An Introduction to the Rock-Forming Minerals
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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 -
November-2018-News.Pdf
Cathedral News November 2018 – No. 679 From: The Dean Safeguarding is much talked about in the Church of England, and in the nation more generally, but what does it mean in practice for us here at Exeter Cathedral? It is easy to focus on the preventative: on putting policies and processes in place to protect children and vulnerable adults from abuse and neglect. And that is very important, not least because of our Church’s woeful record, alongside many other institutions, over the past fifty years and more. Children and adults have every right to expect to be kept safe from harm when they come to the Cathedral: we speak of God as a loving Father, and all his children can surely expect us at the cathedral to embody and model his love and his protection when they visit us. But safeguarding also requires a proactive approach - to enable people to fulfil their potential and to flourish; or as Jesus puts it: “I have come that you may have life and have it abundantly.” Abundant life is the Good News we proclaim and pursue for everyone at the Cathedral: visitors, congregations, volunteers, staff and clergy alike. We have come a long way over the past 25 years, when the whole idea of safeguarding, or child protection as it was then called, was first introduced to the Church. But exactly how far, we shall know better in February, since the Cathedral is to receive a safeguarding audit from the Social Care Institute for Excellence. This body has worked its way through the dioceses of the Church of England, and is now turning its attention to cathedrals. -
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. -
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. -
Information Clearance Review and Release Approval
INFORMATION CLEARANCE REVIEW AND RELEASE APPROVAL Part I: Background Information Title: TEST RESULTS FOR CAUSTIC DEMAND MEASUREMENTS Information Category: ON TANK 241-AX-101 AND TANK 241-AX-103 ARCHIVE SAMPLES 0 Abstract 0 Journal Article 0 Summary 0 Internet 0 Visual Aid 0 Software Publish to OSTI? 0 Yes □ No 0 Full Paper 0 Report 0 Other Yes NA Trademark/Copyright “Right to Use” Information or Permission Documentation O 0 Document Number: WRPS-1602862 Revision 0 Date: July 2016 Author: Doll, Stephanie R Part II: External/Public Presentation Information Conference Name: Sponsoring Organization(s): WRPS Date of Conference: Conference Location: Will Material be Handed Out? □ Yes 0 No Will Information be Published? □ Yes 0 No ^formatinstuctfons/guidance^1106 Part III: WRPS Document Originator Checklist Description Yes N/A Print/Sign/Date Information Product meets requirements in TFC-BSM-AD-C-01? o 0 Document Release Criteria in TFC-ENG-DESIGN-C-25 completed? 0 (Attach checklist) o If product contains pictures, safety review completed? 0 o Lindberg, Chandy IDMS Data File att. Part IV: WRPS Internal Review Function Organization Date Print Name/Signature/Date Subject Matter Expert WRPS 10/04/2016 Doll, Stephanie R IDMS Data File att. Responsible Manager WRPS 08/08/2016 Cooke, Gary A IDMS Data File att. Other: Part V: IRM Clearance Services Review Description Yes No Print Name/Signature Document Contains Classified Information? o H If Answer is “Yes,” ADC Approval Required Print Name/Signature/Date Document Contains Information Restricted by DOE Operational o 0 Reviewer Signature: Security Guidelines? Print Name/Signature/Date Document is Subject to Release Restrictions? o H Document contains: If theanswer is “Yes, ” please mark category at right and describe 0 Applied Technology 0 Protected CRADA limitation or responsible organization below: 0 Personal/Private 0 Export Controlled 0 Proprietary 0 Procurement - Sensitive 0 Patentable Info. -
The Structure of Stilpnomelane Reexamined
THE STRUCTURE OF STILPNOMELANE REEXAMINED JouN W. Gnunon, Uniaersity of Minnesota, Mi.nneapolis,Minnesota. Assrnect New r-ray data show the distribution of ions normal to the basal cleavage in the layer silicate stilpnomelane. Since it is similarto talc and biotite a structure consistentwithits properties can be proposed. It explains satisfactorily the behavior of the mineral including its base exchange of K for Tl. Stilpnomelane is an important essential constituent of certain iron formations. fNrnooucrroN The writer (1) made an attempt in 1937 to determine the composition and crystal structure of stilpnomelane. At that time the mineral had been reported from the quartz veins in iron formations and from the chlorite-epidote-albite schists in New Zealand (8 and 11). Recently it has been identified in large amounts in the iron formations of the Cuyuna and Mesabi ranges of Minnesota. There it is one of the three principal iron silicates,iron talc, to be describedin detail shortly, being the second and greenalite the third. As was pointed out previously, (1, p. 912) stilpnomelane may readily be mistaken for biotite under the microscope.Like biotite it is negative with a small optic angle and has similar pleochroism. In the hand speci- men it resembleseither biotite or chlorite, but is much more brittle. Its cleavageis excellent. Basal sections with partially developed hexagonal outlines have been observed. These properties and the discussion that follows make it certain that stilpnomelane has a layer structure and is related to the micas and chlorites. CnBurcar CouposrrroN Nothing essentially new can be added with regard to the chemical composition of stilpnomelane. -
Manchester Design Standards
Appendix A Appendix A MANCHESTER DESIGN STANDARDS for the Manchester Village Commercial District Adopted with the 2007 Manchester Community Plan December 2007 A-1 Appendix A TABLE OF CONTENTS INTRODUCTION: THE CHARACTER OF MANCHESTER .......................................... A-4 CHAPTER 1: PURPOSE OF DESIGN STANDARDS FOR THE MANCHESTER VILLAGE COMMERCIAL ZONE (MVC) ......................................................................... A-5 Intent .............................................................................................................................A-5 CHAPTER 2: GENERAL PROVISIONS ........................................................................ A-5 Flexibility in Administration ............................................................................................A-5 Applicability....................................................................................................................A-6 Minor Changes ..............................................................................................................A-6 Mandatory Standards and Permissive Guidelines. .......................................................A-6 CHAPTER 3: SITE PLANNING ..................................................................................... A-7 Intent .............................................................................................................................A-7 Building Location and Orientation .................................................................................A-7 Setbacks -
Approaches to the Low Grade Metamorphic History of the Karakaya Complex by Chlorite Mineralogy and Geochemistry
Minerals 2015, 5, 221-246; doi:10.3390/min5020221 OPEN ACCESS minerals ISSN 2075-163X www.mdpi.com/journal/minerals Article Approaches to the Low Grade Metamorphic History of the Karakaya Complex by Chlorite Mineralogy and Geochemistry Sema Tetiker 1, Hüseyin Yalçın 2,* and Ömer Bozkaya 3 1 Department of Geological Engineering, Batman University, 72100 Batman, Turkey; E-Mail: [email protected] 2 Department of Geological Engineering, Cumhuriyet University, 58140 Sivas, Turkey 3 Department of Geological Engineering, Pamukkale University, 20070 Denizli, Turkey; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +90-0542-412-16-19. Academic Editor: Antonio Simonetti Received: 18 November 2014 / Accepted: 9 April 2015 / Published: 16 April 2015 Abstract: In this study, chlorite is used to investigate the diagenetic-metamorphic evolution and accurate geological history of the different units belonging to the Karakaya complex, Turkey. Primary and secondary chlorite minerals in the very low-grade metamorphic rocks display interference colors of blue and brown and an appearance of optical isotropy. Chlorites are present in the matrix, pores, and/or rocks units as platy/flaky and partly radial forms. X-ray diffraction (XRD) data indicate that Mg-Fe chlorites with entirely IIb polytype (trioctahedral) exhibit a variety of compositions, such as brunsvigite-diabantite-chamosite. The major element contents and structural formulas of chlorite also suggest these were derived from both felsic and metabasic source rocks. Trace and rare earth element (REE) concentrations of chlorites increase with increasing grade of metamorphism, and these geochemical changes can be related to the tectonic structures, formational mechanics, and environments present during their generation. -
Crystal Chemistry of Cancrinite-Group Minerals with an Ab-Type Framework: a Review and New Data
1151 The Canadian Mineralogist Vol. 49, pp. 1151-1164 (2011) DOI : 10.3749/canmin.49.5.1151 CRYSTAL CHEMISTRY OF CANCRINITE-GROUP MINERALS WITH AN AB-TYPE FRAMEWORK: A REVIEW AND NEW DATA. II. IR SPECTROSCOPY AND ITS CRYSTAL-CHEMICAL IMPLICATIONS NIKITA V. CHUKANOV§ Institute of Problems of Chemical Physics, 142432 Chernogolovka, Moscow Oblast, Russia IGOR V. PEKOV, LYUDMILA V. OLYSYCH, NATALIA V. ZUBKOVA AND MARINA F. VIGASINA Faculty of Geology, Moscow State University, Leninskie Gory, 119992 Moscow, Russia ABSTRACT We present a comparative analysis of powder infrared spectra of cancrinite-group minerals with the simplest framework, of AB type, from the viewpoint of crystal-chemical characteristics of extra-framework components. We provide IR spectra for typical samples of cancrinite, cancrisilite, kyanoxalite, hydroxycancrinite, depmeierite, vishnevite, pitiglianoite, balliranoite, davyne and quadridavyne, as well as the most unusual varieties of cancrinite-subgroup minerals (Ca-deficient cancrinite, H2O-free cancrinite, intermediate members of the series cancrinite – hydroxycancrinite, cancrinite–cancrisilite, cancrinite– kyanoxalite, K-rich vishnevite, S2-bearing balliranoite). Samples with solved crystal structures are used as reference patterns. Empirical trends and relationships between some parameters of IR spectra, compositional characteristics and unit-cell dimensions 2– are obtained. The effect of Ca content on stretching vibrations of CO3 is explained in the context of the cluster approach. The existence of a hydrous variety of quadridavyne is demonstrated. Keywords: cancrinite, cancrisilite, kyanoxalite, hydroxycancrinite, depmeierite, vishnevite, pitiglianoite, balliranoite, davyne, quadridavyne, cancrinite group, infrared spectrum, crystal chemistry. SOMMAIRE Nous présentons une analyse comparative des spectres infrarouges obtenus à partir de poudres de minéraux du groupe de la cancrinite ayant la charpente la plus simple, de type AB, du point de vue des caractéristiques cristallochimiques des composantes externes à la charpente. -
I-93 Exit 4A Final EIS And
NHDOT Project Number: 13065 I-93 EXIT 4A Federal Project Number: IM-0931(201) FINAL ENVIRONMENTAL FHWA EIS # FHWA-NH-EIS-07-01-F IMPACT STATEMENT AND RECORD OF DECISION VOLUME I: MAIN TEXT FEBRUARY 2020 Federal Highway Administration (FHWA) New Hampshire Department of Transportation (NHDOT) Town of Londonderry Town of Derry This page intentionally left blank. This page intentionally left blank. NHDOT Project No. 13065 I-93 Exit 4A FEIS Federal Highway Administration Record of Decision FHWA-NH-EIS-07-01-F Derry-Londonderry IM-0931(201) 13065 I-93 Exit 4A Rockingham County, New Hampshire 1.0 DECISION 1.1 Summary This Record of Decision (ROD) is for the proposed Interstate 93 (I-93) Exit 4A Project (Project). The Project, located in the Towns of Derry and Londonderry (the Towns), includes construction of a new interchange with I-93 (known as Exit 4A) and other transportation improvements to reduce congestion and improve safety along State Route 102 (NH 102), from I-93 easterly through downtown Derry, and to promote economic vitality in the Derry/Londonderry area. Based on the information presented in the 2007 Draft Environmental Impact Statement (DEIS); 2018 Supplemental Draft Environmental Impact Statement/Section 4(f) Evaluation (SDEIS); the 2020 Final Environmental Impact Statement (FEIS); all technical reports and supporting documentation incorporated by reference in the DEIS, SDEIS, and FEIS; and consideration of input received from other agencies and the public, the Federal Highway Administration (FHWA) has selected Alternative A for implementation. Alternative A is the environmentally preferred alternative because it best balances the need for the Project with social, economic, and natural environmental concerns. -
Place Branding: the Need for an Evaluative Framework
PLACE BRANDING: THE NEED FOR AN EVALUATIVE FRAMEWORK JOLANTA RUZINSKAITE A thesis submitted to the University of Huddersfield in partial fulfilment of the requirements for the degree of Doctor of Philosophy April 2015 Place branding: the need for an evaluative framework 2015 CONTENTS LIST OF FIGURES .............................................................................................. 8 LIST OF TABLES .............................................................................................. 11 ACKNOWLEDGEMENTS ................................................................................ 13 ABBREVIATIONS ............................................................................................. 14 PUBLICATIONS ................................................................................................ 15 ABSTRACT ......................................................................................................... 16 CHAPTER 1: INTRODUCTION ...................................................................... 18 1.0 CONTEXT AND RATIONALE ............................................................................. 18 1.1 RESEARCH FOCUS ........................................................................................... 18 1.2 THE RESEARCH NEED ...................................................................................... 21 1.3 AIMS AND OBJECTIVES OF THE STUDY............................................................ 28 1.4 OUTLINE RESEARCH DESIGN ......................................................................... -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote