LAPIS LAZULI from the COQUIMBO REGION, CHILE by Robert R
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Chemical Composition of Mn-And Cl-Rich Apatites from the Szklary
minerals Article Chemical Composition of Mn- and Cl-Rich Apatites from the Szklary Pegmatite, Central Sudetes, SW Poland: Taxonomic and Genetic Implications Adam Szuszkiewicz 1,* ID , Adam Pieczka 2, Bozena˙ Goł˛ebiowska 2, Magdalena Duma ´nska-Słowik 2 ID , Mariola Marszałek 2 and Eligiusz Szeł˛eg 3 1 Institute of Geological Sciences, University of Wrocław, pl. M. Borna 9, 50-204 Wrocław, Poland 2 Department of Mineralogy, Petrography and Geochemistry, AGH University of Science and Technology Mickiewicza 30, 30-059 Kraków, Poland; [email protected] (A.P.); [email protected] (B.G.); [email protected] (M.D.-S.); [email protected] (M.M.) 3 Department of Geochemistry, Mineralogy and Petrography, Faculty of Earth Sciences, University of Silesia, B˛edzi´nska60, 41-200 Sosnowiec, Poland; [email protected] * Correspondence: [email protected] Received: 6 July 2018; Accepted: 9 August 2018; Published: 14 August 2018 Abstract: Although calcium phosphates of the apatite group (apatites) with elevated contents of Mn are common accessory minerals in geochemically evolved granitic pegmatites, their Mn-dominant M1 M2 X analogues are poorly studied. Pieczkaite, Mn2 Mn3(PO4)3 Cl, is an exceptionally rare Mn analogue of chlorapatite known so far from only two occurrences in the world, i.e., granitic pegmatites at Cross Lake, Manitoba, Canada and Szklary, Sudetes, SW Poland. In this study, we present the data on the compositional variation and microtextural relationships of various apatites highly enriched in Mn and Cl from Szklary, with the main focus on compositions approaching or attaining the stoichiometry of pieczkaite (pieczkaite-like apatites). -
DIARIO OFICIAL I DE LA REPUBLICA DE CHILE SECCIÓN Ministerio Del Interior Y Seguridad Pública
DIARIO OFICIAL I DE LA REPUBLICA DE CHILE SECCIÓN Ministerio del Interior y Seguridad Pública LEYES, REGLAMENTOS, DECRETOS Y RESOLUCIONES DE ORDEN GENERAL Núm. 42.795 | Martes 3 de Noviembre de 2020 | Página 1 de 5 Normas Generales CVE 1840876 MINISTERIO DEL INTERIOR Y SEGURIDAD PÚBLICA Subsecretaría del Interior EXTIENDE VIGENCIA DE LA DECLARACIÓN DE LAS ZONAS AFECTADAS POR CATÁSTROFE EN LAS COMUNAS DE LAS REGIONES DE COQUIMBO Y VALPARAÍSO QUE INDICA Núm. 398.- Santiago, 7 de septiembre de 2020. Visto: Lo dispuesto en el artículo 32 Nº 6 de la Constitución Política de la República; en el decreto supremo Nº 104, de 29 de enero de 1977, del Ministerio del Interior, que fijó el texto refundido, coordinado y sistematizado del Título I, de la Ley Nº 16.282, sobre disposiciones permanentes para casos de sismos o catástrofes y sus modificaciones; en el decreto supremo Nº 156, de 2002, del Ministerio del Interior que aprobó el Plan Nacional de Protección Civil y sus modificaciones; en la Ley Nº 21.192, de Presupuestos del Sector Público, año 2020; en los decretos supremos Nº 234, del 28 de febrero de 2012; Nº 856, del 6 de agosto de 2012; Nº 105, del 28 enero de 2013; Nº 133, del 1 febrero de 2013: Nº 675, del 25 de junio de 2013; Nº 1.422, del 29 de julio de 2014; Nº 1.523, del 22 de agosto de 2014; Nº 1.776, del 28 de octubre de 2014; Nº 815, del 23 de junio de 2015; Nº 912, del 17 de junio de 2016; 1.280, del 25 de septiembre de 2017; Nº 1.128, del 24 de julio de 2018; Nº 308, del 20 de agosto de 2019, todos del Ministerio del Interior y Seguridad Pública, y en la resolución Nº 7, de 2019, de la Contraloría General de la República. -
The Journal of Gemmology Data Depository Photomicrographs To
The Journal of Gemmology Data Depository Photomicrographs to accompany the article: Hänni H.A., Brunk R. and Franz L. 2021. An investigation of grinding hardness of some ornamental stones. Journal of Gemmology, 37(6), 2021, 632–643, https://doi.org/10.15506/JoG.2021.37.6.632. The following photomicrographs of thin sections of the samples were made with a Leica DFC490 camera mounted on a Leica DMRD polarising microscope with transmitted light. For each sample, figure A shows the sample in plane-polarised light (II Pol.) and figure B with crossed polarisers (X Pol.); the sample numbers correspond to those in the article. Photomicrographs © L. Franz. 1 1 Aventurine quartz, green: Foliated matrix with aligned quartz (Qz) grains, fuchsite (Fu) tablets and accessory zircon (Zrn). 2 2 Aventurine quartz, orangey red: Mylonitic fabric with quartz (Qz) ribbons and recrystallized grains as well as intergrowths of muscovite with hematite (Ms & Hem). 3 3 Chalcedony, light grey: Intensely interlocked chalcedony (Chc) crystals with random orientation. 4 4 Chrysoprase: In a matrix of tiny chalcedony (Chc) and quartz (Qz) crystals, larger quartz aggregates occur. In microfractures, palisade-shaped chalcedony crystals and quartz grains formed. 5 5 Dumortierite: A banded texture with layers rich in dumortierite (Dum), dumortierite and quartz (Dum & Qz), quartz (Qz) and tourmaline (Tur). 6 6 Granite: The holocrystalline fabric is made up of subhedral plagioclase (Pl), orthoclase (Or), biotite (Bt) and anhedral quartz (Qz). 7 7 Green quartz: A granoblastic texture made up of large quartz (Qz) crystals as well as a microfolded layer of fuchsite (Fu). 8 8 Heliotrope (bloodstone): Green, brown and colourless accumulations of chalcedony (Chc) are recognizable. -
Thermal Behavior of Afghanite, an ABABACAC Member of the Cancrinite Group
American Mineralogist, Volume 97, pages 630–640, 2012 Thermal behavior of afghanite, an ABABACAC member of the cancrinite group PAOLO BALLIRANO1,2,* AND FERDINANDO BOSI1,3 1Dipartimento di Scienze della Terra, Sapienza Università di Roma, P.le Aldo Moro 5, I-00185, Roma, Italy 2CNR-IGAG, Istituto di Geologia Ambientale e Geoingegneria, Sede di Roma, Via Bolognola 7, I-00138 Roma, Italy 3CNR-IGG Istituto di Geoscienze e Georisorse, Sede di Roma, P.le A. Moro, 5, I-00185 Roma, Italy ABSTRACT Thermal behavior of afghanite, (Na15K5Ca11)Σ31[Si24Al24O96](SO4)6Cl6, P31c, a = 12.7961(7) Å, c = 21.4094(13) Å, an eight-layer member of the cancrinite group, has been investigated by combined electron microprobe analysis, X-ray single-crystal diffraction, and high-temperature X-ray powder diffraction. Non-ambient X-ray powder diffraction data were collected in the 323–1223 K thermal range on a specimen from Case Collina, Latium, Italy. Structural refinement and site assignment based on the bond-valence analysis, performed on room-temperature single-crystal X-ray diffraction data, provided more accurate site allocation of cations than the available model in the literature. The results show that the cancrinite cages alternating with the liottite cages are more compressed along the c-axis than the remaining ones. As a result the chlorine atom, located at the center of the cages, is driven off-axis to release the steric strain due to the cage compression. Thermal expansion shows a discontinuity at 448 K for both a and c unit-cell parameters, a feature previously reported for other cancrinite-like minerals. -
Repoussé Work for Amateurs
rf Bi oN? ^ ^ iTION av op OCT i 3 f943 2 MAY 8 1933 DEC 3 1938 MAY 6 id i 28 dec j o m? Digitized by the Internet Archive in 2011 with funding from Boston Public Library http://www.archive.org/details/repoussworkforamOOhasl GROUP OF LEAVES. Repousse Work for Amateurs. : REPOUSSE WORK FOR AMATEURS: BEING THE ART OF ORNAMENTING THIN METAL WITH RAISED FIGURES. tfjLd*- 6 By L. L. HASLOPE. ILLUSTRATED. LONDON L. UPCOTT GILL, 170, STRAND, W.C, 1887. PRINTED BY A. BRADLEY, 170, STRAND, LONDON. 3W PREFACE. " JjJjtfN these days, when of making books there is no end," ^*^ and every description of work, whether professional or amateur, has a literature of its own, it is strange that scarcely anything should have been written on the fascinating arts of Chasing and Repousse Work. It is true that a few articles have appeared in various periodicals on the subject, but with scarcely an exception they treated only of Working on Wood, and the directions given were generally crude and imperfect. This is the more surprising when we consider how fashionable Repousse Work has become of late years, both here and in America; indeed, in the latter country, "Do you pound brass ? " is said to be a very common question. I have written the following pages in the hope that they might, in some measure, supply a want, and prove of service to my brother amateurs. It has been hinted to me that some of my chapters are rather "advanced;" in other words, that I have gone farther than amateurs are likely to follow me. -
Red Glass for the Pharaoh Thilo Rehren
. ARCHAEOLOGY INTERNATIONAL HildO<heim, Genn•ny) '' excmting '� Red glass for the Pharaoh industrial estate dating to the foundatio period of the new city, including the larg-� I Thilo Rehren est known bronze foundries of antiquity,1 Glass in ancient Egypt appears to have been used as a substitute military workshops supplying and main for precious stones that were not available in the country. Here taining the pharaoh's chariotry including the process of glass manufacture is traced through the examina stables for hundreds of horses, and the only known production site for glass in tion of the fr agmentaryremains of ceramic reaction vessels and Bronze Age Egypt and Mesopotamia. The crucibles used in the production of small glass ingots. excavations date back to the 1980s, but only in the past couple of years have we been able to identify the glassmaking evi n archaeological terms, glass is a these precious materials, and ancient Egypt dence, although much of it had been exca relatively young material that was is no exception to this rule. It was famous vated many years previously. Why this invented much later than pottery or for its riches in gold, but had no silver ores; delay? Because we didn't know how to rec Imetals; only from the beginning of it produced amethyst, carnelian and tur ognize glassmaking: there being no prece the Late Bronze Age onwards do we quoise, but not lapis lazuli, amber or ob dent or template to follow when looking have good evidence for its intentional and sidian. Should the country's rulers there for Bronze Age glassmaking, and the evi routine production. -
The Hydrous Component in Andradite Garnet
American Mineralogist, Volume 83, pages 835±840, 1998 The hydrous component in andradite garnet GEORG AMTHAUER* AND GEORGE R. ROSSMAN² Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A. ABSTRACT Twenty-two andradite samples from a variety of geological environments and two syn- thetic hydroandradite samples were studied by Fourier transform IR spectroscopy. Their 2 spectra show that H enters andradite in the form of OH . Amounts up to 6 wt% H2O occur in these samples; those from low-temperature formations contain the most OH2. Some 42 ↔ 42 features in the absorption spectra indicate the hydrogarnet substitution (SiO4) (O4H4) whereas others indicate additional types of OH2 incorporation. The complexity of the spectra due to multi-site distribution of OH2 increases with increasing complexity of the garnet composition. 42 ↔ 42 INTRODUCTION tution (O4H4) (SiO4) . This observation has been Systematic studies have shown that hydroxide is a con®rmed by XRD of a hydrous andradite with a Si de- common minor component of grossular and pyrope-al- ®ciency of about 50%, and a high OH content (Arm- mandine-spessartite garnets (Aines and Rossman 1985; bruster 1995). The structure of this particular sample with Rossman and Aines 1991). Comparable surveys of an- space group Ia3d is composed of disordered microdo- dradite garnet have not been previously presented. Sev- mains containing (SiO4) and (O4H4) tetrahedral units. eral reports indicate that appreciable amounts of OH2 can The aim of the present investigation was to perform a be incorporated in both natural and synthetic andradite- Fourier transform infrared (FTIR) study on different sam- rich garnet (Flint et al. -
Wetedge Catalog
PRODUCT CATALOG 1 OUR STORY 3 HOW DID WE FACILITIES 4 GET HERE? PRODUCT LINE Years ago our founder, Laurence Turley, PRIMERA STONE 8 started his career in the mining industry. His worldwide experience in mining led SERENITY STONE 12 him to source exclusive materials from PRISM MATRIX 14 remote regions of the globe. In the early 80’s he focused his energy on the SIGNATURE MATRIX 17 pool industry and later formed Wet Edge Technologies. LUNA QUARTZ 21 Wet Edge Technologies has grown into ALTIMA 25 an industry leader through constant WATER COLOR HUE GUIDE 26 innovation in manufacturing, sourcing and application of our products. We THANK YOU 30 have introduced many new concepts and materials into the pool industry. These new additions enhance both the beauty and durability of our pool finishes. wetedgetechnologies.com 3 THE WET EDGE DIFFERENCE The stones used in our products have been shaped by water over millennia. Their roundness comes from the rushing water of rivers, the ebb and flow WESTERN PRODUCTION DRYING & SCREENING PLANT of tides, the endless motion of ocean waves, the ARIZONA MISSISSIPPI slow march of glacial movement and countless cycles of ice melting. We go to great lengths and expense to discover, recover and import these exotic stones from all over the globe. The roundness of our stones give you the smoothest pool finishes possible. Additionally, we control all aspects of sourcing, sizing and bagging our pebbles to ensure consistency and quality. Our proprietary admixtures used in all Wet Edge products fortify strength and bonding quality of each pool finish, giving you the longest lasting pool finish available. -
The Use of Titanium in Dentistry
Cells and Materials Volume 5 Number 2 Article 9 1995 The Use of Titanium in Dentistry Toru Okabe Baylor College of Dentistry, Dallas Hakon Hero Scandinavian Institute of Dental Materials, Haslum Follow this and additional works at: https://digitalcommons.usu.edu/cellsandmaterials Part of the Dentistry Commons Recommended Citation Okabe, Toru and Hero, Hakon (1995) "The Use of Titanium in Dentistry," Cells and Materials: Vol. 5 : No. 2 , Article 9. Available at: https://digitalcommons.usu.edu/cellsandmaterials/vol5/iss2/9 This Article is brought to you for free and open access by the Western Dairy Center at DigitalCommons@USU. It has been accepted for inclusion in Cells and Materials by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. Cells and Materials, Vol. 5, No. 2, 1995 (Pages 211-230) 1051-6794/95$5 0 00 + 0 25 Scanning Microscopy International, Chicago (AMF O'Hare), IL 60666 USA THE USE OF TITANIUM IN DENTISTRY Toru Okabe• and HAkon Hem1 Baylor College of Dentistry, Dallas, TX, USA 1Scandinavian Institute of Dental Materials (NIOM), Haslum, Norway (Received for publication August 8, 1994 and in revised form September 6, 1995) Abstract Introduction The aerospace, energy, and chemical industries have Compared to the metals and alloys commonly used benefitted from favorable applications of titanium and for many years for various industrial applications, tita titanium alloys since the 1950's. Only about 15 years nium is a rather "new" metal. Before the success of the ago, researchers began investigating titanium as a mate Kroll process in 1938, no commercially feasible way to rial with the potential for various uses in the dental field, produce pure titanium had been found. -
Marinellite, a New Feldspathoid of the Cancrinite-Sodalite Group
Eur. J. Mineral. 2003, 15, 1019–1027 Marinellite, a new feldspathoid of the cancrinite-sodalite group ELENA BONACCORSI* and PAOLO ORLANDI Dipartimento di Scienze della Terra, Universita` di Pisa, Via S. Maria 53, I-56126 Pisa, Italy * Corresponding author, e-mail: [email protected] Abstract: Marinellite, [(Na,K)42Ca6](Si36Al36O144)(SO4)8Cl2·6H2O, cell parameters a = 12.880(2) Å, c = 31.761(6) Å, is a new feldspathoid belonging to the cancrinite-sodalite group. The crystal structure of a twinned crystal was preliminary refined in space group P31c, but space group P62c could also be possible. It was found near Sacrofano, Latium, Italy, associated with giuseppettite, sanidine, nepheline, haüyne, biotite, and kalsilite. It is anhedral, transparent, colourless with vitreous lustre, white streak and Mohs’ hardness of 5.5. The mineral does not fluoresce, is brittle, has conchoidal fracture, and presents poor cleavage on {001}. Dmeas is 3 3 2.405(5) g/cm , Dcalc is 2.40 g/cm . Optically, marinellite is uniaxial positive, non-pleochroic, = 1.495(1), = 1.497(1). The strongest five reflections in the X-ray powder diffraction pattern are [d in Å (I) (hkl)]: 3.725 (100) (214), 3.513 (80) (215), 4.20 (42) (210), 3.089 (40) (217), 2.150 (40) (330). The electron microprobe analysis gives K2O 7.94, Na2O 14.95, CaO 5.14, Al2O3 27.80, SiO2 32.73, SO3 9.84, Cl 0.87, (H2O 0.93), sum 100.20 wt %, less O = Cl 0.20, (total 100.00 wt %); H2O calculated by difference. The corresponding empirical formula, based on 72 (Si + Al), is (Na31.86K11.13Ca6.06) =49.05(Si35.98Al36.02)S=72O144.60(SO4)8.12Cl1.62·3.41H2O. -
Damage Assessment of the 2015 Mw 8.3 Illapel Earthquake in the North‑Central Chile
Natural Hazards https://doi.org/10.1007/s11069-018-3541-3 ORIGINAL PAPER Damage assessment of the 2015 Mw 8.3 Illapel earthquake in the North‑Central Chile José Fernández1 · César Pastén1 · Sergio Ruiz2 · Felipe Leyton3 Received: 27 May 2018 / Accepted: 19 November 2018 © Springer Nature B.V. 2018 Abstract Destructive megathrust earthquakes, such as the 2015 Mw 8.3 Illapel event, frequently afect Chile. In this study, we assess the damage of the 2015 Illapel Earthquake in the Coquimbo Region (North-Central Chile) using the MSK-64 macroseismic intensity scale, adapted to Chilean civil structures. We complement these observations with the analysis of strong motion records and geophysical data of 29 seismic stations, including average shear wave velocities in the upper 30 m, Vs30, and horizontal-to-vertical spectral ratios. The calculated MSK intensities indicate that the damage was lower than expected for such megathrust earthquake, which can be attributable to the high Vs30 and the low predominant vibration periods of the sites. Nevertheless, few sites have shown systematic high intensi- ties during comparable earthquakes most likely due to local site efects. The intensities of the 2015 Illapel earthquake are lower than the reported for the 1997 Mw 7.1 Punitaqui intraplate intermediate-depth earthquake, despite the larger magnitude of the recent event. Keywords Subduction earthquake · H/V spectral ratio · Earthquake intensity 1 Introduction On September 16, 2015, at 22:54:31 (UTC), the Mw 8.3 Illapel earthquake occurred in the Coquimbo Region, North-Central Chile. The epicenter was located at 71.74°W, 31.64°S and 23.3 km depth and the rupture reached an extent of 200 km × 100 km, with a near trench rupture that caused a local tsunami in the Chilean coast (Heidarzadeh et al. -
26 May 2021 Aperto
AperTO - Archivio Istituzionale Open Access dell'Università di Torino The crystal structure of sacrofanite, the 74 Å phase of the cancrinite–sodalite supergroup This is the author's manuscript Original Citation: Availability: This version is available http://hdl.handle.net/2318/90838 since Published version: DOI:10.1016/j.micromeso.2011.06.033 Terms of use: Open Access Anyone can freely access the full text of works made available as "Open Access". Works made available under a Creative Commons license can be used according to the terms and conditions of said license. Use of all other works requires consent of the right holder (author or publisher) if not exempted from copyright protection by the applicable law. (Article begins on next page) 05 October 2021 This Accepted Author Manuscript (AAM) is copyrighted and published by Elsevier. It is posted here by agreement between Elsevier and the University of Turin. Changes resulting from the publishing process - such as editing, corrections, structural formatting, and other quality control mechanisms - may not be reflected in this version of the text. The definitive version of the text was subsequently published in MICROPOROUS AND MESOPOROUS MATERIALS, 147, 2012, 10.1016/j.micromeso.2011.06.033. You may download, copy and otherwise use the AAM for non-commercial purposes provided that your license is limited by the following restrictions: (1) You may use this AAM for non-commercial purposes only under the terms of the CC-BY-NC-ND license. (2) The integrity of the work and identification of the author, copyright owner, and publisher must be preserved in any copy.