Glossary of Obsolete Mineral Names
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Impact of High Temperatures on Aluminoceladonite Studied by Mössbauer, Raman, X-Ray Diffraction and X-Ray Photoelectron Spectroscopy
Title: Impact of high temperatures on aluminoceladonite studied by Mössbauer, Raman, X-ray diffraction and X-ray photoelectron spectroscopy Author: Mariola Kądziołka-Gaweł, Maria Czaja, Mateusz Dulski, Tomasz Krzykawski, Magdalena Szubka Citation style: Kądziołka-Gaweł Mariola, Czaja Maria, Dulski Mateusz, Krzykawski Tomasz, Szubka Magdalena. (2021). Impact of high temperatures on aluminoceladonite studied by Mössbauer, Raman, X-ray diffraction and X-ray photoelectron spectroscopy. “Mineralogy and Petrology” (Vol. 115, iss. 0, 2021, s. 1- 14), DOI: 10.1007/s00710-021-00753-z Mineralogy and Petrology (2021) 115:431–444 https://doi.org/10.1007/s00710-021-00753-z ORIGINAL PAPER Impact of high temperatures on aluminoceladonite studied by Mössbauer, Raman, X-ray diffraction and X-ray photoelectron spectroscopy Mariola Kądziołka-Gaweł1 & Maria Czaja2 & Mateusz Dulski3,4 & Tomasz Krzykawski2 & Magdalena Szubka1 Received: 9 March 2020 /Accepted: 28 April 2021 / Published online: 18 May 2021 # The Author(s) 2021 Abstract Mössbauer, Raman, X-ray diffraction and X-ray photoelectron spectroscopies were used to examine the effects of temperature on the structure of two aluminoceladonite samples. The process of oxidation of Fe2+ to Fe3+ ions started at about 350 °C for the sample richer in Al and at 300 °C for the sample somewhat lower Al-content. Mössbauer results show that this process may be associated with dehydroxylation or even initiate it. The first stage of dehydroxylation takes place at a temperature > 350 °C when the adjacent OH groups are replaced with a single residual oxygen atom. Up to ~500 °C, Fe ions do not migrate from cis- octahedra to trans-octahedra sites, but the coordination number of polyhedra changes from six to five. -
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 -
Factors Responsible for Crystal Chemical Variations in The
American Mineralogist, Volume 95, pages 348–361, 2010 Factors responsible for crystal-chemical variations in the solid solutions from illite to aluminoceladonite and from glauconite to celadonite VICTOR A. DRITS ,1 BELL A B. ZV I A GIN A ,1 DOUGL A S K. MCCA RTY,2,* A N D ALFRE D L. SA LYN 1 1Geological Institute of the Russian Academy of Science, Pyzhevsky per. 7, 119017 Moscow, Russia 2Chevron ETC, 3901 Briarpark, Houston, Texas 77063, U.S.A. AB STR A CT Several finely dispersed low-temperature dioctahedral micas and micaceous minerals that form solid solutions from (Mg,Fe)-free illite to aluminoceladonite via Mg-rich illite, and from Fe3+-rich glauconite to celadonite have been studied by X-ray diffraction and chemical analysis. The samples have 1M and 1Md structures. The transitions from illite to aluminoceladonite and from glauconite to celadonite are accompanied by a consistent decrease in the mica structural-unit thickness (2:1 layer + interlayer) or csinβ. In the first sample series csinβ decreases from 10.024 to 9.898 Å, and in the second from 10.002 to 9.961 Å. To reveal the basic factors responsible for these regularities, struc- tural modeling was carried out to deduce atomic coordinates for 1M dioctahedral mica based on the unit-cell parameters and cation composition. For each sample series, the relationships among csinβ, maximum and mean thicknesses of octahedral and tetrahedral sheets and of the 2:1 layer, interlayer distance, and variations of the tetrahedral rotation angle, α, and the degree of basal surface corruga- tion, ∆Z, have been analyzed in detail. -
(12) United States Patent (10) Patent No.: US 8,367,760 B1 Wang Et Al
US008367760B1 (12) United States Patent (10) Patent No.: US 8,367,760 B1 Wang et al. (45) Date of Patent: Feb. 5, 2013 (54) NON-BLACK RUBBER MEMBRANES 3,842,111 A 10/1974 Meyer-Simon et al. 3,873,489 A 3, 1975 Thurn et al. 3,978, 103 A 8/1976 Meyer-Simon et al. (75) Inventors: Hao Wang, Copley, OH (US); James A. 3,997,581 A 12/1976 Petka et al. Davis, Westfield, IN (US); William F. 4,002,594 A 1/1977 Fetterman Barham, Jr., Prescott, AR (US) 5,093,206 A 3, 1992 Schoenbeck 5,468,550 A 11/1995 Davis et al. (73) Assignee: Firestone Building Products Company, 5,580,919 A 12/1996 Agostini et al. LLC, Indianapolis, IN (US) 5,583,245 A 12/1996 Parker et al. 5,663,396 A 9, 1997 Musleve et al. 5,674,932 A 10/1997 Agostini et al. (*) Notice: Subject to any disclaimer, the term of this 5,684, 171 A 11/1997 Wideman et al. patent is extended or adjusted under 35 5,684, 172 A 11/1997 Wideman et al. U.S.C. 154(b) by 207 days. 5,696, 197 A 12/1997 Smith et al. 5,700,538 A 12/1997 Davis et al. 5,703,154 A 12/1997 Davis et al. (21) Appl. No.: 12/389,145 5,804,661 A 9, 1998 Davis et al. 5,854,327 A * 12/1998 Davis et al. ................... 524,445 (22) Filed: Feb. 19, 2009 6,579,949 B1 6/2003 Hergenrother et al. -
Mineral Fundort (Location) Quality Habit Size Qty
Exchange list Elmar Lackner 22.03.2016 This is my exchange/trade list for advanced Collectors. All specimens are of good quality or rarity (sometimes both). Please accept that this minerals are only exchanged with comparable minerals ! Some rare Micromounts are small, but i don't use capsules (marked with small). Some hygroscopic minerals are sealed in glass-vials (mainly from Tolbachik vulcano) Quality: A = very good, B= good, C= acceptable Habit: xx = crystals, x= crystal, (xx) = intergrown crystals, (x) = intergrown crystal, oo= no crystals Sizes (Box Size !): MM: european Micromount Box, KS1 = Box 40*35*30mm, KS2 = 58*40*35mm, KS3 = 82*58*36mm, KS4 = 82*58*63mm, KS5 = 96*80*50mm Qty.: available specimens Mineral Fundort (Location) Quality Habit Size Qty. Prices More Info Adamite Tsumeb Mine, Otjikoto, Namibia B XX KS2 1 29 € green xls (Var. Cuproadamite) Adamite Mina Ojuela, Mapimi, Durango, Mexiko A XX KS3 1 15 € rich speciomen complety covered wid pale green xls Adamite (Var. Alumo-) Serpieri Mine, Laurion, Greece A+ xx MM 1 9 € very nice blue clusters on white matrix Akanthite Fresnillo, Zacatecas, Mexico A xx KS1 1 15 € xx up to 4 mm Akanthite Freiberg Distr., Erzgebirge, Sachsen, Germany A xx MM 1 9 € xx Albite Poudrette Quarry, MSH, Quebec, Kanada A+ XX KS4 1 19 € very rich specimen, pale pink crystals up to 5mm Allanpringite (Typl.) Grube Mark, Essershausen, Hessen, Germany B+ xx KS1 1 15 € rare one locality mineral, with Kakoxen and Wavellite Aluminopyracmonite (Typl.) La Fossa Crater, Vulcano, Sizilien, Italy B xx KS1, MM -
Glossary of Obsolete Mineral Names
L.120 = clay, Robertson 22 (1954). laavenite = låvenite, Dana 6th, 375 (1892). labite = palygorskite, AM 22, 811 (1937). laboentsowiet = labuntsovite-Mn, Council for Geoscience 765 (1996). laboita = vesuvianite, de Fourestier 191 (1999). laboundsovite = labuntsovite-Mn, Kipfer 181 (1974). labountsovite = labuntsovite-Mn, MM 35, 1141 (1966). Labrador (Frankenheim) = meionite, Egleston 118 (1892). labrador (Rose) = Na-rich anorthite, MM 20, 354 (1925). Labrador-Bytownit = Na-rich anorthite, Hintze II, 1513 (1896). labradore-stone = Na-rich anorthite, Kipfer 181 (1974). Labrador feldspar = Na-rich anorthite, Dana 6th, 334 (1892). Labrador-Feldspat = Na-rich anorthite, Kipfer 107 (1974). Labrador-Feldspath = Na-rich anorthite, Clark 383 (1993). labrador-felspar = Na-rich anorthite, Clark 383 (1993). Labrador hornblende = Fe-rich enstatite or Mg-rich ferrosilite, AM 63, 1051 (1978). labradorische Hornblende = Fe-rich enstatite or Mg-rich ferrosilite, Dana 6th, 348 (1892). Labradoriserende Feltspat = Na-rich anorthite, Zirlin 71 (1981). labradorite (intermediate) = Na-rich anorthite, Dana 6th, 334 (1892). labradorite-felsite = Na-rich anorthite, Dana 6th, 334 (1892). labradorite-moonstone = gem Na-rich anorthite, Schumann 164 (1977). Labradorit-Mondstein = gem Na-rich anorthite, Chudoba EIV, 48 (1974). labradorkő = Na-rich anorthite, László 155 (1995). labrador moonstone = gem Na-rich anorthite, Read 131 (1988). Labrador oder schillerenden rauten förmigen Feldspath = chrysotile ± lizardite or talc or anthophyllite, Clark 620 (1993). labrador schiller spar = Fe-rich enstatite or Mg-rich ferrosilite, Egleston 162 (1892). labrador spar = gem Na-rich anorthite, Read 131 (1988). Labradorstein = Na-rich anorthite, Dana 6th, 334 (1892). labrador stone = Na-rich anorthite, Chester 149 (1896). labradownite = Na-rich anorthite, Kipfer 181 (1974). labratownite = Na-rich anorthite, AM 11, 138 (1926). -
Synthetic Hypersilicic Cl-Bearing Mica in the Phlogopite-Celadonite
American Mineralogist, Volume 93, pages 1429-1436, 2008 Synthetic hypersilicic Cl-bearing mica in the phlogopite-celadonite join: A multimethodical characterization of the missing link between di- and tri-octahedral micas at high pressures SABRINA NAZZARENI,!'* PAOLA COMODI,! LUCA BINDI,2 OLEG G. SAFONOV,3 YURIY A. LITVIN,3 AND LEONID L. PERCHUK3,4 'Department of Earth Sciences, University ofPerugia, Perugia, Italy 'Museo di Storia Naturale, Sezione di Mineralogia, Universita di Firenze, Via La Pira 4, 1-50121, Firenze, Italy 3Institute of Experimental Mineralogy, Chemogolovka, Moscow, Russia "Department of Petrology, Moscow State University, Moscow, Russia ABSTRACT A hypersilicic Cl-bearing mica was synthesized at 4 GPa and 1200-1250 °C, close to the solidus of the join diopside-jadeite-KCl, in association with diopside-jadeite pyroxene, K-rich alumino silicate glass and/or sanidine and (K,Na)Cl. The mica shows a negative correlation between tetrahedral Si and octahedral (AI + Mg), suggesting an Al-celadonitic substitution (Si + VIAl+ VIO = IVAI+ VIMg) and a chemical formula: Kl01(Mg245AlolDo35h~lSi352Alo48h~401O[(OH,0)166Clo34)h~2' The presence of hydroxyl was confirmed by OH stretching modes at 3734 and 3606 cm' in the Raman spectra. Single- crystal X-ray diffraction data provide the unit-cell parameters (space group C2/m, 1M polytype): a = 5.299(4), b = 9.167(3), C = 10.226(3) A, ~ =100.06(4)°, V= 489.1(4) N. The structure refinement shows the presence of vacancies on the octahedral sites (15% for Ml and 6.5% for M2). Chlorine occupies a position about 0.5 A from 04 with partial occupancy (0.39 apfu). -
Angol-Magyar.Pdf
MINEROFIL KISKÖNYVTÁR V. Fehér Béla ÁSVÁNYKALAUZ 2. -
Shin-Skinner January 2018 Edition
Page 1 The Shin-Skinner News Vol 57, No 1; January 2018 Che-Hanna Rock & Mineral Club, Inc. P.O. Box 142, Sayre PA 18840-0142 PURPOSE: The club was organized in 1962 in Sayre, PA OFFICERS to assemble for the purpose of studying and collecting rock, President: Bob McGuire [email protected] mineral, fossil, and shell specimens, and to develop skills in Vice-Pres: Ted Rieth [email protected] the lapidary arts. We are members of the Eastern Acting Secretary: JoAnn McGuire [email protected] Federation of Mineralogical & Lapidary Societies (EFMLS) Treasurer & member chair: Trish Benish and the American Federation of Mineralogical Societies [email protected] (AFMS). Immed. Past Pres. Inga Wells [email protected] DUES are payable to the treasurer BY January 1st of each year. After that date membership will be terminated. Make BOARD meetings are held at 6PM on odd-numbered checks payable to Che-Hanna Rock & Mineral Club, Inc. as months unless special meetings are called by the follows: $12.00 for Family; $8.00 for Subscribing Patron; president. $8.00 for Individual and Junior members (under age 17) not BOARD MEMBERS: covered by a family membership. Bruce Benish, Jeff Benish, Mary Walter MEETINGS are held at the Sayre High School (on Lockhart APPOINTED Street) at 7:00 PM in the cafeteria, the 2nd Wednesday Programs: Ted Rieth [email protected] each month, except JUNE, JULY, AUGUST, and Publicity: Hazel Remaley 570-888-7544 DECEMBER. Those meetings and events (and any [email protected] changes) will be announced in this newsletter, with location Editor: David Dick and schedule, as well as on our website [email protected] chehannarocks.com. -
MUSCOVITE Which Grades Into “Sericite” at Depth (Klein, 1939)
1939). 4. Arcadian mine (Klein, 1939). 5. Kearsarge lode: Generally found with “adularia,” MUSCOVITE which grades into “sericite” at depth (Klein, 1939). KAl2AlSi3O10(OH)2 6. Wolverine mine, Kearsarge: Variety “sericite” A widespread and abundant mica. It occurs in (Morris, 1983). 7. Quincy mine: Dark green, igneous rocks (granites and granitic pegmatites), waxy, barrel-shaped pseudohexagonal crystals up metamorphic rocks (slates, phyllites, mica schists, to 1 cm (pseudomorphous after chlorite?) occurred and micaceous gneisses), sediments and in a large pocket of calcite crystals associated with sedimentary rocks (chiefly sands and some native copper on the 7th level, approximately 100 sandstones), wall rocks of various ore deposits, and meters NE from the Number 2 Shaft. as a replacement of various primary silicates Iron County: Iron River district: As the 2M1 (plagioclase, andalusite, etc.) as the variety type in oxidized iron formation (Bailey and Tyler, “sericite.” 1960). Muscovite is widespread in the Portage Lake Keweenaw County: 1. Central mine: “Sericite” Volcanics of the Keweenaw (often referred to as forms tan, velvety coatings on calcite. 2. “sericite”) in a variety of parageneses (Livnat, Northeast of Gay: In Jacobsville Sandstone in 1983). While the varietal name “sericite” has been section 16, T56N, R30W; contains 1.5 to 4% used for any fine-grained muscovite, it is best Cr2O3 and ~1% V2O3 (L. L. Babcock, personal applied to secondary fine-grained muscovite that communication). 3. Dan’s Point, section 27, has replaced other pre-existing silicates by low- T59N, R27W: A very fine-grained vanadian temperature potassium metasomatism. “Phengite” muscovite occurs with calcite in veinlets less than 1 defines a series of potassium micas with mm thick on the faces of bleached joints in a silty compositions intermediate between muscovite and Keweenawan sandstone. -
The New IMA List of Minerals – a Work in Progress – Updated: March 2020
The New IMA List of Minerals – A Work in Progress – Updated: March 2020 In the following pages of this document a comprehensive list of all valid mineral species is presented. The list is distributed (for terms and conditions see below) via the web site of the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association, which is the organization in charge for approval of new minerals, and more in general for all issues related to the status of mineral species. The list, which will be updated on a regular basis, is intended as the primary and official source on minerals. Explanation of column headings: Name : it is the presently accepted mineral name (and in the table, minerals are sorted by name). CNMMN/CNMNC approved formula : it is the chemical formula of the mineral. IMA status : A = approved (it applies to minerals approved after the establishment of the IMA in 1958); G = grandfathered (it applies to minerals discovered before the birth of IMA, and generally considered as valid species); Rd = redefined (it applies to existing minerals which were redefined during the IMA era); Rn = renamed (it applies to existing minerals which were renamed during the IMA era); Q = questionable (it applies to poorly characterized minerals, whose validity could be doubtful). IMA No. / Year : for approved minerals the IMA No. is given: it has the form XXXX-YYY, where XXXX is the year and YYY a sequential number; for grandfathered minerals the year of the original description is given. In some cases, typically for Rd and Rn minerals, the year may be followed by s.p. -
Nomenclature of the Micas
Mineralogical Magazine, April 1999, Vol. 63(2), pp. 267-279 Nomenclature of the micas M. RIEDER (CHAIRMAN) Department of Geochemistry, Mineralogy and Mineral Resources, Charles University, Albertov 6, 12843 Praha 2, Czech Republic G. CAVAZZINI Dipartimento di Mineralogia e Petrologia, Universith di Padova, Corso Garibaldi, 37, 1-35122 Padova, Italy Yu. S. D'YAKONOV VSEGEI, Srednii pr., 74, 199 026 Sankt-Peterburg, Russia W. m. FRANK-KAMENETSKII* G. GOTTARDIt S. GUGGENHEIM Department of Geological Sciences, University of Illinois at Chicago, 845 West Taylor St., Chicago, IL 60607-7059, USA P. V. KOVAL' Institut geokhimii SO AN Rossii, ul. Favorskogo la, Irkutsk - 33, Russia 664 033 G. MOLLER Institut fiir Mineralogie und Mineralische Rohstoffe, Technische Universit/it Clausthal, Postfach 1253, D-38670 Clausthal-Zellerfeld, Germany A. M, R. NEIVA Departamento de Ci6ncias da Terra, Universidade de Coimbra, Apartado 3014, 3049 Coimbra CODEX, Portugal E. W. RADOSLOVICH$ J.-L. ROBERT Centre de Recherche sur la Synth6se et la Chimie des Min6raux, C.N.R.S., 1A, Rue de la F6rollerie, 45071 Od6ans CEDEX 2, France F. P. SASSI Dipartimento di Mineralogia e Petrologia, Universit~t di Padova, Corso Garibaldi, 37, 1-35122 Padova, Italy H. TAKEDA Chiba Institute of Technology, 2-17-1 Tsudanuma, Narashino City, Chiba 275, Japan Z. WEISS Central Analytical Laboratory, Technical University of Mining and Metallurgy, T/'. 17.1istopadu, 708 33 Ostrava- Poruba, Czech Republic AND D. R. WONESw * Russia; died 1994 t Italy; died 1988 * Australia; resigned 1986 wUSA; died 1984 1999 The Mineralogical Society M. RIEDER ETAL. ABSTRACT I I End-members and species defined with permissible ranges of composition are presented for the true micas, the brittle micas, and the interlayer-deficient micas.