 - 1971) mineralogist French, b. ? Aguilarite AGUILAR, P. Superintendent of San Carlos mine, Guanajuato, Mexico Mexican, b. ? Aikenite 2 PbS Cu2S Bi2S5 Andersonite ANDERSON, Dr. John Andraos, http://www.careerchem.com/NAMED/Minerals.pdf 2 Andradite ANDRADA e Silva, Jose B. Ca3Fe2(SiO4)3 de (? - 1838) geologist Brazilian, b. ? Arfvedsonite ARFVEDSON, Johann August (1792 - 1841) Swedish, b. Skagerholms- Bruk, Skaraborgs-Län, Sweden Arrhenite ARRHENIUS, Svante Silico-tantalate of Y, Ce, Zr, (1859 - 1927) Al, Fe, Ca, Be Swedish, b. Wijk, near Uppsala, Sweden Avogardrite AVOGADRO, Lorenzo KBF4, CsBF4 Romano Amedeo Carlo (1776 - 1856) Italian, b. Turin, Italy Babingtonite (Ca, Fe, Mn)SiO3 Fe2(SiO3)3 Becquerelite BECQUEREL, Antoine 4 UO3 7 H2O Henri César (1852 - 1908) French b. Paris, France Berzelianite BERZELIUS, Jöns Jakob Cu2Se (1779 - 1848) Swedish, b. -
Revision 2 of Ms. 5419 Page 1 Time's Arrow in the Trees of Life And
Revision 2 of Ms. 5419 Time’s Arrow in the Trees of Life and Minerals Peter J. Heaney1,* 1Dept. of Geosciences, Penn State University, University Park, PA 16802 *To whom correspondence should be addressed: [email protected] Page 1 Revision 2 of Ms. 5419 1 ABSTRACT 2 Charles Darwin analogized the diversification of species to a Tree of Life. 3 This metaphor aligns precisely with the taxonomic system that Linnaeus developed 4 a century earlier to classify living species, because an underlying mechanism – 5 natural selection – has driven the evolution of new organisms over vast timescales. 6 On the other hand, the efforts of Linnaeus to extend his “universal” organizing 7 system to minerals has been regarded as an epistemological misfire that was 8 properly abandoned by the late nineteenth century. 9 The mineral taxonomies proposed in the wake of Linnaeus can be 10 distinguished by their focus on external character (Werner), crystallography (Haüy), 11 or chemistry (Berzelius). This article appraises the competition among these 12 systems and posits that the chemistry-based Berzelian taxonomy, as embedded 13 within the widely adopted system of James Dwight Dana, ultimately triumphed 14 because it reflects Earth’s episodic but persistent progression with respect to 15 chemical differentiation. In this context, Hazen et al.’s (2008) pioneering work in 16 mineral evolution reveals that even the temporal character of the phylogenetic Tree 17 of Life is rooted within a Danan framework for ordering minerals. 18 19 Page 1 Revision 2 of Ms. 5419 20 INTRODUCTION 21 In an essay dedicated to the evolutionary biologist Ernst Mayr, Stephen Jay 22 Gould (2000) expresses his indignation at the sheer luckiness of Carolus Linnaeus 23 (1707-1778; Fig. -
Eskebornite, Two Canadian Occurrences
ESKEBORNITE,TWO CANADIAN OCCURRENCES D.C. HARRIS* am E.A.T.BURKE *r, AssrRAcr The flnt Canadian occurrenceof eskebomitefrom Martin Lake and the Eagle Groug Lake Athabaskaare4 Northern Saskatchewanis reported.Electron microprobe agalysesshow that the formula is cuFese2.The r-ray powdet difiraction pattems are identical to that of eskebornitefrom Tilkerode, Germany,the type locality, Eskeborniteocrurs as island remnantsin, and replac'edby,'u,rnangite'which occurs in pitchblendeores in t}le basa.ltof the Martin formaiion and in granitizedmafic rocls of the Eaglegroup. The mineral can be readily synthesizedat 500"e from pure elements in evacuatedsilica glasstubes, Reflectance and micro-indentationhardness in."r*u**o are given. IlvrnonucttoN Eskebomite, a copper iron selenide, was first discovered and namd by P. Ramdohr in 1949 while studying the selenide minerals from dre Tilkerode area, Harz Mountain, Germany. The mineral has also been reported from Sierra de Cacheuta and Sierra de lJmango, Argentina (Tischendorf 1960). More recentlyo other occurrences of eskebornite have been described: by Kvadek et al. (1965) in the selenide paragenesis at the slavkovice locality in the Bohemian and Moravian Highlands, czecho- slovakia; and by Agrinier et aI. (1967) in veins of pitchblende at Cha- m6anq Puy-de-D6me, France. Earley (1950) and Tischendorf (195g, 1960) made.observations on eskebornite from the Tilkerode locality, but, even today, certain data are still lacking in the characterization of eskebomitg in particular its crystal- lographic symmetry. The purpose of this paper is to record the first occurrence of eskebomite in Canada and to present electron microprobe analyses, reflectance and micro-indentation hardness measurements. GrNsRAr. -
Chrisstanleyite Ag2pd3se4 C 2001-2005 Mineral Data Publishing, Version 1
Chrisstanleyite Ag2Pd3Se4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m or 2. Anhedral crystals, to several hundred µm, aggregated in grains. Twinning: Fine polysynthetic and parquetlike, characteristic. Physical Properties: Tenacity: Slightly brittle. Hardness = ∼5 VHN = 371–421, 395 average (100 g load), D(meas.) = n.d. D(calc.) = 8.30 Optical Properties: Opaque. Color: Silvery gray. Streak: Black. Luster: Metallic. Optical Class: Biaxial. Pleochroism: Slight; pale buff to slightly gray-green buff. Anisotropism: Moderate; rose-brown, gray-green, pale bluish gray, dark steel-blue. Bireflectance: Weak to moderate. R1–R2: (400) 35.6–43.3, (420) 36.8–44.2, (440) 37.8–45.3, (460) 39.1–46.7, (480) 40.0–47.5, (500) 41.1–48.0, (520) 42.1–48.5, (540) 42.9–48.7, (560) 43.5–49.1, (580) 44.1–49.3, (600) 44.4–49.5, (620) 44.6–49.6, (640) 44.5–49.3, (660) 44.4–49.2, (680) 44.2–49.1, (700) 44.0–49.0 Cell Data: Space Group: P 21/m or P 21. a = 6.350(6) b = 10.387(4) c = 5.683(3) β = 114.90(5)◦ Z=2 X-ray Powder Pattern: Hope’s Nose, England. 2.742 (100), 1.956 (100), 2.688 (80), 2.868 (50b), 2.367 (50), 1.829 (30), 2.521 (20) Chemistry: (1) (2) (3) Pd 37.64 35.48 37.52 Pt 0.70 Hg 0.36 Ag 25.09 24.07 25.36 Cu 0.18 2.05 Se 36.39 38.50 37.12 Total 99.30 101.16 100.00 (1) Hope’s Nose, England; by electron microprobe, average of 26 analyses; corresponding to (Ag2.01Cu0.02)Σ=2.03Pd3.02Se3.95. -
European Journal of Mineralogy
Title Grundmannite, CuBiSe<SUB>2</SUB>, the Se-analogue of emplectite, a new mineral from the El Dragón mine, Potosí, Bolivia Authors Förster, Hans-Jürgen; Bindi, L; Stanley, Christopher Date Submitted 2016-05-04 European Journal of Mineralogy Composition and crystal structure of grundmannite, CuBiSe2, the Se-analogue of emplectite, a new mineral from the El Dragόn mine, Potosí, Bolivia --Manuscript Draft-- Manuscript Number: Article Type: Research paper Full Title: Composition and crystal structure of grundmannite, CuBiSe2, the Se-analogue of emplectite, a new mineral from the El Dragόn mine, Potosí, Bolivia Short Title: Composition and crystal structure of grundmannite, CuBiSe2, Corresponding Author: Hans-Jürgen Förster Deutsches GeoForschungsZentrum GFZ Potsdam, GERMANY Corresponding Author E-Mail: [email protected] Order of Authors: Hans-Jürgen Förster Luca Bindi Chris J. Stanley Abstract: Grundmannite, ideally CuBiSe2, is a new mineral species from the El Dragόn mine, Department of Potosí, Bolivia. It is either filling small shrinkage cracks or interstices in brecciated kruta'ite−penroseite solid solutions or forms independent grains in the matrix. Grain size of the anhedral to subhedral crystals is usually in the range 50−150 µm, but may approach 250 µm. Grundmannite is usually intergrown with watkinsonite and clausthalite; other minerals occasionally being in intimate grain-boundary contact comprise quartz, dolomite, native gold, eskebornite, umangite, klockmannite, Co-rich penroseite, and three unnamed phases of the Cu−Bi−Hg−Pb−Se system, among which is an as-yet uncharacterizedspecies with the ideal composition Cu4Pb2HgBi4Se11. Eldragόnite and petrovicite rarely precipitated in the neighborhood of CuBiSe2. Grundmannite is non-fluorescent, black and opaque with a metallic luster and black streak. -
Selenium Minerals and the Recovery of Selenium from Copper Refinery Anode Slimes by C
http://dx.doi.org/10.17159/2411-9717/2016/v116n6a16 Selenium minerals and the recovery of selenium from copper refinery anode slimes by C. Wang*, S. Li*, H. Wang*, and J. Fu* and genesis of native selenium from Yutangba, #65'272 Enshi City, Hubei Province, China in 2004, and pointed out, from the different forms of native Since it was first identified in 1817, selenium has received considerable Se, that selenium can be interest. Native selenium and a few selenium minerals were discovered several decades later. With the increasing number of selenium minerals, activated,transformed, remobilized, and the occurrence of selenium minerals became the focus of much research. A enriched at sites such as in the unsaturated great number of selenium deposits were reported all over the world, subsurface zone or in the saturated zone (Zhu although few independent selenium deposits were discovered. Selenium is et al., 2005). The transport and deposition of obtained mainly as a byproduct of other metals, and is produced primarily selenium in felsic volcanic-hosted massive from the anode mud of copper refineries. This paper presents a compre- sulphide deposits of the Yukon Territory, hensive review of selenium minerals, as well as the treatment of copper Canada was studied and reported by Layton- refinery anode slimes for the recovery of selenium. Our focus is on the Matthews et al. (2005). selenium minerals, including their discovery and occurrence, and the Selenium is a comparatively rare and distribution of selenium resources. In addition, the main methods of greatly dispersed element. The average recovering selenium from copper anode slimes are summarized. -
Eskebornite Cufese2 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Tetragonal, Pseudocubic
Eskebornite CuFeSe2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal, pseudocubic. Point Group: 42m. Crystals thick tabular, to 1 mm; massive, typically intergrown with other selenides. Physical Properties: Cleavage: {001}, perfect. Hardness = 3–3.5 VHN = 155–252, 204 average (15 g load). D(meas.) = 5.35 D(calc.) = 5.44 Distinctly magnetic. Optical Properties: Opaque. Color: Brass-yellow, tarnishes dark brown to black; in reflected light, brown-yellow or cream-yellow, may show an orange tint. Luster: Metallic. Pleochroism: Weak, creamy yellow to yellowish brown. Anisotropism: Marked, yellowish to tan. R1–R2: (400) 22.0–24.5, (420) 24.8–27.9, (440) 26.5–30.1, (460) 27.8–31.8, (480) 28.7–33.1, (500) 29.5–34.2, (520) 30.4–35.0, (540) 31.1–35.6, (560) 31.6–36.0, (580) 32.0–36.2, (600) 32.6–36.4, (620) 33.0–36.6, (640) 33.3–37.0, (660) 33.7–37.5, (680) 33.8–38.1, (700) 34.0–38.7 Cell Data: Space Group: P 42c. a = 5.518(4) c = 11.048(6) Z = 4 X-ray Powder Pattern: Petrovice, Czech Republic. 3.186 (10), 1.951 (9), 1.664 (8), 5.52 (7), 1.127 (7), 1.380 (6), 2.470 (5) Chemistry: (1) (2) (3) Cu 23.62 22.97 22.91 Fe 19.75 20.70 20.14 Ag 0.05 Se 55.96 56.35 56.95 S 0.02 Total 99.32 100.09 100.00 (1) Martin Lake, Canada; by electron microprobe, average of several analyses; corresponding to Cu1.06Fe1.01Se2.00. -
Formation and Study of Copper and Indium Selenides Layers on Glass Using Selenopolythionate Acids
KAUNAS UNIVERSITY OF TECHNOLOGY ALGIMANTAS IVANAUSKAS FORMATION AND STUDY OF COPPER AND INDIUM SELENIDES LAYERS ON GLASS USING SELENOPOLYTHIONATE ACIDS Doctoral dissertation Physical Sciences, Chemistry (03P) 2018, Kaunas This doctoral dissertation was prepared at Kaunas University of Technology, Faculty of Chemical Technology, Department of Physical and Inorganic Chemistry during the period of 2012–2017. Scientific Supervisor: Prof. Dr. Ingrida ANCUTIENĖ (Kaunas University of Technology, Physical Sciences, Chemistry – 03P). Doctoral dissertation has been published in: http://ktu.edu English Language Editor: Dovilė Dumbrauskaitė (Publishing Office “Technologija”). Lithuanian Language Editor: Aurelija Gražina Rukšaitė (Publishing Office “Technologija”). © A. Ivanauskas, 2018 ISBN 978-609-02-1423-7 The bibliographical information of this issue is available at Martynas Mazvydas National Library of Lithuania National Bibliographic Database (NBD) KAUNO TECHNOLOGIJOS UNIVERSITETAS ALGIMANTAS IVANAUSKAS VARIO IR INDŽIO SELENIDŲ SLUOKSNIŲ ANT STIKLO GAVIMAS NAUDOJANT SELENOPOLITIONATŲ RŪGŠTIS Daktaro disertacija Fiziniai mokslai, chemija (03P) 2018, Kaunas Disertacija rengta 2012–2017 metais Kauno technologijos universiteto cheminės technologijos fakultete fizikinės ir neorganinės chemijos katedroje. Mokslinis vadovas: Prof. dr. Ingrida ANCUTIENĖ (Kauno technologijos universitetas, fiziniai mokslai, chemija – 03P). Interneto svetainės, kurioje skelbiama disertacija, adresas: http://ktu.edu Anglų kalbą redagavo: Dovilė Dumbrauskaitė (Leidykla -
D. C. Hannrs, L. J. Cabnr Ano E. J. Munnev
AN OCCURRENCEOF A SULPHUR.BEARINGBERZELIANITE D. C. Hannrs,L. J. CaBnrano E. J. Munnev M,ines Branch, Departm,ent of Energy, M'ines anil, Resources,Ottawa, Canad,a Berzelianite is a selenide of copper with the formula Cuz_"Se.The binary Cu-Se system has been investigated by a number of workers, the most recent of which are Earley (1950), Borchert & Patzak (Lg5b), Heyding (1966) and Bernardini & Catani (1968). From the phase diagram, the cubic Cuz-rSe phase has a very narrow homogeneity range at room temperature, centered at approximately Cur.aSe,within the limits 0.15 ( r { 0.25. To date, no one has reported on the stability relations in the ternary system Cu-S-Se. During an investigation of the selenide minerals from Martin Lake, I ake Athabasca area, northern Saskatchewan,in which a new copper selenide mineral, athabascaite was found (Harris et al,. Ig6g), electron microprobe analysis showed that some of the berzelianite contained sulphur. The purpose of this paper is to report this first occurrenceof a naturally-occurring sulphur-bearing berzelianite. Gnnpnel DBscnrprrox The most common selenidesfrom the Martin Lake locality are uman- gite, berzelianite and clausthalite. Other minor selenides are klock- mannite, eucairite, tyrrellite, eskeborniteand athabascaite.The selenides occur in pitchblende ore and in hematite-stained carbonate vein material in the basalt of the Martin formation. The berzelianite that occursin the pitchblende ore is sulphur-free and it occurs as inclusions in, and replace- ments of, umangite. The sulphur-bearing berzelianite occurs as stringers and veinlets in the vein material. The mineral is associatedwith atha- bascaite, which in this environment is also sulphur-bearing, and with minor umangite.