Abbreviations for Names of Rock-Forming Minerals
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Baddeleyite Microstructures in Variably Shocked Martian Meteorites: an Opportunity to Link Shock Barometry and Robust Geochronology
51st Lunar and Planetary Science Conference (2020) 2302.pdf BADDELEYITE MICROSTRUCTURES IN VARIABLY SHOCKED MARTIAN METEORITES: AN OPPORTUNITY TO LINK SHOCK BAROMETRY AND ROBUST GEOCHRONOLOGY. L. G. Staddon1*, J. R. Darling1, N. R. Stephen2, J. Dunlop1, and K. T. Tait3,4. 1School of Environment, Geography and Geoscience, University of Portsmouth, UK; *[email protected], 2Plymouth Electron Microscopy Centre, Plymouth University, UK, 3Department of Earth Sciences, University of Toronto, Canada, 4Royal Ontario Museum, Toronto, Canada. Introduction: Baddeleyite (monoclinic ZrO2; m- [6]. Shergottites in which plagioclase has undergone ZrO2) has recently been shown to be capable of provid- complete transformation to maskelynite (S4), suggest- ing robust crystallisation ages for shergottites via in- ing shock pressures of at least ~29 GPa [6], are repre- situ U-Pb isotopic analyses [1,2]. However, in contrast sented by enriched shergottites NWA 8679 and NWA to experimental work [3], these studies also highlight 7257. Both samples are similarly evolved lithologies, that U-Pb isotope systematics of baddeleyite can be abundant in late stage phases such as Fe-Ti oxides, Cl- strongly modified by shock metamorphism. Up to apatite and Si- and K- rich mesostasis, though NWA ~80% radiogenic Pb loss was recorded within North- 7257 is doleritic [9,10]. Enriched basaltic shergottite west Africa (NWA) 5298 [1], with close correspond- NWA 5298 represents the most heavily shocked mar- ence of U-Pb isotopic ratios and baddeleyite micro- tian meteorite studied here (S6), containing both structures [4]. Combined microstructural analysis and maskelynite and vesicular plagioclase melt [4]. U-Pb geochronology of baddeleyite therefore offers Baddeleyite grains >2 µm in length were located tremendous potential to provide robust constraints on via a combination of automated backscattered electron crystallisation and impact ages for martian meteorites. -
Geology and Mineral Deposits of the James River-Roanoke River Manganese District Virginia
Geology and Mineral Deposits of the James River-Roanoke River Manganese District Virginia GEOLOGICAL SURVEY BULLETIN 1008 Geology and Mineral ·Deposits oftheJatnes River-Roanoke River Manganese District Virginia By GILBERT H. ESPENSHADE GEOLOGICAL SURVEY BULLETIN 1008 A description of the geology anq mineral deposits, particularly manganese, of the James River-Roanoke River district UNITED STAT.ES GOVERNMENT, PRINTING. OFFICE• WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS· Page Abstract---------------------------------------------------------- 1 Introduction______________________________________________________ 4 Location, accessibility, and culture_______________________________ 4 Topography, climate, and vegetation _______________ .,.. _______ ---___ 6 Field work and acknowledgments________________________________ 6 Previouswork_________________________________________________ 8 GeneralgeologY--------------------------------------------------- 9 Principal features ____________________________ -- __________ ---___ 9 Metamorphic rocks____________________________________________ 11 Generalstatement_________________________________________ 11 Lynchburg gneiss and associated igneous rocks________________ 12 Evington groUP------------------------------------------- 14 Candler formation_____________________________________ 14 Archer Creek formation________________________________ -
Podiform Chromite Deposits—Database and Grade and Tonnage Models
Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S. -
X-Ray Rietveld and 57Fe Mössbauer Study of Babingtonite from Kouragahana, Shimane Peninsula, Japan
Journal of MineralogicalBabingtonite and from Petrological Kouragahana, Sciences, Shimane Volume Peninsula, 108, pageJapan 121─ 130, 2013 121 X-ray Rietveld and 57Fe Mössbauer study of babingtonite from Kouragahana, Shimane Peninsula, Japan * * ** Masahide AKASAKA , Takehiko KIMURA and Mariko NAGASHIMA *Department of Geoscience, Graduate School of Science and Engineering, Shimane University, 1060 Nishikawatsu, Matsue 690-8504, Japan **Department of Earth Science, Graduate School of Science and Engineering, Yamaguchi University, Yamaguchi 753-8512, Japan Babingtonite from Kouragahana, Shimane Peninsula, Japan, was investigated using electron microprobe, X-ray Rietveld, and 57Fe Mössbauer spectral analyses to characterize its chemical compositions, crystal structure, oxi- dation state of Fe, and distribution of Fe between two crystallographically independent octahedral Fe1 and Fe2 sites. _ The_ Kouragahana babingtonite occurs as single parallelohedrons with {100}, {001}, {001}, {111}, {110}, and {101} and sometimes shows penetration twinning. Both normal and sector-zoned crystals occur. Babing- tonite crystals with sector zoning consist of sectors relatively enriched in Fe and of sectors enriched in Mg, Mn, and Al. Babingtonite also shows compositional zoning with higher Fe2+ and Al core and higher Fe3+ and Mn 2+ rim. The average Fe content of the babingtonite without sector zoning is similar to the Fe -rich sector of the sector-zoned babingtonite. The chemical formula based on the average composition of all analytical data (n = 2+ 3+ - 193) is [Na0.01(2)Ca2.01(2)] [Mg0.11(4)Mn0.09(3)Fe0.76(7)Fe_ 0.93(5)Ti0.01(1)Al0.06(5)]Si5.01(4)O14(OH). X ray Rietveld refinement was carried out using a model of space group P1. -
The Krásno Sn-W Ore District Near Horní Slavkov: Mining History, Geological and Mineralogical Characteristics
Journal of the Czech Geological Society 51/12(2006) 3 The Krásno Sn-W ore district near Horní Slavkov: mining history, geological and mineralogical characteristics Sn-W rudní revír Krásno u Horního Slavkova historie tìby, geologická a mineralogická charakteristika (47 figs, 1 tab) PAVEL BERAN1 JIØÍ SEJKORA2 1 Regional Museum Sokolov, Zámecká 1, Sokolov, CZ-356 00, Czech Republic 2 Department of Mineralogy and Petrology, National Museum, Václavské nám. 68, Prague 1, CZ-115 79, Czech Republic The tin-tungsten Krásno ore district near Horní Slavkov (Slavkovský les area, western Bohemia) belongs to the most important areas of ancient mining in the Czech Republic. The exceptionally rich and variable mineral associations, and the high number of mineral species, make this area one of the most remarkable mineralogical localities on a worldwide scale. The present paper reviews the data on geological setting of the ore district, individual ore deposits and mining history. Horní Slavkov and Krásno were known as a rich source of exquisite quality mineral specimens stored in numerous museum collections throughout Europe. The old museum specimens are often known under the German locality names of Schlaggenwald (= Horní Slavkov) and Schönfeld (=Krásno). The megascopic properties and paragenetic position of selected mineral classics are reviewed which include arsenopyrite, fluorapatite, fluorite, hübnerite, chalcopyrite, carpholite, cassiterite, quartz, molybdenite, rhodochrosite, sphalerite, topaz and scheelite. Key words: Sn-W ores; tin-tungsten mineralization; mining history; ore geology; mineralogy; Slavkovský les; Krásno, Horní Slavkov ore district; Czech Republic. Introduction valleys dissected parts of the area. In the ore district area, the detailed surface morphology is modified by large de- In the mining history of Central Europe, Bohemia and pressions caused by the collapse of old underground Moravia are known as important source of gold, silver, workings and by extensive dumps. -
A New Occurrence of Terrestrial Native Iron in the Earth's Surface
geosciences Article A New Occurrence of Terrestrial Native Iron in the Earth’s Surface: The Ilia Thermogenic Travertine Case, Northwestern Euboea, Greece Christos Kanellopoulos 1,2,* ID , Eugenia Valsami-Jones 3,4, Panagiotis Voudouris 1, Christina Stouraiti 1 ID , Robert Moritz 2, Constantinos Mavrogonatos 1 ID and Panagiotis Mitropoulos 1,† 1 Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou, 15784 Athens, Greece; [email protected] (P.V.); [email protected] (C.S.); [email protected] (C.M.); [email protected] (P.M.) 2 Section of Earth and Environmental Sciences, University of Geneva, Rue des Maraichers 13, 1205 Geneva, Switzerland; [email protected] 3 School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK; [email protected] 4 Department of Earth Sciences, Natural History Museum London, Cromwell Road, London SW7 5BD, UK * Correspondence: [email protected] † Professor Panagiotis Mitropoulos has passed away in 2017. Received: 6 April 2018; Accepted: 23 July 2018; Published: 31 July 2018 Abstract: Native iron has been identified in an active thermogenic travertine deposit, located at Ilia area (Euboea Island, Greece). The deposit is forming around a hot spring, which is part of a large active metallogenetic hydrothermal system depositing ore-bearing travertines. The native iron occurs in two shapes: nodules with diameter 0.4 and 0.45 cm, and angular grains with length up to tens of µm. The travertine laminae around the spherical/ovoid nodules grow smoothly, and the angular grains are trapped inside the pores of the travertine. -
Heat Capacity of High Pressure Minerals and Phase Equilibria of Cretan Blueschists
Heat capacity of high pressure minerals and phase equilibria of Cretan blueschists by Matthew Rahn Manon A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology) in The University of Michigan 2008 Doctoral Committee: Professor Eric J. Essene, Chair Professor Rebecca Ann Lange Professor Youxue Zhang Associate Professor Steven M. Yalisove Matthew Rahn Manon 2008 Acknowledgments Cheers to all the grad students who have gone and come through CC-Little over the years. Zeb, Steven, Jim, Chris, Katy, Phillip, Franek, Eric, Tom, Darius, Sarah, Sara, Abir, Laura, Casey, Sam, John and anyone else I’ve been to learned something from, or argued something with. From early nights at Dominicks for subductology “seminars” through to the FWC, Michigan has been a fun place to live. Thanks to Anne Hudon, whos made sure I haven’t been able to place myself in inextricable holes. Thanks also to those from earlier in my life. College professors like Ken Hess or Barbara Nimmersheim who, in their very different ways inspired me to explore what it is I know. I’ll always remember time spent with Bob Wiebe who introduced me to the wild unknown of geology. Immeasurable thanks go to Eric Essene. The fieldtrips we took the first few years were good adventures. He’s always put aside his own issues to be there for me to talk to, especially when I didn’t deserve it. Eric’s scientific curiosity, and mental rigor are deservedly well known. His patience with me may be one of his great, unsung virtues. -
Hydrothermal and Metamorphic Berthierine
n27 CanadianMineralogist Vol. 30,pp. 1127-1142 (1992) HYDROTHERMALAND METAMORPHICBERTHIERINE FROM THE KIDD CREEK VOLCANOGENICMASSTVE SULFIDE DEPOSIT. TIMMINS, ONTARIO JOHNF.SLACK U.S.Geological Survey, Nationnl Center, Mail Stop954, Reston, Virginia 22092, U.S.A. WEI-TEH JIANG ANDDONALD R. PEACOR Depamnent of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, U.S.A. PATRICKM. OKITA* U.S.Geological Survey, National Center,Mail Stop954, Reston,Virginia 22092,U.S.A. ABSTRACT Berthierine,a 7 A pe-Al memberof the serpentinegroup, occursin the footwall stringerzone of the ArcheanKidd Creek massivesulfide deposit, Ontario, associated with quartz,muscovite, chlorite, pyrite, sphalerite,chalcopyrite, and local tourmaline' cassiterite,and halloysite. Berthierine has been identified by the lack of 14A basalreflections on X-ray powderdiffractionpattems, by its composition (electron-microprobedata), and by transmissionelectron microscopy (TEM). Peoogaphic and scanning eiectronmicroscopic (SEM) studiesreveal different types of berthierineocculrences, including interlayerswithin and rims on deformedchlorite, intergrowthswith muscoviteand halloysite,and discretecoarse grains. TEM imagesshow thick packetsof berthierineand chlorite that are parallel or relatedby low-angle boundaries,and layer terminationsof chlorite by berthierine; mixedJayer chlorite-berthierinealso is observed,intergrown with Fe-rich chlorite and berthierine.End-member (Mg-free) berthierineis presentin small domainsin two samples.The Kidd Creekberthierine is chemicallysimilar -
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 -
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 -
Iron.Rich Amesite from the Lake Asbestos Mine. Black
Canodian Mineralogist Yol.22, pp. 43742 (1984) IRON.RICHAMESITE FROM THE LAKE ASBESTOS MINE. BLACKLAKE. OUEBEC MEHMET YEYZT TANER,* AND ROGER LAURENT DAporternentde Gdologie,Universitd Loval, Qudbec,Qudbec GIK 7P4 ABSTRACT o 90.02(1l)', P W.42(12)',1 89.96(8)'.A notreconnais- sance,c'est la premibrefois qu'on ddcritune am6site riche Iron-rich amesite is found in a metasomatically altered enfer. Elles'ct form€ependant l'altdration hydrothermale granite sheet20 to 40 cm thick emplacedin serpentinite of du granitedans la serpentinite,dans les m€mes conditions the Thetford Mi[es ophiolite complex at the Lake Asbestos debasses pression et temperaturequi ont prdsid6d la for- mine (z16o01'N,11"22' W) ntheQuebec Appalachians.The mation de la rodingite dansle granite et de I'amiante- amesiteis associatedsdth 4lodingife 6semblage(grossu- chrysotiledans la serpentinite. lar + calcite t diopside t clinozoisite) that has replaced the primary minerals of the granite. The Quebec amesite Mots-clds:am6site, rodingite, granite, complexeophio- occurs as subhedral grains 2@ to 6@ pm.in diameter that litique, Thetford Mines, Qu6bec. have a tabular habit. It is optically positive with a small 2V, a 1.612,1 1.630,(t -'o = 0.018).Its structuralfor- INTRoDUc"iloN mula, calculated from electron-microprobe data, is: (Mg1.1Fe6.eA1s.e)(Alo.esil.df Os(OH)r.2. X-ray powder- Amesite is a raxehydrated aluminosilicate of mag- diffraction yield data dvalues that are systematicallygreater nesium in which some ferrous iron usually is found than those of amesitefrom Chester, Massachusetts,prob- replacingmapesium. The extent of this replacement ably becauseof the partial replacement of Mg by Fe. -
The Stability, Electronic Structure, and Optical Property of Tio2 Polymorphs
The stability, electronic structure, and optical property of TiO2 polymorphs Tong Zhu and Shang-Peng Gaoa) Department of Materials Science, Fudan University, Shanghai 200433, P. R. China Phonon density of states calculation shows that a new TiO2 polymorph with tridymite structure is mechanically stable. Enthalpies of 9 TiO2 polymorphs under different pressure are presented to study the relative stability of the TiO2 polymorphs. Band structures for the TiO2 polymorphs are calculated by density functional theory with generalized gradient approximation and the band energies at high symmetry k-points are corrected using the GW method to accurately determine the band gap. The differences between direct band gap energies and indirect band gap energies are very small for rutile, columbite and baddeleyite TiO2, indicating a quasi-direct band gap character. The band gap energies of baddeleyite (quasi-direct) and brookite (direct) TiO2 are close to that of anatase (indirect) TiO2. The band gap of the newly predicted tridymite-structured TiO2 is wider than the other 8 polymorphs. For optical response calculations, two-particle effects have been included by solving the Bethe-Salpeter equation for Coulomb correlated electron-hole pairs. TiO2 with cotunnite, pyrite, and fluorite structures have optical transitions in the visible light region. I. INTRODUCTION 1,2 Even after half a century of research, investigation of the fundamental properties of TiO2 crystal phases remains very important properly due to their important role to effectively utilize solar energy. For instance, 3 4 photocatalytic splitting of water into H2 and O2, photovoltaic generation of electricity, degradation of 5,6 7 environmentally hazard materials, and reduction of CO2 into hydrocarbon fuels.