The Rock Cycle
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US Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR *"! ' 5, GEOLOGICAL SURVEI PEGMATITE GEOLOGY OF THE SHELBY DISTRICT NORTH CAROLINA by \ Wallace R. Griffitts > \ I ,' -* U. S. Geological Survey ' ' OPEN FILE REPORT 5 Ihis report is preliminary and has not been edited or reviewed for conformity with Geological Suj'V*-'/ standards or nomenclature. COHTEHTS _ _ - Page Abstract Introduction. ........................... 1 Location and physical features ................ 1 Field work and acknowledgments ................ 2 Geology .............................. k Metamorphic rocks....................... h- Carolina gneiss ..................... Ij- General features .................. ^4- Lithology. ..................... k Biotite gneiss member. ............... 6 Battleground schist ................... 9 General features .................. 9 Lithology. ..................... 9 Hornblende schist and gneiss. .............. 11 General features .................. 11 Gabbroic rocks ................... 11 Hornblende schists ................. 13 Pyroxenite and associated rocks. .......... 13 Schist and granite complex. ................ 14- Igneous rocks. ........................ 15 Toluca quartz monzonite ................. 15 . : .r *- General features .................. 15 ^ c Lithology. ..................... 16 Yorkville granite .................... 19 General features .................. 19 Lithology. ..................... 20 Page CherryvlUe quartz monzonite. ............. 20 General features ................. 20 Relations to enclosing rocks ........... 23 Lithology. -
Iseite, Mn2mo3o8, a New Mineral from Ise, Mie Prefecture, Japan
Journal of Mineralogical and PetrologicalIseite, a new Sciences, mineral Volume 108, page 37─ 41, 2013 37 LETTER Iseite, Mn2Mo3O8, a new mineral from Ise, Mie Prefecture, Japan * ** ** *** Daisuke NISHIO-HAMANE , Norimitsu TOMITA , Tetsuo MINAKAWA and Sachio INABA * The institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan ** Department of Earth Science, Faculty of Science, Ehime University, Matsuyama, Ehime 790-8577, Japan *** Inaba-Shinju Corporation, Minamiise, Mie 516-0109, Japan Iseite, Mn2Mo3O8, a new mineral that is a Mn-dominant analogue of kamiokite, is found in the stratiform ferro- manganese deposit, Shobu area, Ise City, Mie Prefecture, Japan. It is the first mineral species that includes both Mn and Mo as essential constituents. Iseite is iron-black in color and has a submetallic luster. It occurs as ag- gregates up to about 1 mm in size made of minute crystals (<20 μm). Iseite has a zoned structure closely associ- ated with undetermined Mn-Fe-Mo oxide minerals with hexagonal forms, and it occasionally coexists with 3 small amounts of powellite. Its Mohs hardness is 4-5, and its calculated density is 5.85 g/cm . The empirical formula of iseite is (Mn1.787Fe0.193)Σ1.980Mo3.010O8. Its simplified ideal formula is written as Mn2Mo3O8. The min- eral is isostructural with kamiokite (hexagonal, P63mc). The unit cell parameters are a = 5.8052 (3) Å, c = 10.2277 (8) Å, V = 298.50 (4) Å3, and Z = 2. The Rietveld refinement using synchrotron radiation (λ = 0.413 Å) powder XRD data converges to Rwp = 3.11%, and confirms two independent Mn sites—tetrahedral and octahe- IV VI dral—in the crystal structure of iseite, indicating the structure formula Mn Mn Mo3O8. -
Redalyc.Mineralogical Study of the La Hueca Cretaceous Iron-Manganese
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Corona Esquivel, Rodolfo; Ortega Gutiérrez, Fernando; Reyes Salas, Margarita; Lozano Santacruz, Rufino; Miranda Gasca, Miguel Angel Mineralogical study of the La Hueca Cretaceous Iron-Manganese deposit, Michoacán, south-western Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 142-151 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217206 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 143 2000, p. 143- 153 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F MINERALOGICAL STUDY OF THE LA HUECA CRETACEOUS IRON- MANGANESE DEPOSIT, MICHOACÁN, SOUTHWESTERN MEXICO Rodolfo Corona-Esquivel1, Fernando Ortega-Gutiérrez1, Margarita Reyes-Salas1, Rufino Lozano-Santacruz1, and Miguel Angel Miranda-Gasca2 ABSTRACT In this work we describe for the first time the mineralogy and very briefly the possible origin of a banded Fe-Mn deposit associated with a Cretaceous volcanosedimentary sequence of the southern Guerrero terrane, near the sulfide massive volcanogenic deposit of La Minita. The deposit is confined within a felsic tuff unit; about 10 meters thick where sampled for chemical analysis. Using XRF, EDS and XRD techniques, we found besides todorokite, cryptomelane, quartz, romanechite (psilomelane), birnessite, illite-muscovite, cristobalite, chlorite, barite, halloysite, woodruffite, nacrite or kaolinite, and possibly hollandite-ferrian, as well as an amorphous material and two unknown manganese phases. -
Rhodochrosite Gems Unstable Colouration of Padparadscha-Like
Volume 36 / No. 4 / 2018 Effect of Blue Fluorescence on the Colour Appearance of Diamonds Rhodochrosite Gems The Hope Diamond Unstable Colouration of in London Padparadscha-like Sapphires Volume 36 / No. 4 / 2018 Cover photo: Rhodochrosite is prized as both mineral specimens and faceted stones, which are represented here by ‘The Snail’ (5.5 × 8.6 cm, COLUMNS from N’Chwaning, South Africa) and a 40.14 ct square-cut gemstone from the Sweet Home mine, Colorado, USA. For more on rhodochrosite, see What’s New 275 the article on pp. 332–345 of this issue. Specimens courtesy of Bill Larson J-Smart | SciAps Handheld (Pala International/The Collector, Fallbrook, California, USA); photo by LIBS Unit | SYNTHdetect XL | Ben DeCamp. Bursztynisko, The Amber Magazine | CIBJO 2018 Special Reports | De Beers Diamond ARTICLES Insight Report 2018 | Diamonds — Source to Use 2018 The Effect of Blue Fluorescence on the Colour 298 Proceedings | Gem Testing Appearance of Round-Brilliant-Cut Diamonds Laboratory (Jaipur, India) By Marleen Bouman, Ans Anthonis, John Chapman, Newsletter | IMA List of Gem Stefan Smans and Katrien De Corte Materials Updated | Journal of Jewellery Research | ‘The Curse Out of the Blue: The Hope Diamond in London 316 of the Hope Diamond’ Podcast | By Jack M. Ogden New Diamond Museum in Antwerp Rhodochrosite Gems: Properties and Provenance 332 278 By J. C. (Hanco) Zwaan, Regina Mertz-Kraus, Nathan D. Renfro, Shane F. McClure and Brendan M. Laurs Unstable Colouration of Padparadscha-like Sapphires 346 By Michael S. Krzemnicki, Alexander Klumb and Judith Braun 323 333 © DIVA, Antwerp Home of Diamonds Gem Notes 280 W. -
LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, and COBALT ARSENIDE and SULFIDE ORE FORMATION Nicholas Allin
Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2019 EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION Nicholas Allin Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geotechnical Engineering Commons EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION by Nicholas C. Allin A thesis submitted in partial fulfillment of the requirements for the degree of Masters in Geoscience: Geology Option Montana Technological University 2019 ii Abstract Experiments were conducted to determine the relative rates of reduction of aqueous sulfate and aqueous arsenite (As(OH)3,aq) using foils of copper, nickel, or cobalt as the reductant, at temperatures of 150ºC to 300ºC. At the highest temperature of 300°C, very limited sulfate reduction was observed with cobalt foil, but sulfate was reduced to sulfide by copper foil (precipitation of Cu2S (chalcocite)) and partly reduced by nickel foil (precipitation of NiS2 (vaesite) + NiSO4·xH2O). In the 300ºC arsenite reduction experiments, Cu3As (domeykite), Ni5As2, or CoAs (langisite) formed. In experiments where both sulfate and arsenite were present, some produced minerals were sulfarsenides, which contained both sulfide and arsenide, i.e. cobaltite (CoAsS). These experiments also produced large (~10 µm along longest axis) euhedral crystals of metal-sulfide that were either imbedded or grown upon a matrix of fine-grained metal-arsenides, or, in the case of cobalt, metal-sulfarsenide. Some experimental results did not show clear mineral formation, but instead demonstrated metal-arsenic alloying at the foil edges. -
George Robert Rossman Feb 15, 1995
George Robert Rossman 20-Jun-2020 Present Position: Professor of Mineralogy Option Representative for Geochemistry Division of Geological and Planetary Sciences California Institute of Technology Pasadena, California 91125-2500 Office Telephone: (626)-395-6471 FAX: (626)-568-0935 E-mail: [email protected] Residence: Pasadena, California Birthdate: August 3, l944, LaCrosse, Wisconsin Education: B.S. (Chemistry and Mathematics), Wisconsin State University, Eau Claire, 1966, Summa cum Laude Ph.D. (Chemistry), California Institute of Technology, Pasadena, 1971 Experience: California Institute of Technology Division of Geological and Planetary Sciences a) 1971 Instructor in Mineralogy b) 1971-1974 Assistant Professor of Mineralogy and Chemistry c) 1974-1977 Assistant Professor of Mineralogy d) 1977-1984 Associate Professor of Mineralogy e) 1984-2008 Professor of Mineralogy f) 2008-2015 Eleanor and John R. McMillan Professor of Mineralogy e) 2015- Professor of Mineralogy Principal Research Interests: a) Spectroscopic studies of minerals. These studies include problems relating to the origin of color phenomena in minerals; site ordering in crystals; pleochroism; metal ions in distorted sites; analytical applications. b) The role of low concentrations of water and hydroxide in nominally anhydrous solids. Analytical methods for OH analysis, mode of incorporation, role of OH in modifying physical and chemical properties, and its relationship to conditions of formation in the natural environment. c) Long term radiation damage effects in minerals from background levels of natural radiation. The effects of high level ionizing radiation on minerals. d) X-ray amorphous minerals. These studies have involved the physical chemical study of bioinorganic hard parts of marine organisms and products of terrestrial surface weathering, and metamict minerals. -
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 Industries and Geology of Certain Areas
REPORT -->/ OF TFIE STATE GEOLOGIST ON THE S 7 (9 Mineral Industries and Geology 12 of Certain Areas OF -o VERMONT. 'I 6 '4 4 7 THIRD OF THIS SERIES, 1901-1902. 4 0 4 S GEORGE H. PERKINS, Ph. D., 2 5 State Geologist and Professor of Geology, University of Vermont 7 8 9 0 2 4 9 1 T. B. LYON C0MI'ANV, I'RINTERS, ALILiNY, New VORK. 1902. CONTENTS. PG K 1NTRODFCTION 5 SKETCH OF THE LIFE OF ZADOCK THOMPSON, G. H. Perkins ----------------- 7 LIST OF OFFICIAL REPORTS ON VERMONT GEOLOGY ----------------- -- -- ----- 14 LIST OF OTHER PUBLICATIONS ON VERMONT GEOLOGY ------- - ---------- ----- 19 SKETCH OF THE LIFE OF AUGUSTUS WING, H. M. Seely -------------------- -- 22 REPORT ON MINERAL INDUSTRIES, G. H. Perkins ............................ 35 Metallic Products ------------------------------------------------------ 32 U seful Minerals ------------------------------------------------------- 35 Building and Ornamental Stone ----------------------------------------- 40 THE GRANITE AREA OF BAItRE, G. I. Finlay------------------------------ --- 46 Topography and Surface Geology ------------------------------------ - -- 46 General Geology, Petrography of the Schists -------------------------- - -- 48 Description and Petrography of Granite Areas ----------------------------51 THE TERRANES OF ORANGE COUNTY, VERMONT, C. H. Richardson ------------ 6i Topography---------------------------- -............................. 6z Chemistry ------------------------------------------------------------66 Geology -------------------------------------------------------------- -
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 -
Holdawayite Mn (CO3)
2+ Holdawayite Mn6 (CO3)2(OH)7(Cl, OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Fibrous along [001]; commonly in granular aggregates, or massive, with individual grains to 2 cm. Physical Properties: Cleavage: On {100}, perfect. Fracture: Irregular. Tenacity: Moderately brittle. Hardness = ∼3 D(meas.) = 3.19(4) D(calc.) = 3.24 Optical Properties: Transparent to translucent. Color: Pale to dark pink if fresh, turning brown on exposure, developing a dark sooty coating. Streak: Pale pink. Luster: Vitreous, silky in fibrous aggregates. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c = 45(3)◦. Dispersion: r< v,moderate. α = 1.644(1) β = 1.719(1) γ = 1.721(1) 2V(meas.) = 12(3)◦ 2V(calc.) = 18◦ Cell Data: Space Group: C2/m. a = 23.437(5) b = 3.3137(3) c = 16.618(6) β = 111.15(2)◦ Z=4 X-ray Powder Pattern: Kombat mine, Namibia. 10.93 (100), 5.459 (80), 3.879 (70), 2.690 (60b), 2.589 (50b), 7.77 (40), 2.926 (40) Chemistry: (1) CO2 14.2 B2O3 1.2 FeO 0.2 MnO 64.6 MgO 4.4 CaO 0.5 Cl 4.4 H2O 11.47 −O=Cl2 1.0 Total 100.0 (1) Kombat mine, Namibia; by electron microprobe, C by Leco analyzer, H2O by the Penfield method, B may be due to sussexite contamination; corresponds to (Mn5.24Mg0.62 Ca0.06Fe0.02)Σ=5.94[(CO3)1.86(BO3)0.20]Σ=2.06[(OH)7.34Cl0.74]Σ=8.08. Occurrence: Locally abundant as a rare vein mineral in low-grade metamorphosed Mn-rich sedimentary rocks intercalated with sedimentary iron deposits. -
List of New Mineral Names: with an Index of Authors
415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis. -
Sussexite Mn2+BO2(OH)
2+ Sussexite Mn BO2(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As bladed acicular crystals, to 7 mm; cross-vein or radial fibrous, in felted or matted aggregates, nodular. Twinning: Submicroscopic twinning on {100} which cannot be resolved optically. Physical Properties: Tenacity: Inflexible. Hardness = 3–3.5 D(meas.) = 3.30 D(calc.) = 3.335 Optical Properties: Semitransparent. Color: White to buff, straw-yellow, pale pink; colorless in transmitted light. Streak: White. Luster: Silky, dull, earthy. Optical Class: Biaxial (–). Orientation: Parallel extinction; X = elongation; Z ⊥ flattening. Dispersion: r> v. α= 1.670 β = 1.728 γ = 1.732 2V(meas.) = ∼25◦ Cell Data: Space Group: P 21/a. a = 12.866(3) b = 10.718(2) c = 3.287(1) β =94.75(3)◦ Z=8 X-ray Powder Pattern: N’chwaning II mine, South Africa. 6.43 (10), 2.773 (7), 3.34 (6), 2.632 (6), 2.494 (6), 2.741 (5), 2.694 (5) Chemistry: (1) (3) B2O3 30.52 30.33 FeO 0.16 MnO 49.40 61.82 MgO 9.56 CaO 2.03 H2O 8.33 7.85 Total [100.00] 100.00 (1) Franklin, New Jersey, USA; recalculated to 100% after deduction of willemite 4.5%. (2) N’chwaning II mine, South Africa; by electron microprobe, analysis not given; stated to correspond to (Mn0.95Mg0.05)Σ=1.00BO2(OH). (3) MnBO2(OH). Polymorphism & Series: Forms a series with szaib´elyite. Occurrence: A rare hydrothermal mineral typically in veinlets in boron-bearing metamorphosed Mn–Fe–Zn deposits.