Descriptive Mineralogy Classification of the Minerals Native Elements Native Elements: Metals Native Elements: Non-Metals
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Kennedyite, a New Mineral of the Pseudobrookite Series
676 Kennedyite, a new mineral of the pseudobrookite series. By O. VON KNORRING, Ph.D., and K. G. Cox, Ph.D. Research Institute of African Geology, University of Leeds. [Read 26 January 1961.] Summary. A new mineral with the approximate composition of F%MgTiaOxoand isostructural with pseudobrookite F%Ti2010has been observed in an olivine-augite- alkali-feldsparrock of the Karroo succession from the Mateke Hills area in south- eastern Southern Rhodesia. Chemical analysis and indexed X-ray powder data (a 9"77, b 9-95, c 3"73 ~.) of the mineral are given, and the name kennedyite is pro- posed. The name karrooite is proposed for the artificial product MgTi~O5. HE Mateke Hills area lies in the south-eastern part of Southern T Rhodesia and is characterized by several ring-complexes of late- Karroo age, which are emplaced in an extensive trough of Karroo vol- canics with generally thin basal sediments. The Karroo rocks rest un- conformably on the paragneisses of the Limpopo valley. The lower part of the Karroo volcanic succession consists mainly of olivine-rich rocks. These are in part extrusive and may be termed in general limburgites, and in part intrusive as sills, dykes, and plugs. The intrusive rocks are fine- to medium-grained and vary in composition from olivine-dolerites to pieritic and shonkinitic types. The specimens containing the new mineral were collected from what is believed to be an extensive sill at the base of the volcanic succession immediately overlying the Cave Sandstone. Petrographic description. Under the microscope the rock (table I, anal. 1) consists predominantly of broken and abraded olivine pheno- crysts from 1 to 5 mm. -
Heat Treating Corundum: the Bangkok Operation
HEAT TREATING CORUNDUM: THE BANGKOK OPERATION By Jack S. D. Abraham Following LIP on Nassau's 1981 article on Banglzolz gem dealer buys a lo+-ct ruby for a six- the technical aspects of heat treating ruby A figure sum and heats it hoping to improve its color and sapphire, the author reports his and value. After one heating, the stone dulls and cannot personal observations of the actual heat be sold for half of its original price. But a few tries later treatment process in Bangkok. He the stone is so improved that a major European dealer discusses the potential effects that this buys it for almost five times the original amount- process can have on a stone-both positive and negative-and emphasizes lznowing that it has been heat treated. the importance of the natural make-up of Another Thai dealer pays a large sum for a 600-ct piece the stone itself to the success of heot of sapphire rough. He then cuts it into four sections and treatment. heats each. For the largest piece, which is over 100 ctl he receives 20% more than he paid for the entire original stone-again from a buyer who knows the stone is heated. A third dealer, however, heats a sapphire for which he has paid a six-figure sum but instead of enhancing the color, the treatment causes the stone to brealz into several pieces. It is now worth a fraction of its original price. Such incidents suggest that the heating of ruby and sapphire has become a fully acceptedl if very rislzyl fact of life in the Far East. -
Chromite Deposits of the North Elder Creek Area Tehama County, California
UNITED STATES DEPARTMENT OF THE INTERIOR J. A. Krug, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Bulletin 945-G CHROMITE DEPOSITS OF THE NORTH ELDER CREEK AREA TEHAMA COUNTY, CALIFORNIA By G. A. RYNEARSON Strategic Minerals Investigations, 1944 (Pages 191-210) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1946 CONTENTS Page Abstract................................................... 191 Introduction............................................... 192 History and production..................................... 192 Geology.................................................... 194 Franciscan formation................................... 194 Knoxville formation.................................... 195 Argillite and metavolcanic rocks................... 195 Shale and sandstone................................ 195 Peridotite and serpentine.............................. 195 Saxonite........................................... 196 Dunite............................................. 196 Wehrlite........................................... 196 Serpentine......................................... 196 Dike rocks............................................. 197 Alteration............................................. 197 Structure.............................................. 198 Ore bodies................................................. 199 Mineralogy............................................. 199 Character of ore....................................... 200 Localization........................................... 202 Origin................................................ -
New Mineral Names
-------- American Mineralogist, Volume 81, pages 1282-1286, 1996 NEW MINERAL NAMES. JOHN L. JAMBOR,l VLADIMIR A. KOVALENKER,2 JACEK PuZIEWICZ,3 ANDANDREW C. ROBERTS4 lDepartment of Earth Sciences, University of Waterloo, Waterloo, Ontario N2L 3Gl, Canada 21GREM RAN, Russian Academy of Sciences, Moscow 10917, Staromonetnii 35, Russia 'Institute of Geological Sciences, University of Wroc1aw, Cybulskiego 30, 50-205 Wroc1aw, Poland 4Geological Survey of Canada, 601 Booth Street, Ottawa KIA OE8, Canada Clinoatacamite* mineral from the Clear Creek claim, San Benito Coun- ty, California: Description and crystal structure. Pow- J.L. Jambor, J.E. Dutrizac, AC. Roberts, J.D. Grice, J.T. Szymanski (1996) Clinoatacamite, a new polymorph of der Diffraction, 11(1), 45-50. Cu2(OH)3C1,and its relationship to paratacamite and The mineral occurs sparingly with calomel, native mer- "anarakite." Can. Mineral., 34, 61-72. cury, cinnabar, montroydite, and quartz in a single spec- J.D. Grice, J.T. Szymanski, J.L. Jambor (1996) The crys- imen of float near a prospect pit at the former Clear Creek tal structure of clinoatacamite, a new polymorph of mercury mine in the new Idria district of California. The Cu2(OH)3Cl. Can. Mineral., 34, 73-78. specimen contains subhedral to anhedral crystals, typi- Electron microprobe analysis gave CuO 74.7 (73.4- cally bladed to platy, maximum size 0.3 x 0.3 mm, stri- 76.0), C1l6.5 (15.7-17.2), H20 (calc.) 13.5, sum 104.7, ated [001], black to dark brown-black color, dark red- less 0 == Cl 3.7, total 101.0 wt%, corresponding to brown to black streak, opaque to translucent on thin CU1.9603.o3H3.l1Clo.97, ideally Cu2(OH)3C1. -
Bromide from Terlingua, Texas
Canadian Mineralogist Vol. 19, pp. 393-396 (1981) COMANCHEITE,A NEW MEBGURYOXVCHLORIDE - BROMIDE FROMTERLINGUA, TEXAS A.C. ROBERTS eNn H.G. ANSELL Geologicalsurvey of Canada,60l Booth street, ottawa, ontario KlA 088 P.J. DUNN Depdrtmentol Mineral Sciences,Sntithsonian Instittttion, Washington, D.C. 20560, US'A' ABSTRACT en lumibre ultraviolette.Extinction paralldle.allon- gementpositif. Les indicesde r6fraction se situent '1..79. Comancheite is a new mercurv oxychloride- entre 1.78 et Densit6 mesur6e7.7G). cal- bromide mineral from the Mariposa mine. Terlingua cul6e 8.0. A la microsonde6lectronique' on trouve district, Texas. Associated minerals are calcite, la formule Hg,r(Clr.o,Brs.on)t".nrOo.n".d'oi la for- goethite, hematite and quartz. Comancheite occurs mule id6alisdeHgrs(Cl,Br)nOo. La comanch€iteest as anhedral crystalline massesand as stellate groups orthorhombique.groupe spatialPnnm ou Pnn2. a of acicilar crystals, elongate parallel to c. a\reraging 18.4t(l), b 21.64(l),c 6.677(21A', z = 4' Les 80 um lons and 3 to 4 um wide. Masses are red seot raies les plus intensesdu clich6 de poudre (d with an orange-yellow streak and have a resinous (A), / sur 6chellede l0) sont: 5.68(7).5.42(6), lustre; crystals are orange-red to vellow. vitreous 2.878(8). 2.71I(il, 2.669(10). 2.4s7(5\ et and nanslucent to transparent. Comancheite is 1.415(5). brittle with fair cleavase parallel to {001} and (Traduit Par la R6daction) not {ll0}, has a Mohs hardness of 2 and does de lieht. Opticallv. coman- Mots-clds: comanch6ite,oxychlorure-bromure fluoiesce in ultraviolet mine Mari- exhibits parallel extinction and is length- mercure. -
Fe2tio5) Based Thick films
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Serbian Academy of Science and Arts Digital Archive (DAIS) Accepted Manuscript Title: Humidity sensing properties of nanocrystalline pseudobrookite (Fe2TiO5) based thick films Authors: Maria Vesna Nikolic, Zorka Z. Vasiljevic, Miloljub D. Lukovic, Vera P. Pavlovic, Jelena Vujancevic, Milan Radovanovic, Jugoslav B. Krstic, Branislav Vlahovic, Vladimir B. Pavlovic PII: S0925-4005(18)31683-6 DOI: https://doi.org/10.1016/j.snb.2018.09.063 Reference: SNB 25369 To appear in: Sensors and Actuators B Received date: 15-5-2018 Revised date: 23-8-2018 Accepted date: 15-9-2018 Please cite this article as: Nikolic MV, Vasiljevic ZZ, Lukovic MD, Pavlovic VP, Vujancevic J, Radovanovic M, Krstic JB, Vlahovic B, Pavlovic VB, Humidity sensing properties of nanocrystalline pseudobrookite (Fe2TiO5) based thick films, Sensors and Actuators: B. Chemical (2018), https://doi.org/10.1016/j.snb.2018.09.063 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Humidity sensing properties of nanocrystalline pseudobrookite (Fe2TiO5) based thick films Maria Vesna Nikolic1*, Zorka Z. Vasiljevic2, Miloljub D. Lukovic1, Vera P. Pavlovic3, Jelena Vujancevic2, Milan Radovanovic4, Jugoslav B. Krstic5, Branislav Vlahovic6, Vladimir B. -
SGG Corundum Treatment.Pptx
The beauty of colour © Swiss Gemmological Institute SSEF SGG Zentralkurs, Thun, 15. April 2013 Treatment of corundum characteristics, detection and declaration Michael S. Krzemnicki Swiss Gemmological Institute SSEF Switzerland Photos and figures © H.A. Hänni & M.S. Krzemnicki 1! Consumer+expectation+ Quality& Every&gemstone&deposit&produces&stones&of&high&and&low&quality.& Usually&the&quality&distribution&has&the&shape&of&a&pyramid.&& Top&stones&are&rare,&stones&of&lower&quality&are&very&abundant.& The&exploitation&of&gems&is&expensive,®ardless&of&their&quality.& It&is&economically&and&important&to&be&able&to&enhance&stones&of&& the&lower&part&of&the&quality&pyramid&(also&for&the&miners!)& Once&a&treatment&is&developed&and&successfull,&it&often&is&also&applied&& on&stones&of&better&quality&to&make&them&even&better&looking.& Gem$deposit+production+ Quantity& © SSEF Swiss Gemmological Institute Treatment options for corundum... To&modify&transparency:&& &F&Gilling&of&Gissures&with&colourless&substance&&(oil,&artiGicial&resin,&glass)& &F&heating&to&dissolve&inclusions& & To&modify&colour& &F&Gilling&of&Gissures&with&coloured&substance&(oil,&artiGicial&resin,&glass)& &F&heating&in&oxidising&or&reducing&conditions&(±&with&additives)& &F&diffusion&of&„colouring“&elements&into&the&corundum&lattice& &F&irradiation& & To&enhance&stability& &F&Gilling&of&Gissures/cavities&with&solidifyig&substances&& & To&create&optical&effects&& &F&heating&with&additives& & © SSEF Swiss Gemmological Institute! 2! Treatment options for corundum... Fissure&Gilling&and&dyeing& & Foiling,&Painting& Heating&with&blowFpipe& ©&F.&Notari& Heating&with&electrical&furnace& ©&H.A.&Hänni& Irradiation& Heating&combined&with&surface&diffusion& Heating&with&borax&to&induce&Gissure&„healing“& Beryllium&diffusion& LeadFglass&Gissure&Gilling& & CobaltFglass&Gissure&Gilling& & next&treatment&??& & future& 0& 1000& 1900& 2000& Time+scale+ & © SSEF Swiss Gemmological Institute! Treatment options for corundum.. -
Chromite Crystal Structure and Chemistry Applied As an Exploration Tool
Western University Scholarship@Western Electronic Thesis and Dissertation Repository February 2015 Chromite Crystal Structure and Chemistry applied as an Exploration Tool Patrick H.M. Shepherd The University of Western Ontario Supervisor Dr. Roberta L. Flemming The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Patrick H.M. Shepherd 2015 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Shepherd, Patrick H.M., "Chromite Crystal Structure and Chemistry applied as an Exploration Tool" (2015). Electronic Thesis and Dissertation Repository. 2685. https://ir.lib.uwo.ca/etd/2685 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Western University Scholarship@Western University of Western Ontario - Electronic Thesis and Dissertation Repository Chromite Crystal Structure and Chemistry Applied as an Exploration Tool Patrick H.M. Shepherd Supervisor Roberta Flemming The University of Western Ontario Follow this and additional works at: http://ir.lib.uwo.ca/etd Part of the Geology Commons This Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in University of Western Ontario - Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Chromite Crystal Structure and Chemistry Applied as an Exploration Tool (Thesis format: Integrated Article) by Patrick H.M. -
Mercury--Quicksilver
scueu« No. 12 Mineral Technology Series No 6 University of Arizona Bulletin Mercury---Quicksilver By P. E. JOSEPH SECOND ISSUE NOVEMBER, 1916. Entered as second class matter November 2:1, 191~, at the postoftice at Tucson, Arizona. under the Act ot August 24, 1912. Issued weekb". September to Ya)·. PUBLISHED BY THE University of Arizona Bureau of Mines CHARLES F. WILLIS, Director TUCSON, ARIZONA 1916-17 BIBLIOGRAPHY Bancroft, Howland. Notes on the occurrence of cinnabar in central western Arizona. U. S. G. S. Bull. 430, pp. 151-153, 1910. Becker, G. F. Geology of- the quicksilver deposits of the Pacific slope, with atlas. Mon. 13, p. 486, 1888. Only the atlas in stock. Quicksilver Ore Deposits; Mineral Resources U. S. for 1892, pp. 139-168, 1893. Christy, S. B. Quicksilver reduction at New Almaden, Cal. Min- eral Resources U. S. for 1883-1884, pp. 603-636, 1885. Hillebrand, W. F., and Schaller, W. T. Mercury miner-als from Terlingua, Tex. U. S. G. S. Bull. 405, pp. 174, 1909. McCaskey, H. D. Quicksilver in 1912; Mineral Resources U. S. for 1912, Pt. 1, pp. 931-948, 1913. Quicksilver in 1913-Production and Resources; Mineral Resources U. S. for 1913, Pt. 1, pp. 197-212, 1914. Melville, W. H., and Lindgren, Waldemar. Contributions to the mineralogy of the Pacific coast. U. S. G. S. Bull. 61, 30 pp., 1890. Parker, E. W. Quicksilver; Twenty-first Ann. Rept. U. S. G. S., Pt. 6, pp. 273-283, 1901. University of Arizona Bulletin BULLETIN No. 12 SECOND ISSUE, NOVEMBER, 1916 MERCURY-QUICKSILVER By P. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Descriptive Mineralogy
Descriptive Mineralogy Oxides and Hydroxides Classification of the Minerals • Non-Silicates • Silicates – Native Elements – Orthosilicates – Halides – Sorosilicates – Sulfides – Cyclosilicates – Oxides – Chain Silicates – Hydroxides – Layer Silicates – Carbonates – Tektosilicates – Sulfates – Phosphates Simple Oxides • Hemioxides • Sesquioxides – Cuprite (Cu O) 2 – Corundum (Al2O3) – Ice (H O) 2 – Hematite (Fe2O3) • Monoxides – Bixbyite (Mn2O3) – Periclase (MgO) • Dioxides – Wüstite (FeO) – Rutile (TiO2) – Manganosite (MnO) – Anatase (TiO2) – Lime (CaO) – Brookite (TiO2) – Zincite (ZnO) – Cassiterite(SnO2) – Bromellite (BeO) – Pyrolusite(MnO2) – Tenorite (CuO) Simple Oxides Hemi-Oxides (M2O) • Ice (H2O) Hexagonal • Cuprite (Cu2O) • Why not Na2O? – (Na radius too large) Cuprite Cu2O • Occurrence: Low Temp Hydrothermal (Supergene) • Use: Minor ore of Cu Ice H2O Crystal System Hexagonal Point Group 6/mmm Space Group P63/mmc Optical Uniaxial Color Colorless Luster Vitreous Hardness 1.5 Density 0.95 Ice H2O Ice H2O Ice H2O High Pressure Phase Diagram Monoxides (MO) • Rocksalt oxides – Periclase MgO - Wüstite FeO – Manganosite MnO – Lime CaO – Bunsenite NiO • Zincite oxides: – Zincite ZnO, – Bromellite BeO • Other monoxides: – TenoriteCuO, Montroydite HgO Rocksalt Oxides MgO-FeO-MnO-CaO Crystal System Cubic Point Group 4/m-32/m Space Group Fm3m Optical Isotropic Periclase - Wüstite MgO - FeO Lower mantle phase Mg2SiO4 = MgSiO3 + MgO Ringwoodite = Perovskite + periclase Periclase MgO Sesquioxides (M2O3) • Corundum Group – Corundum Al2O3 – Hematite -
Taylor Creek Tin Distrisl
tions such as Paramount Canyon, the veins TaylorCreek tin distrisl- may reach three to four centimeters in width and a few meters in height and length. A dis- seminated cassiterite halo has been noted stratigraphy,structure, around the veins in Squaw Creek. A recently discoveredrhyolite porphyry has andtiming of mineralizationintensely altered the surrounding country rock near NM-59 where the road crossesthe Conti- byTed L. Egglestonand David L Norman,New Mexico lnstitute of Miningand Technology, Socorro, NM nental Divide. This porphyry is locally quartz- sericite altered and contains as much as I go pyrite. Similar intrusives have been mapped Introduction The Taylor Creek tin district is located in by Woodard (1982) southeast of the Taylor Primary tin depositscommonly are found in the north-central Black Range some 80 km Creek region. granitic plutonic environments where the tin west of Truth or Consequences,New Mexico occurs as cassiterite in greisen veins and as (fig. l). Cassiteritenuggets were first found in Regional geology disseminations in altered granite (Taylor, placers (Fries, 1940a). in the district in 1909 The tin-bearing Taylor Creek Rhyolite is 1979).In southwest New Mexico, however, tin Shortly wood tin thereafter, cassiterite and located in the Mogollon-Datil volcanic field, a occurs as cassiterite in hematite-cassiterite were porphyritic found in vein depositsin rhy- mid-Tertiary volcanic field consisting of inter- veins which cut Tertiary rhyolite domes and placer (Hill, olite lavas as well as in deposits mediate to