B-2 a Preliminary Report on the Corundum Deposits of Georgia
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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. -
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.. -
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 .................................... -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Rubies and Sapphires from Snezhnoe, Tajikistan
FEATURE ARTICLES RUBIES AND SAPPHIRES FROM SNEZHNOE , T AJIKISTAN Elena S. Sorokina, Andrey K. Litvinenko, Wolfgang Hofmeister, Tobias Häger, Dorrit E. Jacob, and Zamoniddin Z. Nasriddinov Discovered during the late 1970s, the Snezhnoe ruby and sapphire deposit in Tajikistan was active until the collapse of the former Soviet Union in the early 1990s and the outbreak of regional conflicts. This marble-hosted occurrence has seen renewed interest, as it is a large and potentially productive deposit that has not been sufficiently studied. Testing of samples identified solid inclusions of margarite enriched with Na and Li (calcic ephesite or soda margarite). These are believed to be previously unreported for gem corundum. Allanite, muscovite, and fuchsite (chromium-bearing muscovite) were identified for the first time in ruby and sapphire from Snezhnoe. These and other inclusions such as zircon, rutile, K- feldspar, and Ca-Na-plagioclase could serve to distinguish them from stones mined elsewhere. Con - centrations of trace elements were typical for ruby and sapphire of the same formation type. The highest Cr concentrations were observed within the bright red marble-hosted rubies, and these values were very similar to those of the famous Burmese rubies from Mogok. orundum— -Al O —is a common, though net, scapolite, lazurite, and variscite (Litvinenko α 2 3 minor, component of many metamorphic and Barnov, 2010). The occurrence of ruby in the Crocks. Gem-quality varieties of ruby and sap - Pamirs was first suggested by the Soviet mineralo - phire occur in only a few primary metamorphic and magmatic rock types depleted in silica and enriched Figure 1. -
Contact Zone Mineralogy and Geochemistry of the Mt. Mica Pegmatite, Oxford County, Maine
University of New Orleans ScholarWorks@UNO University of New Orleans Theses and Dissertations Dissertations and Theses Spring 5-16-2014 Contact Zone Mineralogy and Geochemistry of the Mt. Mica Pegmatite, Oxford County, Maine Kimberly T. Clark University of New Orleans, [email protected] Follow this and additional works at: https://scholarworks.uno.edu/td Part of the Geochemistry Commons, and the Geology Commons Recommended Citation Clark, Kimberly T., "Contact Zone Mineralogy and Geochemistry of the Mt. Mica Pegmatite, Oxford County, Maine" (2014). University of New Orleans Theses and Dissertations. 1786. https://scholarworks.uno.edu/td/1786 This Thesis is protected by copyright and/or related rights. It has been brought to you by ScholarWorks@UNO with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights- holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Thesis has been accepted for inclusion in University of New Orleans Theses and Dissertations by an authorized administrator of ScholarWorks@UNO. For more information, please contact [email protected]. Contact Zone Mineralogy and Geochemistry of the Mt. Mica Pegmatite, Oxford County, Maine A Thesis Submitted to the Graduate Faculty of the University of New Orleans in partial fulfillment of the requirements for the degree of Master of Science In Earth and Environmental Science By Kimberly T. Clark B.S. -
An In-Vitro Evaluation of the Capacity of Local Tanzanian Crude Clay and Ash Based Materials in Binding Aflatoxins in Solution
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 2 November 2018 doi:10.20944/preprints201811.0021.v1 Peer-reviewed version available at Toxins 2018, 10, 510; doi:10.3390/toxins10120510 An in-vitro evaluation of the capacity of local Tanzanian crude clay and ash based materials in binding aflatoxins in solution 1,3Ayo E. M; 2G. H. Laswai; 1A. Matemu; 1M. E. Kimanya* 1 The Nelson Mandela African Institution of Science and Technology, P.O. Box 447, Arusha. Tanzania E-mails: [email protected]; [email protected]: kimanya.martin@nm-aist 2 Sokoine University of Agriculture, P.O. Box 3004, Morogoro. Tanzania, E-mail: [email protected] 3 Institute of Rural Development Planning, P.O. Box 138, Dodoma, Tanzania, E-mail: [email protected] *The corresponding author, email: kimanya.martin@nm-aist Corresponding author: Prof Martin E. Kimanya (Associate Professor of Food safety and Nutrition Sciences) P.O. Box 447, Arusha. Tanzania; e-mail: [email protected] Abstract Aflatoxins in feeds cause great health hazards to animals and in advance, to human. Potential of crude clays designated AC, KC, CC and MC and ashes VA and RA were evaluated for their capacity to adsorb aflatoxins B1 (AFB1), B2 (AFB2), G1 (AFG1) and G2 (AFG2) relative to a commercial binder MycobinderR (Evonik Industries AG) using in-vitro technique. On average, CC, VA, KC, MC, AC, RA and MycobindR adsorbed 39.9%, 51.3%, 61.5%, 62.0%, 72.6%, 84.7% and 98.1% of the total aflatoxins in buffered solution, respectively. -
Clay Minerals
American Minetralogist, Volume 65, pages 1-7, 1980 Summary of recommendations of AIPEA nomenclature committee on clay minerals S. W. BAILEY, CHAIRMAN1 Department of Geology and Geophysics University of Wisconsin-Madison Madi~on, Wisconsin 53706 Introduction This summary of the recommendations made to Because of their small particle sizes and v~riable date by the international nomenclature committees degrees of crystal perfection, it is not surprisi4g that has been prepared in order to achieve wider dissemi- clay minerals proved extremely difficult to character- nation of the decisions reached and to aid clay scien- ize adequately prior to the development of ~odem tists in the correct usage of clay nomenclature. Some analytical techniques. Problems in charactetization of the material in the present summary has been led quite naturally to problems in nomenclatute, un- taken from an earlier summary by Bailey et al. doubtedly more so than for the macroscopic~ more (1971a). crystalline minerals. The popular adoption ~ the early 1950s of the X-ray powder diffractometer for Classification . clay studies helped to solve some of the probl ms of Agreement was reached early in the international identification. Improvements in electron micro copy, discussions that a sound nomenclatur~ is necessarily electron diffraction and oblique texture electr ;n dif- based on a satisfactory classification scheme. For this fraction, infrared and DT A equipment, the de elop- reason, the earliest and most extensive efforts of the ment of nuclear and isotope technology, of high- several national nomenclature committees have been speed electronic computers, of Mossbauer spec rome- expended on classification schemes. Existing schemes ters, and most recently of the electron micr probe were collated and discussed (see Brown, 1955, Mac- and scanning electron microscope all have ai ed in kenzie, 1959, and Pedro, 1967, for examples), sym- the accumulation of factual information on clays. -
Chromite Deposits of North Carolina
CI 2 Nortfc C *°<™ Sftfe library ^/t°' C Raleigh NORTH CAROLINA DEPARTMENT OF CONSERVATION AND DEVELOPMENT R. BRUCE ETHERIDGE, DiRECTQR DIVISION OF MINERAL RESOURCES JASPER L. STUCKEY, STATE GEOLOGIST Bulletin No. 42 Chromite Deposits of North Carolina By Charles e. hunter, Thomas g. Murdock and Gerald r. Maccarthy Prifared and Published ih Cooperation with the Tennessee Valley Authority under the direction of Jasper L. Stuckey, North Carolina Department of Conservation and Development and H. S. Rankin, Tennessee Valley Authorjty • RALEIGH 1942 Digitized by the Internet Archive in 2013 i http://archive.org/details/chromitedeposits1942nort North Carolina State library Raleigh North Carolina Department of Conservation and Development R. Bruce Etheridge, Director (J, Division of Mineral Resources Jasper L. Stuckey, State Geologist Bulletin No. 42 Chromite Deposits of North Carolina Geology and Mining Charles E. Hunter and Thomas G. Murdock Geophysics Gerald R. MacCarthy Prepared and Published in Cooperation with the Tennessee Valley Authority Under the Direction of Jasper L. Stuckey, North Carolina Department of Conservation and Development and H. S. Rankin, Tennessee Valley Authority Raleigh 1942 i MEMBERS OF THE BOARD OF CONSERVATION AND DEVELOPMENT Governor J. Melville Broughton, Chairman Raleigh Santford Martin, Vice-Chairman Winston-Salem Harry Bailey Spruce Pine Oscar Breece Fayetteville J. Wilbur Bunn Raleigh Bruce Cameron . Wilmington K. Clyde Council Wananish W. J. Damtoft Asheville J. Horton Doughton . Statesville Irving F. Hall -
GEMSTONES with ALEXANDRITE EFFECT by E
GEMSTONES WITH ALEXANDRITE EFFECT By E. Gubelin and K. Schmetzer The term alexandrite effect refers to the he alexandrite effect was observed for the first time apparent change of color in certain T in 1830, in a chromium-bearing variety of chryso- minerals from blue-green or greenish beryl from the emerald mines on the eastern slopes of the violet in daylight to red or reddish violet Ural Mountains. The new gem was named by the Swed- in incandescent light. This effect was ish explorer Nils Nordenskiold in 1838 (Koksharov, 1861), discovered in chrome-bearing chrysoberyl in honor of then-Tsarevitch Alexander Nikolayevitch, from the Ural Mountains as early as the beginning of the 19th century. In more the future Tsar Alexander I1 (1818-1881). The alexandrite, recent time's, it has also been observed in famous for its conspicuous change of color-green in day- certain varieties of garnet, corundum, light and red in incandescent light-soon enjoyed great spinel, kyanite, fluorite, and monazite. It popularity as well. This gem was appreciated not only for has been determined that the absorption its curious color change, which has only very recently spectrum of all alexandrite-like minerals been explained (Carstens, 1973; Hassan et al., 1974; is characterized by transmission maxima Gubelin, 1976 a and b; and Schmetzer et al., 1980 a and in the blue-green and red regions and by b) but also because red and green were the colors of the a transmission minimum in the yellow tsarist army; thus the alexandrite was considered by many region. The color of minerals with two to be the national gem of tsarist Russia. -
Mineral Deposit Models for Northeast Asia
Mineral Deposit Models for Northeast Asia By Alexander A. Obolenskiy1, Sergei M. Rodionov2, Sodov Ariunbileg3, Gunchin Dejidmaa4, Elimir G. Distanov1, Dangindorjiin Dorjgotov5, Ochir Gerel6, Duk Hwan Hwang7, Fengyue Sun8, Ayurzana Gotovsuren9, Sergei N. Letunov10, Xujun Li8, Warren J Nokleberg11, Masatsugu Ogasawara12, Zhan V. Seminsky13, Akexander P. Smelov14, Vitaly I. Sotnikov1, Alexander A. Spiridonov10, Lydia V. Zorina10, and Hongquan Yan8 1 Russian Academy of Sciences, Novosibirsk 2 Russian Academy of Sciences, Khabarovsk 3 Mongolian Academy of Sciences, Ulaanbaatar 4 Mineral Resources Authority of Mongolia, Ulaanbaatar 5 Mongolian National University, Ulaanbaatar 6 Mongolian University of Science and Technology, Ulaanbaatar 7 Korea Institute of Geology, Mining, and Materials, Taejon 8 Jilin University, Changchun, China 9 Mongolia Ministry of Industry and Commerce, Ulaanbaatar 10 Russian Academy of Sciences, Irkutsk 11 U.S. Geological Survey, Menlo Park 12 Geological Survey of Japan/AIST, Tsukuba 13 Irkutsk State Technical University, Irkutsk 14 Russian Academy of Sciences, Yakutsk This article is prepared by a large group of Russian, Chinese, Mongolian, South Korean, Introduction and Companion Japanese, Studies and USA geologists who are members of the joint Metalliferous and selected non-metalliferous lode international project on Major Mineral Deposits, and placer deposits for Northeast Asia are classified Metallogenesis, and Tectonics of the Northeast Asia. into various models or types described below. The This project is being conducted by the Russian mineral deposit types used in this report are based on Academy of Sciences, the Mongolian Academy of both descriptive and genetic information that is Sciences, Mongolian National University, Mongolian systematically arranged to describe the essential Technical University, the Mineral Resources Authority properties of a class of mineral deposits. -
Progressive Low-Grade Metamorphism of a Black Shale Formation, Central Swiss Alps, with Special Reference to Pyrophyllite and Margarite Bearing Assemblages*
Progressive Low-Grade Metamorphism of a Black Shale Formation, Central Swiss Alps, with Special Reference to Pyrophyllite and Margarite Bearing Assemblages* ^MARTIN FREYf Mineralogisch-petrographisches Institut der Universitdt Bern, Sahlistrasse 6, CH-3012 Bern, Switzerland (Received 23 July 1976, in revised form 21 February 1977) ABSTRACT The unmetamorphosed equivalents of the regionally metamorphosed clays and marls that make up the Alpine Liassic black shale formation consist of illite, irregular mixed-layer illite/montmoril- lonite, chlorite, kaolinite, quartz, calcite, and dolomite, with accessory feldspars and organic material. At higher grade, in the anchizonal slates, pyrophyllite is present and is thought to have formed at the expense of kaolinite; paragonite and a mixed-layer paragonite/muscovite presumably formed from the mixed-layer illite/montmorillonite. Anchimetamorphic illite is poorer in Fe and Mg than at the diagenetic stage, having lost these elements during the formation of chlorite. Detrital feldspar has disappeared. In epimetamorphic phyllites, chloritoid and margarite appear by the reactions pyrophyllite + chlorite = chloritoid + quartz + H2O and pyrophyllite + calcite ± paragonite = margarite + quartz + H2O + CO2, respectively. At the epi—mesozone transition, paragonite and chloritoid seem to become incompatible in the presence of carbonates and yield the following breakdown products: plagioclase, margarite, clinozoisite (and minor zoisite), and biotite. The maximum distribution of margarite is at the epizone-mesozone boundary; at higher metamorphic grade margarite is consumed by a continuous reaction producing plagioclase. Most of the observed assemblages in the anchi- and epizone can be treated in the two subsystems MgO (or FeO)-Na2O-CaO-Al2O3-<KAl3O5-Si02-H2O-CO2). Chemographic analyses show that the variance of assemblages decreases with increasing metamorphic grade.