The Mineralogy and Geochemistry of the Green Giant Vanadium-Graphite Deposit, S.W
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Roscoelite K(V ; Al; Mg)2Alsi3o10(OH)2 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
3+ Roscoelite K(V ; Al; Mg)2AlSi3O10(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: As minute scales, in druses, rosettes, or fan-shaped groups; ¯brous and in felted aggregates; as impregnations, massive. Physical Properties: Cleavage: Perfect on 001 . Hardness = Soft. D(meas.) = 2.92{2.94 D(calc.) = [2.89] f g Optical Properties: Transparent to translucent. Color: Dark clove-brown, greenish brown to dark greenish brown. Luster: Pearly. Optical Class: Biaxial ({). Pleochroism: X = green-brown; Y = Z = olive-green. ® = 1.59{1.610 ¯ = 1.63{1.685 ° = 1.64{1.704 2V(meas.) = 24.5±{39.5± Cell Data: Space Group: C2=c: a = 5.26 b = 9.09 c = 10.25 ¯ = 101:0± Z = 2 X-ray Powder Pattern: Paradox Valley, Colorado, USA. 10.0 (100), 4.54 (80), 3.35 (80), 2.60 (80), 1.52 (60), 3.66 (50), 3.11 (50) Chemistry: (1) SiO2 47.82 Al2O3 12.60 V2O5 19.94 FeO 3.30 MgO 2.43 CaO trace Na2O 0.33 K2O 8.03 + H2O 5.13 Total 99.58 (1) Stuckslager mine, California, USA. Polymorphism & Series: Forms a series with muscovite; 1M polytype. Mineral Group: Mica group. Occurrence: An early-stage gangue mineral in low-temperature epithermal Au-Ag-Te deposits; from the oxidized portions of low-temperature sedimentary U-V ores. Association: Quartz, pyrite, carbonates, °uorite, gold (Au-Ag-Te mineral association); corvusite, hewettite, carnotite, tyuyamunite (U-V mineral association). Distribution: In the USA, from the Stuckslager mine, Lotus, El Dorado Co., California; in Colorado, from Cripple Creek, Teller Co., La Plata district, La Plata Co., Magnolia district, Boulder Co., the Gateway district, Mesa Co., in the Uravan and Paradox, Bull Canyon, and Slick Rock districts, in Montrose, San Miguel, and Dolores Cos. -
Spectral Evolution Gold Exploration
spectral evolution Gold Exploration SPECTRAL EVOLUTION’s oreXpress and oreXpress Platinum with EZ-ID software for mineral identification are well-suited for gold exploration. These rugged, field spectrometers can be used in field mapping and mineral identification for many different gold deposit types, including: Paleoplacer deposits Massive sulfides Hot spring deposits Low sulfidation High sulfidation Breccia pipes Porphyry gold deposits Skarns Orogenic deposits Carbonate placements Greenstone belts oreXpress and oreXpress Platinum spectrometers are ideal With our oreXpress spectrometers and EZ-ID software, geologists can scan and identify for single-user field exploration in common alteration minerals, such as: gold mining. For low sulfidation: illite, kaolinite, chlorite, illite/smectite, buddingtonite, epidote, montmorillonite, zeolite, quartz, calcite, hematite For high sulfidation: alunite, opal, dickite, pyrophyllite, diaspora, zunyite, topaz, illite, kaolinite, chlorite, epidote, quartz, montmorillonite, goethite, jaosite, hematite For orogenic gold: muscovite, paragonite muscovite, roscoelite, illite, kaolinite, quartz, siderite, ankerite, calcite, dolomite, carbonates Using EZ-ID with the USGS spectral library, or the SpecMIN™ library available from Spectral International, the software quickly provides accurate matching of an unknown target with a known mineral spectra. With an oreXpress spectrometer and EZ-ID a geologist can identify minerals indicating gold in real-time, in the field. Benefits include: Quickly collect a lot of scans EZ-ID software identifies minerals Cover more ground in less time for better mapping in real-time by matching your Collect more accurate data for a more complete picture of the area target spectra against a known you are exploring spectral library such as the USGS Get results immediately instead of waiting for lab analysis library, or the SpecMIN library. -
CORVUSITE and RILANDITE, NEW MINERALS from the UTAH-COLORADO CARNOTITE REGIOI{ Eowenn P
CORVUSITE AND RILANDITE, NEW MINERALS FROM THE UTAH-COLORADO CARNOTITE REGIOI{ Eowenn P. HBNonnsoNAND Fnaxr L. Hnss,x U. S. National, Museum. InrnonucrroN In the carnotite-bearing depositsof Colorado and Utah the sand- stone and accompanying clays are impregnated with many dark brown and black mineral masses,which show no crystal form to the unaided eye and few other definite characteristics. The most common of the dark colored minerals are listed below. Roscoelite vanadium mica Rauvite CaO'2UOr'6VzOr'2OHrO Vanoxite 2VzOr'VzOs(S* )HzO Corvusite VrOr'6VeOs'XH:O Rilandite hydrouschromium aluminum silicate Lignite Tar (?) Asphaltite Psilomelane Iron-copper-cobaltoxide. Two of the names, corvusite and rilandite, are new and are pro- posed in this paper. The authors hesitated to give names to such compounds as those to which they are applied becauseno entirely satisfactory formula can be ofiered for either, but since the sub- stance called corvusite is common in the carnotite region a verbal handle seemsnecessary. Rilandite, although at present known from only one locality, was obtained in rather large quantity and its as- sociation is such that it seemslikely that it will be obtained from other places in the carnotite region. If at some future date further study shows these names unnecessarythey can easily be relegated to oblivion. Gr,Nnner, Rnr.attoNsrups Roscoelite or a similar dark mineral is provisionally identifiable by the microscope from many places in this region. Roscoelite is well known, rauvite and vanoxitel and the asphaltitez have been * Published by permission of the Secretary of the Smithsonian Institution. I Hess, Frank L., New and known minerals from the Utah-Colorado carnotite region: U. -
Alkalic-Type Epithermal Gold Deposit Model
Alkalic-Type Epithermal Gold Deposit Model Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. Department of the Interior U.S. Geological Survey Cover. Photographs of alkalic-type epithermal gold deposits and ores. Upper left: Cripple Creek, Colorado—One of the largest alkalic-type epithermal gold deposits in the world showing the Cresson open pit looking southwest. Note the green funnel-shaped area along the pit wall is lamprophyre of the Cresson Pipe, a common alkaline rock type in these deposits. The Cresson Pipe was mined by historic underground methods and produced some of the richest ores in the district. The holes that are visible along several benches in the pit (bottom portion of photograph) are historic underground mine levels. (Photograph by Karen Kelley, USGS, April, 2002). Upper right: High-grade gold ore from the Porgera deposit in Papua New Guinea showing native gold intergrown with gold-silver telluride minerals (silvery) and pyrite. (Photograph by Jeremy Richards, University of Alberta, Canada, 2013, used with permission). Lower left: Mayflower Mine, Montana—High-grade hessite, petzite, benleonardite, and coloradoite in limestone. (Photograph by Paul Spry, Iowa State University, 1995, used with permission). Lower right: View of north rim of Navilawa Caldera, which hosts the Banana Creek prospect, Fiji, from the portal of the Tuvatu prospect. (Photograph by Paul Spry, Iowa State University, 2007, used with permission). Alkalic-Type Epithermal Gold Deposit Model By Karen D. Kelley, Paul G. Spry, Virginia T. McLemore, David L. Fey, and Eric D. Anderson Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. -
MINERAL POTENTIAL REPORT for the Lands Now Excluded from Grand Staircase-Escalante National Monument
United States Department ofthe Interior Bureau of Land Management MINERAL POTENTIAL REPORT for the Lands now Excluded from Grand Staircase-Escalante National Monument Garfield and Kane Counties, Utah Prepared by: Technical Approval: flirf/tl (Signature) Michael Vanden Berg (Print name) (Print name) Energy and Mineral Program Manager - Utah Geological Survey (Title) (Title) April 18, 2018 /f-P/2ft. 't 2o/ 8 (Date) (Date) M~zr;rL {Signature) 11 (Si~ ~.u.. "'- ~b ~ t:, "4 5~ A.J ~txM:t ;e;,E~ 't"'-. (Print name) (Print name) J.-"' ,·s h;c.-+ (V\ £uA.o...~ fk()~""....:r ~~/,~ L{ ( {Title) . Zo'{_ 2o l~0 +(~it71 ~ . I (Date) (Date) This preliminary repon makes information available to the public that may not conform to UGS technical, editorial. or policy standards; this should be considered by an individual or group planning to take action based on the contents ofthis report. Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding it!I suitability for a panicular use. The Utah Department ofNatural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users ofthis product. TABLE OF CONTENTS SUMMARY AND CONCLUSIONS ........................................................................................................... 4 Oil, Gas, and Coal Bed Methane ........................................................................................................... -
Tungsten Minerals and Deposits
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 652 4"^ TUNGSTEN MINERALS AND DEPOSITS BY FRANK L. HESS WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Page. Introduction.............................................................. , 7 Inquiries concerning tungsten......................................... 7 Survey publications on tungsten........................................ 7 Scope of this report.................................................... 9 Technical terms...................................................... 9 Tungsten................................................................. H Characteristics and properties........................................... n Uses................................................................. 15 Forms in which tungsten is found...................................... 18 Tungsten minerals........................................................ 19 Chemical and physical features......................................... 19 The wolframites...................................................... 21 Composition...................................................... 21 Ferberite......................................................... 22 Physical features.............................................. 22 Minerals of similar appearance................................. -
Geology, Geochemistry, and Mineralogy of the Ridenour Mine Breccia Pipe, Arizona
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology, Geochemistry, and Mineralogy of the Ridenour Mine Breccia Pipe, Arizona by Karen J. Wenrich1 , Earl R. Verbeek 1 , Hoyt B. Sutphin2 , Peter J. Modreski 1 , Bradley S. Van Gosen 11, and David E. Detra Open-File Report 90-0504 This study was funded by the Bureau of Indian Affairs in cooperation with the Hualapai Tribe. 1990 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. U.S. Geological Survey 2U.S. Pollution Control, Inc. Denver, Colorado Boulder, Colorado CONTENTS Page Abstract ................................................................... 1 Introduction ............................................................... 2 Geology and structure of the Ridenour mine ................................. 5 Structural control of the Ridenour and similar pipes ....................... 7 Mine workings ............................................................. 11 Geochemistry .............................................................. 11 Metals strongly enriched at the Ridenour pipe ......................... 23 Vanadium ......................................................... 23 Silver ........................................................... 30 Copper ........................................................... 30 Gallium .......................................................... 30 Isotopic studies ...................................................... 30 Mineralogy ............................................................... -
Petrological, Mineralogical, Fluid Inclusion and Stable Isotope Characteristics of the Tuvatu Gold-Silver Telluride Deposit, Upper Sabeto River Area, Fiji
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1-1-2002 Petrological, mineralogical, fluid inclusion and stable isotope characteristics of the Tuvatu gold-silver telluride deposit, upper Sabeto River area, Fiji Nancy L. Scherbarth Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Recommended Citation Scherbarth, Nancy L., "Petrological, mineralogical, fluid inclusion and stable isotope characteristics of the Tuvatu gold-silver telluride deposit, upper Sabeto River area, Fiji" (2002). Retrospective Theses and Dissertations. 21314. https://lib.dr.iastate.edu/rtd/21314 This Thesis is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Petrological, mineralogical, fluid inclusion and stable isotope characteristics of the Tuvatu gold-silver telluride deposit, upper Sabeto River area, Fiji by Nancy L. Scherbarth A thesis submitted to the graduate faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Major: Geology Program of Study Committee: Paul G. Spry, Major Professor Karl E. Seifert C. Lee Burras Iowa State University Ames, Iowa 2002 11 Graduate College Iowa State University This is to certify that the master's thesis of Nancy Lee Scherbarth has met the thesis requirements of Iowa State University Signatures have been redacted for privacy lll This thesis is dedicated in loving memory to my stepfather, Norman H. Rybka, who always showed support and interest in my educational and personal endeavors. -
Ana P. Carvalho, Angela Martins, Joao M. Silva, Joao Pires, Helena Vasques and M. Brotas De Carvalho. Characterization of the Acidity of Al-And Zr-Pillared Clays P. Adamo, M. Pigna, S
FORTHCOMING PAPERS The following are some papers that have been accepted for publication in future issues of Clays and Clay Minerals: Victoria C. Hover and Gail M. Ashley. reflectance spectrum in relation to the color and Geochemical signatures of paleodepositional crystal properties of hematite and diagenetic environments: a STEM/AEM Basil Hubbard, Wenxing Kuang, Arvin Moser, study of authigenic clay minerals from an arid Glenn A. Facey and Christian Detellier. rift basin, Olduvai Gorge, Tanzania Structural study of Maya Blue: textural, ther- Christopher Q. Kautz and Peter C. Ryan. The 10 AÊ mal, and solid-state multinuclear magnetic to 7 AÊ halloysite transition in a tropical soil resonance characterization of the palygorksite- sequence, Costa Rica indigo and sepiolite-indigo adducts Aldo Mirabella and Markus Egli. Structural George E. Christidis and Sortiria Kosiari. transformations of clay minerals in soils of a Decolorization of vegetable oils: a study of climosequence in an Italian Alpine environment the mechanism of adsorption of b-carotene by Aydog´an Akbulut and Selahattin Kadir. The geology an acid-activated bentonite from Cyprus and origin of sepiolite, palygorskite and saponite Hadar Heller and Rami Keren. Anionic polyacry- in Neogene lacustrine sediments of the Serinhisar- lamide polymer adsorption by pyrophyllite and Acipayam Basin, Denizli, SW Turkey montmorillonite Chao Shang, James A. Rice, Dennis D. Eberl and Ana P. Carvalho, Angela Martins, Joa˜o M. Silva, Jar-Shyong Lin. Measurement of the illite Joa˜o Pires, Helena Vasques and M. Brotas de particle thickness using a direct Fourier trans- Carvalho. Characterization of the acidity of Al- form of small-angle X-ray scattering data and Zr-pillared clays Maria Franca Brigatti, Enrico Caprilli, Marco P. -
Primary Minerals of the Jáchymov Ore District
Journal of the Czech Geological Society 48/34(2003) 19 Primary minerals of the Jáchymov ore district Primární minerály jáchymovského rudního revíru (237 figs, 160 tabs) PETR ONDRU1 FRANTIEK VESELOVSKÝ1 ANANDA GABAOVÁ1 JAN HLOUEK2 VLADIMÍR REIN3 IVAN VAVØÍN1 ROMAN SKÁLA1 JIØÍ SEJKORA4 MILAN DRÁBEK1 1 Czech Geological Survey, Klárov 3, CZ-118 21 Prague 1 2 U Roháèových kasáren 24, CZ-100 00 Prague 10 3 Institute of Rock Structure and Mechanics, V Holeovièkách 41, CZ-182 09, Prague 8 4 National Museum, Václavské námìstí 68, CZ-115 79, Prague 1 One hundred and seventeen primary mineral species are described and/or referenced. Approximately seventy primary minerals were known from the district before the present study. All known reliable data on the individual minerals from Jáchymov are presented. New and more complete X-ray powder diffraction data for argentopyrite, sternbergite, and an unusual (Co,Fe)-rammelsbergite are presented. The follow- ing chapters describe some unknown minerals, erroneously quoted minerals and imperfectly identified minerals. The present work increases the number of all identified, described and/or referenced minerals in the Jáchymov ore district to 384. Key words: primary minerals, XRD, microprobe, unit-cell parameters, Jáchymov. History of mineralogical research of the Jáchymov Chemical analyses ore district Polished sections were first studied under the micro- A systematic study of Jáchymov minerals commenced scope for the identification of minerals and definition early after World War II, during the period of 19471950. of their relations. Suitable sections were selected for This work was aimed at supporting uranium exploitation. electron microprobe (EMP) study and analyses, and in- However, due to the general political situation and the teresting domains were marked. -
Introduction to Apatites
Chapter 1 Introduction to Apatites Petr Ptáček Additional information is available at the end of the chapter http://dx.doi.org/10.5772/62208 Abstract Apatite is the generic name, which was first introduced by German geologist A.G. Werner. These minerals and their synthetic analogs represent a major class of ionic compounds and the most common crystalline form of calcium phosphates, which are of interest of many industrial branches and scientific disciplines. Since, apatite (fluora‐ patite) is the most abundant phosphate mineral, apatite bearing phosphate rocks represents an important source of inorganic phosphorus. First chapter of this book introduces the basic concepts of nomenclature, composition, classification, crystal structure, mineralogy and properties of minerals from the supergroup of apatite. Furthermore, the minerals from the group of apatite and polysomatic apatites are described. Since, the most of the topics mentioned in this chapter will be developed in the following chapters, the key concepts provided in this chapter are important to understood before proceeding further. Keywords: Apatite, Group of Apatite, Polysomatic Apatites, Fluorapatite, Hydroxyla‐ patite, Chlorapatite, Vanadinite The minerals1 [1],[2],[3],[4],[5] from the apatite group2 [6] are classified as hexagonal or pseudo‐ hexagonal monoclinic anhydrous phosphates containing hydroxyl or halogen of the generic formula3: 1Minerals are individual components comprising rocks formed by geological processes classified according to their crystal structure and chemical composition. The total number of minerals accepted by mineralogical community is about 4000. Mineraloids are mineral-like phases including synthetic materials, human-treated substances, and some biological materials, which do not fulfill the criteria for the definition of mineral species [2]. -
Schreyerite, Vztisoe, a New Mineral
American Mineralogist, Volume 63, pages I182-l 186, 1978 Schreyerite,VzTisOe, a newmineral Orep MnoaNBACH Institut tilr M ineralogie, Ruhr-Uniuersitiit D-4630 Bochum, West Germany ANDKARL Sctrunrznn I nsti tut fitr M ineral ogie, Rupp recht - Karl - Uniu e rs itiit D-6900 H eidelberg, l(est Germany Abstract Schreyerite,a new vanadiumtitanium oxide with the composition(Vo.rrCroo.Alo.0r)2Tisoe givingidealized VrTirOr, is describedfrom the Kwale District, southof Voi, Kenya.The ore mineraloccurs as exsolutionlamellae and particlesin rutile coexistingwith kyanite,sillima- nite, tourmaline,and kornerupinein a highly metamorphosedgneiss. The reflectivityof schreyeriteis 2l percent,and the microhardnessafter Knoop is l100-1200kp/mm,.The d valuesof 4.075(m ), 3.381(m), 2.874(s), 2.737 (vs), and 2.a32(w) suggesta directanalogy to an Anderssonphase (Cro.ruFe6.,u)2TisO" with a monoclinicunit cell. The investigationof a depositof greenvanadium- overlyingweathered zone were collected by Dr. H. bearingkornerupine from Kenya (Schmetzeret al., Krupp, Heidelberg,who visitedthe mine in 1974.The 1974)has revealedthe presenceof a new vanadium strongly weathered,highly metamorphosedgneiss mineral through observationsin reflectedlight. The contains quartz, biotite, tourmaline, diopside,and mineralis calledschreyerite in honour of Professor epidote.The most abundantopaque minerals are Dr. Werner Schreyer,Professor of Mineralogyat graphite and rutile, although traces of pyrrhotite, Ruhr University,Bochum (F.R. Germany),distin- chalcopyrite, and pentlandite are also found. guishedfor his mineralogicaland petrologicalwork Schreyeritealways occurs in intergrowthwith rutile. on kornerupine-and sapphirine-bearingrocks. The The rutile grainsin the gneissreach a diameterof up mineral and its name have been approvedby the to 0.5mmand are partly idiomorphic.The ratio of Commissionof New Mineralsand Mineral Names of schreyeriteto rutile is stronglyvariable.