Naturally Occurring Layered Mineral Franckeite with Anisotropic Raman Scattering and Third-Harmonic Generation Responses
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Both Pestle and Mortar Should Be Sent to a Commercial Heat Treating House to Be Carburized to a Depth of at Least $ Inch and Hardened to 62-64 Rockwell C
NOTES AND NEWS 165 Both pestle and mortar should be sent to a commercial heat treating house to be carburized to a depth of at least $ inch and hardened to 62-64 Rockwell C. It is not necessaryto harden the sleeve although it may be cyanided. After heat treating the mortar is chucked in the lathe and the diameter of the projection is ground with a tool post grinder to a tight, but re- movable, fi.t to the sleeve. The face of the projection should be ground true to the side at the same chucking. The pestle is also chucked and the diameter of the grinding end reduced about .005 inch, or a working fit in the sleeve.The face of the pestle should also be ground true with the side. A NEW LOCALITY FOR GREENOCKITE CRYSTALS IN BOLIVIA FnBoBnrco Aur,rnr,o, C ochabambo, Bol'ivia. Greenockite is a rare mineral in the Bolivian tin deposits' It has been describedonly from Llallagua by S. Gordon (1). The mineral forms coat- ings of minute red crystals, resembling vanadinite in colour, upon quartz' marcasite, cassiteriteand on the wall rock, almost always associatedwith wavellite. The crystals are exceedinglyminute, rarely measuring as much as 0.1 mm. They vary greatly in habit from pyramidal to thick tabular and prismatic. Cyclic twins are common. Gordon ascribesthe formation of the mineral to supergenesolutions. The source of the cadmium may have been from the wurtzite or sphalerite which has relaced pyrrhotite. 166 NOTESAND NEWS Recently I found a secondoccurrence of greenockite in Bolivia, which is remarkable for the larger size and the rich red colour of the crystals. -
Toward the Crystal Structure of Nagyagite, [Pb(Pb,Sb)S2][(Au,Te)]
American Mineralogist, Volume 84, pages 669–676, 1999 Toward the crystal structure of nagyagite, [Pb(Pb,Sb)S2][(Au,Te)] HERTA EFFENBERGER,1,* WERNER H. PAAR,2 DAN TOPA,2 FRANZ J. CULETTO,3 AND GERALD GIESTER1 1Institut für Mineralogie und Kristallographie, Universität Wien, Althanstrasse 14, A-1090 Vienna, Austria 2Institut für Mineralogie, Universität Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg 3Kärntner Elektrizitäts AG, Arnulfplatz 2, A-9021 Klagenfurt, Austria ABSTRACT Synthetic nagyagite was grown from a melt as part of a search for materials with high-tempera- ture superconductivity. Electron microprobe analyses of synthetic nagyagite and of nagyagite from the type locality Nagyág, Transylvania (now S˘ac˘arîmb, Romania) agree with data from literature. The crystal chemical formula [Pb(Pb,Sb)S2][(Au,Te)] was derived from crystal structure investi- gations. Nagyagite is monoclinic pseudotetragonal. The average crystal structure was determined from both synthetic and natural samples and was refined from the synthetic material to R = 0.045 for 657 single-crystal X-ray data: space group P21/m, a = 4.220(1) Å, b = 4.176(1) Å, c = 15.119(3) Å, β = 95.42(3)°, and Z = 2. Nagyagite features a pronounced layer structure: slices of a two slabs thick SnS-archetype with formula Pb(Pb,Sb)S2 parallel to (001) have a thickness of 9.15 Å. Te and Au form a planar pseudo-square net that is sandwiched between the SnS-archetype layers; it is [4Te] assumed that planar Au Te4 configurations are edge connected to chains and that Te atoms are in a zigzag arrangement. -
Tin, Arsenic, Zinc and Silver Vein Mineralization Many Vein
MINING GEOLOGY, 38(5), 407•`418, 1988 Tin, Arsenic, Zinc and Silver Vein Mineralization in the Besshi Mine, Central Shikoku, Japan Katsuo KASE* Abstract: Intense Sn-As-Zn-Ag vein mineralization was found at the 26th Level of the Besshi mine, of which deposit is a conformable massive sulfidetype (Besshi-type).The mineralization resulted in formation of such rare Sn minerals as rhodostannite, hocartite and a franckeite-like mineral, as well as common stannite and cassiterite. Pyrite, arsenopyrite, sphalerite, tetrahedrite, manganese carbonates, quartz, tourmaline and so on occur in associa- tion with these Sn minerals. The prominently polymetallic ores are composed of minerals that were formed at several stages during the mineralization sequence. The present microprobe analyses, combined with previous chemicaldata, indicate that the substitution of Ag for Cu is extensivein rhodostannite, whereas that of Zn for Fe is very limited. The substitution relationship of these elementsin stannite and hocartite is just the opposite to that found in rhodostannite. Divalent Sn may substitute for Pb in the franckeite-like mineral, which is considered to be mainly responsible for the extensive solid solution ob- served in this mineral. The mineralization may have taken place nearly simultaneously with contact metamorphism, which con- verted the massive pyrite ores and surrounding pelitic schists to massivepyrrhotite ores and biotite hornfels, respec- tively. A granitic intrusion, which is supposed to be hidden in the deeper part of the Besshi mining district, probably caused the vein mineralization and contact metamorphism. The geological situation and mineralogical characteristics of the vein mineralization are quite similar to those observedin the Sn deposits adjacent to Miocene granitic intrusives in the Outer Zone of Southwest Japan at Kyushu. -
New Mineral Names*
American Mineralogist, Volume 68, pages 1248-1252,1983 NEW MINERAL NAMES* Perr J. DUNN, MrcHeE'r-FLerscHen, Gr,oncB Y. CHno, Lours J. Cesnr, AND JosEpHA. MexoanrNo Biivoetite* Lcpersonnite* bright yellow and is transparent and translucent. No fluores- Unnamed CeNi-Mg uranyl silicate cence was observed under short- or long-wave UV. The mea- sureddensity is 3.97g/cmr. It is opticallybiaxial negative,2V = M. Deliensand P. Piret (1982)Bijvoetite et lepersonnite,carbon- 73" calc.,a = 1.638, : 1.666,y : 1.682;pleochroic with X pale ates hydratds d'uranyle et des terres rares de Shinkolobwe, B yellow, bright yellow and Z bnght yellow; orientation, only Zaire. Can. Mineral.. 20.231J38. I=cisgiven. = Bijvoetite The mineral is orthorhombic, Pnnm or Pnn2 with a 16.23(3), b = 38.7aQ),c : rr.73Q)4, Z : 2, (V : 7375(50)43,J.A.M.). Blivoetite and lepersonniteoccur with hydrated uranium ox- The density calculated from the unit cell parameters and the ides near primary uraninite in the lower part of the oxidation empirical formula is 4.01 g/cm3. Strongest lines in the X-ray zone at Shinkolobwe, Zaire. Bijvoetite is rare and is known only powder diffraction pattern (for CuKa) are: 8.15(100X200), from a single specimen. Associated minerals are: lepersonnite, 4.06(I 5X400),3.65(70X1 33), 3.2I (50X0.I 2.0) and 2.86(40)(283). sklodowskite, curite, uranophane, becquerelite, rutherfordine, An electronmicroprobe analysis gave: SiO22.79, UOj76.14, studtite and a CeMg-Ni uranyl silicate structurally related to Gd2O32.W,Dy2O3 1.07, Y2O3 0.41, Tb2O3 0.(D, CaO 0.45,CO2 uranophane. -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951). -
And Its Relations to Franckeite and Cylindrite. by O
21 On Tealllte, a new sulphostannite of lead from Bolivia; and its relations to Franckeite and Cylindrite. By O. T. PaxoR, M.A., F.G.S. Assistant in the Mineral Department of the British Museum. [Read February 2, 1904.] ZONGST the specimens recently selected for the British ]~useum from the collection of South American minerals brought together by the late Theodor Hohmann, are two on which occurs a mineral in thin laminae resembling graphite. From the locality and associations, the mineral was at first presumed to be either franckeite or cylindrite, the two sulphantim- onite-sulphostannates of lead from Bolivia, which were described in 1893 by Stelzner and Frenzel respectively 1. Qualitative analysis, however, soon showed that, although similar to them in physical characters, it differed chemically from both franckelte and cylindrite in containing no antimony, but only lead, tin, and sulphur. Of the two specimens from the Hohmann collection, one was labelled ' sulphoselenide of lead from Bolivia,' and the other ' selenide of lead from Atacama,' so that unfortunately the precise locality of the mineral is at present unknown. In all probability both specimens came from the same district in Bolivla, since in appearance they are very similar. The new mineral occurs in thin graphlte-like folia embedded in glistening kaolin, upon a dark grey matrix impregnated with iron- pyrites; on one specimen it is associated with a little wurtzlte in thin plates, and on the other with a little galena. Gry~allographio ff/uzrac~rs:--The teallite on the two specimens occurs for the most part in very thin folia with irregular boundaries. -
Exfoliated Pyrite (Fes2) – a Non-Van Der Waals 2D Ferromagnet
JPCC, DOI: 10.1021/acs.jpcc.1c04977 Apparent Ferromagnetism in Exfoliated Ultra-thin Pyrite Sheets Anand B. Puthirath1†*, Aravind Puthirath Balan2†, Eliezer F. Oliveira1,3,4†, Vishnu Sreepal2, Francisco C. Robles Hernandez1,5, Guanhui Gao1, Nithya Chakingal1, Lucas M. Sassi1, Prasankumar Thibeorchews 1, Gelu Costin7, Robert VaJtai1, Douglas S. Galvao1,3,4 Rahul R. Nair2 and Pulickel M. AJayan1* 1Department of Material Science and NanoEngineering, Rice University, Houston, Texas, 77005, United States. 2Department of Chemical Engineering and Analytical Science (CEAS) & National Graphene Institute (NGI), University of Manchester, Manchester, M13 9PL, UK 3 Group of Organic Solids and New Materials, Gleb Wataghin Institute of Physics, University of Campinas (UNICAMP), Campinas, SP 13083-970, Brazil 4 Center for Computational Engineering & Sciences (CCES), University of Campinas (UNICAMP), Campinas, SP 13083-970, Brazil 5Mechanical Engineering Technology Program, Department of Engineering Technology, College of Technology, University of Houston, TX, 77204, USA †These authors contributed equally Email: [email protected], [email protected] 1 JPCC, DOI: 10.1021/acs.jpcc.1c04977 Abstract Experimental evidence for ferromagnetic ordering in isotropic atomically thin two-dimensional crystals has been missing until a bilayer Cr2Ge2Te6, and a three-atom thick monolayer CrI3 are shown to retain ferromagnetic ordering at finite temperatures. Here, we demonstrate successful isolation of a non-van der Waals type ultra-thin nanosheet of FeS2 derived from naturally occurring pyrite mineral (FeS2) by means of liquid-phase exfoliation. Structural characterizations imply that (111) oriented sheets are predominant and is supported theoretically by means of density functional theory surface energy calculations. Spin-polarized density theory calculations further predicted that (111) oriented three-atom thick pyrite sheet has a stable ferromagnetic ground state different from its diamagnetic bulk counterpart. -
Cylindrite Pb3sn4fesb2s14 C 2001-2005 Mineral Data Publishing, Version 1
Cylindrite Pb3Sn4FeSb2S14 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Triclinic. Point Group: 1. In concentric spherical or tubular shells and aggregates, up to 5 cm across and 2–3 cm in length, rarely terminated; also massive. Physical Properties: Cleavage: {100}, excellent. Tenacity: Slightly malleable. Hardness = 2.5 VHN = 54–93 (100 g load). D(meas.) = 5.42–5.49 D(calc.) = 5.443 Optical Properties: Opaque. Color: In reflected light, galena-white. Streak: Black. Luster: Metallic. Pleochroism: Weak in air, stronger in oil. Anisotropism: Distinct, gray to pale yellowish or brownish gray. R1–R2: (400) 34.5–40.3, (420) 34.3–40.1, (440) 34.1–40.1, (460) 33.6–39.8, (480) 33.1–39.4, (500) 32.5–38.9, (520) 31.8–38.3, (540) 31.2–37.8, (560) 30.7–37.2, (580) 30.3–36.7, (600) 29.9–36.3, (620) 29.6–35.9, (640) 29.3–35.5, (660) 28.9–35.1, (680) 28.6–34.7, (700) 28.4–34.4 Cell Data: Space Group: Two subcells are recognized, both P 1 : the first (pseudotetragonal) has a = 11.733(5) b = 5.790(8) c = 5.810(5) α =90.00(0.20)◦ β =92.38(0.20)◦ γ =93.87(0.20)◦ Z = 2 and the second (pseudohexagonal) has a = 11.709(5) b = 3.670(8) c = 6.320(5) α =90.00(0.20)◦ β =92.58(0.20)◦ γ =90.85(0.20)◦ Z=2 X-ray Powder Pattern: Poop´o,Bolivia. -
Mineralogy and Distribution of Critical Elements in the Sn–W–Pb–Ag–Zn Huanuni Deposit, Bolivia
minerals Article Mineralogy and Distribution of Critical Elements in the Sn–W–Pb–Ag–Zn Huanuni Deposit, Bolivia Andreu Cacho 1, Joan-Carles Melgarejo 1 , Antoni Camprubí 2,*, Lisard Torró 3 , Montgarri Castillo-Oliver 4, Belén Torres 1, David Artiaga 5, Esperança Tauler 1 , Álvaro Martínez 6, Marc Campeny 1,7, Pura Alfonso 8 and Osvaldo R. Arce-Burgoa 9,10 1 Departament de Mineralogia, Petrologia i Prospecció Geològica, Facultat de Ciències de la Terra, Universitat de Barcelona, Carrer de Martí i Franquès s/n, 08028 Barcelona, Spain; [email protected] (A.C.); [email protected] (J.-C.M.); [email protected] (B.T.); [email protected] (E.T.); [email protected] (M.C.) 2 Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, 04510, CDMX, Mexico 3 Geological Engineering Program, Faculty of Sciences and Engineering, Pontifical Catholic University of Peru (PUCP), Av. Universitaria 1801, San Miguel, Lima 15088, Peru; [email protected] 4 ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, North Ryde, NSW 2109, Australia; [email protected] 5 Centres Científics i Tecnològics, Universitat de Barcelona, Carrer de Martí i Franquès s/n, 08028 Barcelona, Spain; [email protected] 6 Departement des Sciences de la Terre, Université de Genève, Rue des Maraîchers 13, 1205 Genève, Switzerland; [email protected] 7 Departament de Mineralogia, Museu de Ciències Naturals de Barcelona, Passeig Picasso s/n, 08003 Barcelona, Spain 8 Departament d’Enginyeria Minera, Industrial i TIC, Escola Tècnica Superior d’Enginyeria de Mines de Manresa, Universitat Politècnica de Catalunya, Avinguda de les Bases de Manresa 61–73, 08242 Manresa, Spain; [email protected] 9 Colegio de Geólogos de Bolivia, Edificio Señor de la Exaltación Nro. -
Naturally Occurring Van Der Waals Materials Riccardo Frisenda,1 Yue Niu,2 Patricia Gant,1 Manuel Muñoz3 and Andres Castellanos-Gomez*1
Naturally occurring van der Waals materials Riccardo Frisenda,1 Yue Niu,2 Patricia Gant,1 Manuel Muñoz3 and Andres Castellanos-Gomez*1 1 Materials Science Factory, Instituto de Ciencia de Materiales de Madrid, Consejo Superior de Investigaciones Científicas, 28049, Madrid, Spain 2 National Center for International Research on Green Optoelectronics and Guangdong Provincial Key Laboratory of Optical Information Materials and Technology, Institute of Electronic Paper Displays, South China Academy of Advanced Optoelectronics, South China Normal University, Guangzhou 510006, People's Republic of China. 3 Instituto de Tecnologías Físicas y de la Información ITEFI-CSIC, 28006 Madrid, Spain *E-mail: [email protected] ABSTRACT:. The exfoliation of two naturally occurring van der Waals minerals, graphite and molybdenite, arouse an unprecedented level of interest by the scientific community and shaped a whole new field of research: 2D materials research. Several years later, the family of van der Waals materials that can be exfoliated to isolate 2D materials keeps growing, but most of them are synthetic. Interestingly, in nature plenty of naturally occurring van der Waals minerals can be found with a wide range of chemical compositions and crystal structures whose properties are mostly unexplored so far. This Perspective aims to provide an overview of different families of van der Waals minerals to stimulate their exploration in the 2D limit. KEYWORDS: layered minerals, van der Waals materials, naturally occurring 2D materials, exfoliation -
Suredaite, Pbsns3, a New Mineral Species, from the Pirquitas Ag-Sn Deposit, NW-Argen- Tina: Mineralogy and Crystal Structure
American Mineralogist, Volume 85, pages 1066–1075, 2000 Suredaite, PbSnS3, a new mineral species, from the Pirquitas Ag-Sn deposit, NW-Argen- tina: mineralogy and crystal structure WERNER H. PAAR,1 RONALD MILETICH,2,6 DAN TOPA,3 ALAN J. CRIDDLE,4 MILKA K. DE BRODTKORB,5 GEORG AMTHAUER,1 AND GEROLD TIPPELT1 1Institut für Mineralogie, Universität Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg, Austria 2Laboratory for Crystallography, ETH Zürich, Sonneggstrasse 5, CH-8092 Zürich, Switzerland 3Institute of Geology and Paleontology, Universität Salzburg, Hellbrunnerstrasse 34, 5020 Salzburg, Austria 4Department of Mineralogy, The Natural History Museum, London SW7 5BD, U.K. 5Consejo Nacional de Investigaciones Cientificas y Tecnicas—University of Buenos Aires, Paso 258-9A, 1640 Martinez, Argentina 6Bayerisches Geoinstitut, Universität Bayreuth, D-95445 Bayreuth, Germany ABSTRACT Suredaite, ideally PbSnS3, is a new mineral species from the Pirquitas Ag-Sn deposit (Province Jujuy, NW-Argentina). It was observed in symmetrically banded veins in the Oploca district, and is associated with sphalerite, arsenopyrite, pyrite-marcasite, cassiterite, cylindrite, franckeite, hocartite, rhodostannite, and various Ag-Sb and Ag-Bi sulfosalts in minor amounts. Suredaite occurs in layers up to 1 cm in thickness as aggregates of radially arranged tabular-prismatic (single) crystals, has a metallic lustre, and a dark grey streak. VHN50 ranges between 18.2 and 20.6 (mean 19.6) GPa, the Mohs hardness is 2.5–3. It has perfect cleavages parallel to {001}, {101}, and {100}. The measured 3 3 density varies between 5.54 and 5.88 g/cm , Dx was determined to be 5.615 g/cm . In reflected plane-polarised light, it is white and is not perceptibly bireflectant or pleochroic. -
Franckeite: a Naturally Occurring Van Der Waals Heterostructure
Franckeite: a naturally occurring van der Waals heterostructure Aday J. Molina-Mendoza,1,† Emerson Giovanelli,2,† Wendel S. Paz,1 Miguel Angel Niño,2 Joshua O. Island,3 Charalambos Evangeli,1,§ Lucía Aballe,4 Michael Foerster,4 Herre S. J. van der Zant,3 Gabino Rubio-Bollinger,1,5 Nicolás Agraït,1,2,5 J. J. Palacios,1,* Emilio M. Pérez,2,* and Andres Castellanos-Gomez.2,* 1Departamento de Física de la Materia Condensada, Universidad Autónoma de Madrid, Campus de Cantoblanco, E-28049, Madrid, Spain. 2Instituto Madrileño de Estudios Avanzados en Nanociencia (IMDEA-Nanociencia), Campus de Cantoblanco, E-28049 Madrid, Spain. 3Kavli Institute of Nanoscience, Delft University of Technology, Lorentzweg 1, 2628 CJ Delft, The Netherlands. 4ALBA Synchrotron Light Facility, Carrer de la Llum 2-26, Cerdanyola del Vallés, Barcelona 08290, Spain. 5Condensed Matter Physics Center (IFIMAC), Universidad Autónoma de Madrid, E-28049 Madrid, Spain. †These authors contributed equally. §Present address: Department of Physics, Lancaster University, Lancaster LA1 4YB, United Kingdom. *email: [email protected]; [email protected]; [email protected]. The fabrication of van der Waals heterostructures, artificial materials assembled by individually stacking atomically thin (2D) materials, is one of the most promising directions in 2D materials research. Until now, the most widespread approach to stack 2D layers relies on deterministic placement methods which are cumbersome when fabricating multilayered stacks. Moreover, they tend to suffer from poor control over the lattice orientations and the presence of unwanted adsorbates between the stacked layers. Here, we present a different approach to fabricate ultrathin heterostructures by exfoliation of bulk franckeite which is a naturally occurring and air stable van der Waals heterostructure (composed of alternating SnS2-like and PbS-like layers stacked on top of each other).