Download the Scanned

Total Page:16

File Type:pdf, Size:1020Kb

Download the Scanned TNDEX TO VOLUME 33 Leading articles are in boid face type; notes, abstracts and reviews are in ordinary type. Only minerals for which definite data are given are indexed. pH, Abrasion feld test for distin- Ballast sands of Japaneseballoons, Suishins minerals (Stevens, mineralogy of (Ross). 207 Carron). 31 Bannister,F. A... ..98,249,787 Absolute intensity scale for crystal Barium titanate, crystallographyof diffraction data (Harker). 764 the polymorphic forms of. Achromatization of diffraction (Evans, Burbank) 758 lines.(Ekstein, Siegel)...... lJl Barium titanate, ferroelectric ac- Acta Crystallographica,Vol. l, Pt. tivitiesof. (Matthias)....... 769 1. (Review) 514 Barium titanate, permanent polar- Adamite from Ojuela Mine, Ma- iztion of a single crystal of. pimi (Mrose). Notes on oc- (de Bretteville, Levin, Estelle) 754 (Mayers, culrence Wise) 449 Barksdale,J. D.. 192 Ahrens, L.H.. 19r Barrett,C. S.... 749 Allen, V. T., and f,'ahey, J. J., Barshad, I. Vermiculite and its Mansfieldite, a new arsenare relation to biotite. 655 the aluminum analogue of Barth, T. F. W. Memorial of Gre- scorodite,and the mansfieldite- gori Aminofi. 166 scorodite series. t22 193 191 Basaluminite(Bannister, Hollings- AlPOa, crystal structure of. (Brill, worth). .. 787 de Bretteville) 750 Bear,R.S...... .. 749 Aluminum, role of, in rock-forming Becke line colors, use in refractive silicates. (Thompson) 2Og index deterrnination (Em- Aminofi, G., memorial of. (Barth). 166 mons, Gates). 612 Ammonium and potassium molyb- Becquerelite and billietite, addi- dotellurates.(Evans)... 758 tional data on. (Schoep, Stra- Anatase in fireclay deposits. aliot)... 503 (Brindley,Robinson). .. 94 Berry, L. G., and Graham, A. R,, Andrews,K.W....... 652 X-ray measurements on Angelelli,V......... 653 brackebuschite and hemato- Anthoinite. (Varlamofi) 3S5 lite.... 489 Anthophyllite series, new study of. ......193,750 (Rabbitt). 263 Billietite and becquerelite, addi- Atacamite twinning re-examined. tional data on (Schoep, Stra- (Donnay) 7s5 diot)... 503 Axelrod, J. M., X-ray data on Billietite.(Vaes). ........ 384 mansfieldite, aluminian scoro- Biographical notices of mineralo- dite and scorodite. 133 gists recently deceased(1939- 195 47) (Spencer) 94 Blyth, F. G. H., Pyroxene from Bader, H. Degrees of freedom of Squitver dolerite, South simple symmetry operations. 642 Shropshire.. 652 Bailly, R. Infra-red light for min- Bolduan,O. E. A.. 749 eral deternrination.... .192,Slg Boldyrev, A. K., memorial of. Ball, S. H., and Graf, D. L., with (Poir6)..... 516 Kerr, P. F. Carbonado from Bond, W. L., Transformation of Venezuela. ...... .. 2Sl axes.. 703 791 INDEX Bosazza, V. L., Petrography and Clay minerals, rehydration and de- Petrology of South African hydration of. (Grirn' BradleY) 50 Clays.Bookreview. ... 650 Clinopyroxenes, optical Property Bowen,N.L...... ..193,210 curves.(Hess). 199 Brackebuschite and hernatolite, Collagen fibrils, nature of the order r-ray measurements on. (Ber- of large size exhibited by, ry, Graham). 489 (Bear, Bolduan) 749 Bradley, W. F., with Grim, R. E., Collagen, water uptake as evi- Rehydration and dehydration denced by its low angle *-ray of clay minerals. 50 diffraction pattern. (Wright). 780 Brasseur, If., Properties and Conductivity of dilute water solu- chemical formula of fourrnari- tions near critical temPera- erite. 619 ture. (Owen, Swinnerton).. 204 Brazilianite, second occuffence of. Connolly, J. P., memorial of. (Frondel,Lindberg). .135, 196 (Graton). 172 Rredigite.(Tilley, Vincent). 786 Cornwallite,(Berry) 193 Brill, R. 750,751 Corundum deposits,'l-urret, Chaf- Brindley,G.W... ,. 94 fee Co., Colo. (Heinrich, Grif- Bromehead,C. E. N.. 653 fitts)..... 199 Burbank,R. D.. 758 Crystal chemistry of elementsfrom Buttgenbach,H. Les Min6raux de actinium to americium.(Zach- Belgique et du Congo Belge. ariasen) 783 Bookreview.... 382 Crystallographic data, collection Buerger, M. J., The role of tem- and publicationof. (McCrone) 770 peraturein mineralog5r. .101, 193 Crystallographic elements, rela- Structural nature of min- tionsamong.(Evans)... 60 eralizer action of fluorine and (Corrections) 380 hydroxyl 74+ Crystallographic Society of Amer- with Ilamburger, G. E. ica Proceedings 749 oftourmaline Cummingtoniteanalyses and r-raY _tr*o*" 1t1iil, data... .288'309 Curved crystal monochromator Ca:SiOr, high temperature orth- for study of low angle scatter- orhombic form, in Scawt ing. (Guinier, Fournet) 759 Hill contact zone, and in slags. Cuspidinein the systemCaO.SiOz (Tilley, Vincent) 94 . CaFg. (McCaughey, Kautz, Carbonado from Venezuela, (Kerr Wells).... 2OO Graf,Ball)... 251 Custerite-Cuspidine.('tilley) ... 100 Carl, H. F. Reliability of x-ray diffraction spectrometer for Dark-feld color immersion meth- quantitative mineral analyses 645 orl.(Dodge)... 194,541 Carron, M. K., wit! Stevens, R. E. Darneal, R. L, Immersion media Sirnple field test for distin- containing methylene iodide. 346 gurshing minerals by abrasion Davisson,J.W..... 754 pII. ... 31 de Bretteville,A., J... ... .. .. 754 Chako,N.. 753 Decaborane,crystal structure of. Chapman, C. A. Memorial of Ter- (Kasper, Luicht, Harker) . 768 ence Thomas Quirke. 178 Degrees of freedom of simple sym: Chrysotile, thermal decornposition metry operations.(Bader)... 642 of.(Hey,Bannister)........ 249 Diderichite.(Vaes). 385 INDEX 793 Diorite, gabbro and related rocks, Falkmanite and yenerite, identity definitionsof. (Ellis). 652 with boulangerite. (Robinson) 716 Discreditedminerals. ..100,386, 654 Fankuchen, I.. 77s Dolomites,siliceous, earlier stages Faust, G. T. Therrnal analysis of in metamorphismof. (Tilley). 94 quartz and its use in calibra- Dodge, N. B. Dark-field color im- tion in therrnal atralysis studies JJ/ mersion method. .194, 541 Feldspar, introduction in Red Donnay, J. D.H. Book review. 382 River district, N. Mex. (Park, McKinlay) 204 Donohue,J. 756 Feldspar, use in petrofabric analy- Dunham,K.C....... 249 sis of igneous rocks. (Snyder) 208 Druif,J. H.. 787 Fenimore, C. P. 755 Dry silicatesystems, present status Ferquson, R. 8.. 195 of laboratory studies.(Schairer) 207 Festschrift for Paul Niggli. (Re- view)....... 785 Earley,J.W.......' 194 Fire hazard with C. D. West's high Egli, P. H. Survey of inorganic refractive index liquids. (Mil- piezoelectric materials. 622 ton). 512 Ekstein,H..... 757 Fluorite-rare earth mineral peg- Electronicdigital computer.(Gold- matites of Chaffee and Fre- stine)...... 759 mont Counties, Colo. (Ifein- Ellis,S. E.. 652 rich). 6+ Elpasoiite aad hagemannite, new Foshag,W. F.. 195 data on. (Frondel). 84 Foster, W. R. Useful aspects of the Emmons, R, C., and Gates, R. M. fluorescenceof zircon... .196,724 Use of Becke line colors in re- Fourier analysis, punched card fractive index deterination. 612 methodsof. (Thomas) 777 Bookreview...., 96 Fourier synthesizer, electronic. Erickson,M. P., with Stringham,B. (Pepinsky) 771 'Ihermal metamorphismof til- Fourier transforms, application to lite at Alta, Utah. 369 a crYstal structure anall'sis. Eruptive rocks. (Shand) Book re- (wrinch). 782 vierv...... 517 Fourmarierite, Properties and Estelle,H.. 754 chemical compositior of. (Brasseur). 619 Ir,ulite.(Poldervaarl ) . 99 . Fox,P. P.... 196 Evans, H. T., Jr. Relations among crystallographic ele- Fournct,G... 759 ments. 60 Francd, R. R., and Loewenstein, (Corrections) 380 W. Zirconium from the region Unit cell and spacegroup of Pogos de Caldas 142 of pirssonite. 261 Franckeite in relation to lengen- /J6 bachite(Nuffield)... 203 Frederickson, A. F. Differential 372 Fahey, J. J., with Allen, V. T. thermal curve of siderite '... Mansfieldite. A new arsenate, Mode of occurrence of ti- the aluminum analogue of tanium and zirconium in lat- scoroditeand the mansfieldite- erites . Jt+ scoroditeseries,....... 122 Frondel, C. New data on elPaso- 195,205 lite and hagemannite.. ..... 84 794 INDEX Tourrnaline pressure Venezuela. 251 gauges. I Graham, A. R.., with Berry, L. G. / .).t X-ray measurements on J, and Lindberg, M. L. Sec- brackebtrsdilte and hemato- olilTTi,.,nulite.... 489 :ii :""":::""' Graton, L. C. Memorial of Joseph P. Connolly. 172 Gardener, L. with Gruner, J. W. Griffitts. w. R.. 199 Book review. 382 Grim, R. E., and Bradley, W. F. Garnet and associated minerals of Rehydration and dehydration Barton Mine, North Creek, of clayminerals............ 50 N. Y., paragenesisof (Shaub). 208 Grossularite,stability relations of. Garnet-idocrase rock, a pseudo- (Yoder) 2ll jade from Placer Co., Cal. Growing crystals from solution. (Rogers) 206 (Holden) 766 'W'. Garrels,R.M... ....... 680 Gruner, J. Progress in silicate Gates, R. M., with Enmons, R. C. structures. 679,759 Use of Becke line colors in 197 refractive inder deterrrina- and Gardiner, L. Book re- tion... 612 view. 382 Geiger counter characteristics, ob- Guinier,A...... ........ 759 servations on, by means of a grid-controlled tc-ray tube. Eagemannite and elpasolite, new (Pepinsky,Long)... .. 772 data on. (Frondel).. ... 84 Geiger counter spectrometer, high Hagner, A. F.. 203 intensity, with extended angu- Hallimond, A. F.. 94 lar range.(Parrish, Hamacher) 770 Hamacher,E. A... ....760,770 Geiger counter spectrometer, im- Ifamburger, G. E., and Buerger, proved. (Hamacher, Parrish) 760 M. J. Stnrcture of tourmaline. Geiger counter spectrometer, pre- .5s2,76r ferred orientation and sample Harker,D.. .. .. ....762,763,764,768 preparation for. (Pr6vot, Harrison, J. M.. 197 Schwarz) 773 Hawley,J.E.... ........ 198 Gems and Gem Materials. (Kraus, Eeirich, E. W. Fluorite-rare earth Slawson)Book review...-.. 382
Recommended publications
  • 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
    [Show full text]
  • Burangaite, a New Phosphate Mineral from Rwanda
    BURANGAITE, A NEW PHOSPHATE MINERAL FROM RWANDA O. von KNORRING, MARTTI LEHTINEN and TH. G. SAHAMA KNORRING, O. von, LEHTINEN, MARTTI and SAHAMA, Th. G. 1977: Burangaite, a new phosphate mineral from Rwanda. BulL GeoL Soc. Finland 49: 33-36. This paper describes a new phosphate, burangaite, from the Buranga pegmatite in Rwanda. Burangaite is monoclinic with the idealized formula (Na,Ca)2 (Fe2+,Mg)2Aho(OH,Oh2(P04)S·4H20, Z = 2. The crystals exhibit narrow, bladed prisms, elongated parallel to the b-axis. Perfect cleavage parallel to 100. Mohs' hardness 5. Streak slightly bluish. 0 Unit-cell data: ao 25.09 A, bo 5.048 A, Co 13.45 A, fJ 110.91 , space group C2Ic. These parameters and the indexed X-ray powder pattern (Table 1) indicate a marked relationship with dufrenite. 0 The mineral is blue in color with y 11 band c /\a = 11 0, 2Va = 58 , strong pleochroism, refractive indices a 1.611, fJ 1.635, Y 1.643. Com­ mon hourglass structure with a blue core and a colorless margin. O. von Knorring, Department of Earth Sciences, Leeds University, Leeds LS2 9JT, England. Martti Lehtinen and Th. G. Sahama, Department of Geology and Mineralogy, University of Helsinki, P.O. Box 115, SF-00170 Hel­ sinki 17, Finland. Introduction commonly associated with bjarebyite (von Knorring and Fransolet 1975), wardite and The occurrence of a long-prismatic bluish other phosphates under study. Wardite occurs phosphate mineral from the Buranga pegma­ as white crystals of pyramidal habit, up to tite, Rwanda, was noted and provisionally 2 mm in size, with dominating {012} and described by one of us (von Knorring 1973).
    [Show full text]
  • On Scorzalite from the Angarf-Sud Pegmatite, Zenaga Plain, Anti-Atlas, Morocco
    Spec. Issue: r Fortschr. 52 IMA-Papers 9th Meeting 285 - 291 Stuugan Miner. Berlin· Regensburg 1974 December 1975 L-- On scorzalite from the Angarf-Sud pegmatite, Zenaga Plain, Anti-Atlas, Morocco Andre.M.thieu Fransolet* With 2 tables Abrtract: Scolzalite occurs frequently but not abundantly in the phosphate minerals from the AngaIf­ Sud Precambrian pegmatite Qutcropping in Zenaga Plain, Anti-Atlas. Morocco. Scorzalite is characterized by a determination of the ratio Fe2 +/ Mg. The value obtained for the ratio FeH/(Fe1+ + Mg) is 0.54. The unit cell dimensions are also given. In the Angarf-Sud pegmatite. the phosphate nodules are zoned. A core of gray triphylite, widely replaced by green alluaudite, is fringed by reddish fine-grained apatite. The more important secondary phosphate minerals are: melonjosephite, barbosalHe, tavorite, lipsco mbite, mitridatite, and rock­ bridgeite. If muscovite occurs in this asseJIlbiage, it is systematically accompanied by scorzaiite and fringed by apatite. Scorzalite replaces muscovite and is inserted in its cleavage. It seems that scorzalite forms under a low oxygen fugacity, more or less simultaneously with Mg­ triphylite. The so lution, rich in P, Fe2 + and with a little Mg, reacts with mica which provides AI; Si02 and K are released. It is not necessary to evoke a metasomatic process to explain the presence of AL Introduction Minerals of the lazulite MgAI,(PO.), (OH), - scorzalite FeAI, (PO.), (OH), isomor· phous series described by Pecora& Fahey (1950), occur rather frequently in pegmatites but they are scarcely abundant. Systematic study of phosphates from Precambrian pegmatites injected in micaschists and gneiss in Zenaga Plain, Anti-Atlas, Morocco, has revealed the occurrence of a mineral belonging to this series in the Angarf·Sud pegmatite.
    [Show full text]
  • Wyllieitej Na2fe~~1 [P04 ]31 a New Species by Paul B
    WyllieiteJ Na2Fe~~1 [P04 ]31 A New Species by Paul B. Moore, Department of the Geophysical Sciences, The University of Chicago, Chicago, Illinois 60637 and Jun Ito Department of Geological Sciences, Harvard University, Cambridge, Massachusetts 02138 INTRODUCTION mention that optical studies indicated a 7(n:, triphylite the After two field and collecting excursions to 102 Black composition. We have good evidence that this phase was Hills pegmatites in the summers of 1971 and 1972, it be­ indeed the wyllieite. A 70% triphylite would have a ml'an he came clear that the Victory mine pegmatite was chemi­ index of refraction around 1.695, the value found hy Pe­ cally unique, so peculiar in fact that a major mineralogical cora and Fahey (1949) for their "triphylitc" fWIll the Vic­ m. investigation is now in progress. Not only is the pegmatite tory mine, the sample of which we found to hc in fact not ile of interest to the mineralogist for an unusual abundance triphylite but wyllieite. This index of refraction i~ practi­ >cr· ., of Na-rich primary phosphates rarely encountered else­ cally identical to our observations on wyllicite. Finally. where, but the textures of the cocrystallizing phases are we remark that our wyllieite specimcns show abundant in themselves a source of interest to petrologists as well. coarse quartz and perlhile as well as the pl;lgioda~e, ~ug­ Our account concerns a new species which evidently oc­ gesting that the mineral crystallized toward the end of thl! curred in considerable abundance during operation of the wall zone formation and during early core cot1\olidation.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • Master Thesis
    Master Thesis Degree Project in Geology 60 hp Protolith of a kyanite-bearing, quartz-rich rock in Hålsjöberg, western Sweden Andreas Sjöqvist Stockholm 2017 Department of Geological Sciences Stockholm University SE-106 91 Stockholm Table of Content Abstract ............................................................................................................................. 4 Sammanfattning ................................................................................................................ 6 Introduction ....................................................................................................................... 7 Previous research and findings ..................................................................................................................................... 8 Methods .......................................................................................................................... 11 Fieldwork ............................................................................................................................................................................. 11 Sample preparation ......................................................................................................................................................... 11 Results ............................................................................................................................. 13 Outcrop map ......................................................................................................................................................................
    [Show full text]
  • New Mineral Names*
    American Mineralogist, Volume 59, pages 873-475, 1974 NEWMINERAL NAMES* Mrcnapl Frprscnpn Bjarebyite* Borovskite* P. B. MooRE, D. H. LuNo, eNo K, L. KBrsrBn (1923) A. A. Yerovor, A. F. Sroonov, N. S. RuomnEvsKrr AND Bjarebyite, (Ba,Sr)(Mn,Fe,Mg),AL(Olt)s(por)a a new I. A. Buo'ro (1973) Borovskite, PdSbTer, ? n€w mineral. species. Mineral. Rec. 4, 282-285, Zapiski Vses.Mineral. Obshch. 102, 427431 (in Russian). Microprobe pure Microprobe analysis by G. Z. Zecttnan gave (av. 60 area analyses, using metals and BirTer as standards, on 4 grains gave scan) Ba 21.81, Sr O.79, Ca 0.06, Mn 7.15, Fe 6.95, Pd 32.94, 31.90, 32.37, 32.37, av. 32.39; Pt. 1.21, 1.25, 1.23, Mg 0.84, Al 7.01, giving the formula above with pOr and 1.20, av. 1.23; Ni 0.26, O.24,0.26, O.25,av.0.25; Fe OH on the basis of the structure. The ratio Mn/Fe is 0.04, 0.04, 0.06, 0.02, av. 0.04; Sb 1,0.92,10.97, 11.01, 11.00, av. 10.98; variable, indicating the likelihood of the occurrence of an Bi 3.35,3.34,3.34, Fe'g*analogue. av. 3.34; Te 51.86, 52.39, 51.70, 51.93, av. 51.97; sum 100.58, 99.98, percent, Weissenberg and rotation photographs show the mineral 10O.14, 100.11, av. 10O.21 corre- sponding to (Pd" (Sbo to be monoclinic, space grotp P2r/m, a 8.930, b lZ.O73, 6PtowNio orFeo o.) *Bio ru)Te" or, or PdaSbTe+.
    [Show full text]
  • The Corrego Frio Pegmatite, Minas Gerais
    THE CORREGOFRIO PEGMATITE, MINAS GERAIS: SCORZALITEAND SOUZAI.ITE,TWO NEW PHOSPHATEMINERALS1 Wrr-r-rRuT. Pncone aNo Josnrn J. Fannv, U. S. GeologicalSuraey, Washington, D. C. Tlst-n or CoNrnNts Introduction and acknowledgments. 83 Location 84 History. 85 Regionalgeology..... 85 The CorregoFrio Pegmatite. ..... 86 Descriptive mineralogy. 88 Minerals in the pegmatite . .. 88 Scorzalite 88 Souzalite.. 88 Brazilianite. 91 Otherminerals. 92 Genesis. 93 References 93 Asstnecr This paper describes the structure and mineralogy of a pegmatite that has yielded three new phosphate minerals in recent years. The pegmatite is well zoned into three structural units of characteristic texture and mineral association. The minerals present include albite, muscovite, quartz, scorzalite (new mineral), souzalite (new mineral), brazilianite, apatite, zircon, tapiolite, and two unidentified phosphate minerals. Detailed descriptions, with chemical analyses, are given for scorzalite and souzatte, both of which are hydrous iron magnesium aluminum phosphates. Scorzalite is isomorphous with lazulite; the structural relationships of souzalite are not known. INrnopucrtoN AND AcrNowr-BUcMENTS This paper contains a detailed description of the structure and mineral- ogy of the Corrego Frio pegmatite, Minas Gerais, BtaziT, which has yielded three new phosphate minerals since its discovery in t942. Two of these new minerals, scorzalite and souzalite, are described in this paper. Additional information on brazilianite, described in 1945,is also presented. The authors are indebted to a number of colleaguesin the Section of Geochemistry and Petrology, U. S. Geological Survey, for courteous as- sistancein mineral study. K. J. Murata made spectrographic analysesof scorzalite and souzalite that served as a guide for the chemical analyses by Fahey. J. M.
    [Show full text]
  • Vibrational Spectroscopy of the Phosphate Mineral Lazulite €“ (Mg
    Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 107 (2013) 241–247 Contents lists available at SciVerse ScienceDirect Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy journal homepage: www.elsevier.com/locate/saa Vibrational spectroscopy of the phosphate mineral lazulite – (Mg, Fe)Al2(PO4)2Á(OH)2 found in the Minas Gerais, Brazil ⇑ Ray L. Frost a, , Yunfei Xi a, Martina Beganovic b, Fernanda Maria Belotti c, Ricardo Scholz b a School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia b Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG 35400-00, Brazil c Federal University of Itajubá, Campus Itabira, Itabira, MG 35903-087, Brazil highlights graphical abstract " In this work, we have studied the structure of lazulite. " Lazulite is pegmatite phosphate with calculated formula (Fe0.11)Al1.86(PO4)2.08(OH)2.04. " The structure of lazulite was assessed using a combination of Raman and infrared spectroscopy. article info abstract Article history: This research was done on lazulite samples from the Gentil mine, a lithium bearing pegmatite located in the Received 20 September 2012 municipality of Mendes Pimentel, Minas Gerais, Brazil. Chemical analysis was carried out by electron Received in revised form 6 November 2012 microprobe analysis and indicated a magnesium rich phase with partial substitution of iron. Traces of Ca Accepted 23 January 2013 and Mn, (which partially replaced Mg) were found. The calculated chemical formula of the studied sample Available online 1 February 2013 is: (Mg0.88,Fe0.11)Al1.87(PO4)2.08(OH)2.02.
    [Show full text]
  • Lacroixite Naal(PO4)F C 2001-2005 Mineral Data Publishing, Version 1
    Lacroixite NaAl(PO4)F c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Rough crystals, to 1 cm; as druses, massive. Physical Properties: Cleavage: Indistinct on {111} and {111}. Hardness = 4.5 D(meas.) = 3.29 D(calc.) = 3.29 Optical Properties: Transparent. Color: Gray, pale yellow to pale green, almost white; colorless in transmitted light. Luster: Vitreous, pearly on cleavages. Optical Class: Biaxial (–). Dispersion: r< v.α= 1.546(1) β = 1.563(1) γ = 1.580(1) 2V(meas.) = 89(1)◦ 2V(calc.) = 89.1◦ Cell Data: Space Group: C2/c. a = 6.414 b = 8.207 c = 6.885 β = 115.47◦ Z=4 X-ray Powder Pattern: Greifensteine, Germany. 3.155 (100), 2.895 (98), 2.476 (57), 4.73 (51), 2.166 (43), 4.627 (32), 1.578 (27) Chemistry: (1) (2) P2O5 44.7 43.30 Al2O3 32.1 31.09 Na2O 16.4 18.90 F 12.3 11.59 −O=F2 5.17 4.88 Total 100.3 100.00 (1) Greifensteine, Germany; by electron microprobe; (OH)1− absent by IR and structure analysis. (2) NaAl(PO4)F. Occurrence: In druses in granite (Greifensteine, Germany); an alteration product rimming natromontebrasite in a complex granite pegmatite (Rusororo, Rwanda). Association: Morinite, viitaniemiite, apatite, childrenite, roscherite, feldspar, tourmaline, quartz (Greifensteine, Germany); montebrasite, scorzalite, berlinite (Rusororo pegmatite, Rwanda); apatite, augelite, brazilianite, natromontebrasite (Strickland quarry, Connecticut, USA). Distribution: Large crystals [from the Koppar quarry,] on the Greifensteine, near Ehrenfriedersdorf, Saxony, Germany. At L´aznˇe Kynzvart, near Mari´ansk´e L´aznˇe (K¨onigswart, near Marienbad), and Jeˇclov, near Jihlava, Czech Republic.
    [Show full text]
  • Lazulite Mgal2(PO4)2(OH)2 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Monoclinic
    Lazulite MgAl2(PO4)2(OH)2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As crystals, stubby to acute dipyramidal with forms {111}, {111}, {101}, to 15 cm, or tabular on {111} or {101}, with several other forms noted; granular, massive. Twinning: Common on {100} with composition plane {001} and marked re-entrant, occasionally producing lamellar or polysynthetic groups; rare on {223};by reflection on {221} with composition plane {331}; several other twin laws reported. Physical Properties: Cleavage: Poor to good on {110}; indistinct on {101}. Fracture: Uneven to splintery. Tenacity: Brittle. Hardness = 5.5–6 D(meas.) = 3.122–3.240 D(calc.) = 3.144 Optical Properties: Transparent to translucent, may be nearly opaque. Color: Azure-blue, sky-blue, bluish white, yellow-green, blue-green, rarely green. Streak: White. Luster: Vitreous. Optical Class: Biaxial (–). Pleochroism: Strong; X = colorless; Y = blue; Z = darker blue. Orientation: Y = b; X ∧ c =10◦. Dispersion: r< v,weak. Absorption: Z > Y X. α = 1.604–1.626 β = 1.626–1.654 γ = 1.637–1.663 2V(meas.) = ∼70◦ Cell Data: Space Group: P 21/c. a = 7.144(1) b = 7.278(1) c = 7.228(1) β = 120.50(1)◦ Z=2 X-ray Powder Pattern: Werfen, Austria; nearly identical to scorzalite. 3.23 (100), 3.20 (59), 3.14 (55), 3.077 (42), 4.73 (18), 2.548 (18), 1.571 (18) Chemistry: (1) (2) (1) (2) P2O5 45.79 44.64 FeO 3.95 11.30 TiO2 0.20 MgO 10.38 6.34 Al2O3 32.49 32.06 CaO 0.06 Fe2O3 0.60 H2O 6.48 5.66 Total 99.95 100.00 (1) Graves Mountain, Georgia, USA.
    [Show full text]
  • List of Mineral Symbols
    THE CANADIAN MINERALOGIST LIST OF SYMBOLS FOR ROCK- AND ORE-FORMING MINERALS (January 1, 2021) ____________________________________________________________________________________________________________ Ac acanthite Ado andorite Asp aspidolite Btr berthierite Act actinolite Adr andradite Ast astrophyllite Brl beryl Ae aegirine Ang angelaite At atokite Bll beryllonite AeAu aegirine-augite Agl anglesite Au gold Brz berzelianite Aen aenigmatite Anh anhydrite Aul augelite Bet betafite Aes aeschynite-(Y) Ani anilite Aug augite Bkh betekhtinite Aik aikinite Ank ankerite Aur auricupride Bdt beudantite Akg akaganeite Ann annite Aus aurostibite Beu beusite Ak åkermanite An anorthite Aut autunite Bch bicchulite Ala alabandite Anr anorthoclase Aw awaruite Bt biotite* Ab albite Atg antigorite Axn axinite-(Mn) Bsm bismite Alg algodonite Sb antimony Azu azurite Bi bismuth All allactite Ath anthophyllite Bdl baddeleyite Bmt bismuthinite Aln allanite Ap apatite* Bns banalsite Bod bohdanowiczite Alo alloclasite Arg aragonite Bbs barbosalite Bhm böhmite Ald alluaudite Ara aramayoite Brr barrerite Bor boralsilite Alm almandine Arf arfvedsonite Brs barroisite Bn bornite Alr almarudite Ard argentodufrénoysite Blt barylite Bou boulangerite Als alstonite Apn argentopentlandite Bsl barysilite Bnn bournonite Alt altaite Arp argentopyrite Brt baryte, barite Bow bowieite Aln alunite Agt argutite Bcl barytocalcite Brg braggite Alu alunogen Agy argyrodite Bss bassanite Brn brannerite Amb amblygonite Arm armangite Bsn bastnäsite Bra brannockite Ams amesite As arsenic
    [Show full text]