Turquoise in New Mexico
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Beneficiation of High Phosphorus Limonite Ore by Sodium- Carbonate-Added Carbothermic Reduction
ISIJ International, Vol. 52 (2012), No. 10, pp. 1757–1763 Beneficiation of High Phosphorus Limonite Ore by Sodium- carbonate-added Carbothermic Reduction Shaojun BAI,1) Shuming WEN,1,2)* Dianwen LIU,1) Wenbin ZHANG1) and Qinbo CAO1) 1) Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming, Yunnan, 650093 PR China. E-mail: [email protected], [email protected], [email protected], [email protected] 2) Engineering Research Center and Ministry of Education for Efficient Utilization of Mineral Resources in Western of China, Kunming 650093, PR China. (Received on March 1, 2012; accepted on June 6, 2012) The characteristics of Huimin high phosphorus limonite ore and the beneficiation of this iron ore by sodium-carbonate-added carbothermic reduction, ultrafine grinding and magnetic separation were investi- gated. Iron particle size in reduced ore without Na2CO3 additive is tiny and the fayalite is abundant. It is indicated that the formation of fayalite is the main hindrance to accelerate the reduction of limonite. With a mass ratio of Na2O3 to ore of 10% additive, the reduction of limonite can be reinforced. The reinforcing affect may be caused by the increase of the reducing reaction activity of FeO and the acceleration of the carbon gasification reaction rate. Fluorapatite were not reduced in the low temperature reduction process and entered to gangue phases, after ultrafine grinding-magnetic separation process, a qualified iron con- centrate with 76.47% Fe, a recovery of 73.20% is obtained with simultaneous decrease in the phosphorus content down to 0.25%. KEY WORDS: iron ore; beneficiation; high phosphorus limonite ore; sodium carbonate; carbothermic reduc- tion; metallic iron; ultrafine grinding. -
Get Reactive in System 96!
Get Reactive in System 96! Uroboros has created two unique glass formulas for System 96 that are designed to create an interface color, or a reac on, when melted against certain other colors. This occurs when ions from the two adjacent glasses migrate and mingle when the gl asses become hot and ß uid. Given the right glass chemistry, the comingled ions form a very thin colored line, or reac on. Since our formulas react to create a no ceably reddish hue we named them Red Reac ves: as in Red Reac ve Transparent, and Red Reac ve Opal. The primary ingredient needed in a glass to generate a reac on color with our Reac ve glass is Copper. Copper is present in many blue and blue-green glass colors, but in some cases in too low a concentra on to create a no ceable reac on. For simplicity, all System 96 colors have been graded for their poten al to react into three categories: Strong, Medium, and Mild. See them all listed in the chart on the back of this page. You will Þ nd that the intensity of the reac on color will get stronger with longer, ho er, or repeat Þ rings. This is because the copper ions have more me to mingle with their friendly reac ve partners in the adjacent glass. The chart rankings are based on a typical single Þ ring cycle. You could get a Medium reac on from a color graded as Mild by Þ ring it ho er, or Þ ring mul ple mes. -
RAL COLOR CHART ***** This Chart Is to Be Used As a Guide Only. Colors May Appear Slightly Different ***** Green Beige Purple V
RAL COLOR CHART ***** This Chart is to be used as a guide only. Colors May Appear Slightly Different ***** RAL 1000 Green Beige RAL 4007 Purple Violet RAL 7008 Khaki Grey RAL 4008 RAL 7009 RAL 1001 Beige Signal Violet Green Grey Tarpaulin RAL 1002 Sand Yellow RAL 4009 Pastel Violet RAL 7010 Grey RAL 1003 Signal Yellow RAL 5000 Violet Blue RAL 7011 Iron Grey RAL 1004 Golden Yellow RAL 5001 Green Blue RAL 7012 Basalt Grey Ultramarine RAL 1005 Honey Yellow RAL 5002 RAL 7013 Brown Grey Blue RAL 1006 Maize Yellow RAL 5003 Saphire Blue RAL 7015 Slate Grey Anthracite RAL 1007 Chrome Yellow RAL 5004 Black Blue RAL 7016 Grey RAL 1011 Brown Beige RAL 5005 Signal Blue RAL 7021 Black Grey RAL 1012 Lemon Yellow RAL 5007 Brillant Blue RAL 7022 Umbra Grey Concrete RAL 1013 Oyster White RAL 5008 Grey Blue RAL 7023 Grey Graphite RAL 1014 Ivory RAL 5009 Azure Blue RAL 7024 Grey Granite RAL 1015 Light Ivory RAL 5010 Gentian Blue RAL 7026 Grey RAL 1016 Sulfer Yellow RAL 5011 Steel Blue RAL 7030 Stone Grey RAL 1017 Saffron Yellow RAL 5012 Light Blue RAL 7031 Blue Grey RAL 1018 Zinc Yellow RAL 5013 Cobolt Blue RAL 7032 Pebble Grey Cement RAL 1019 Grey Beige RAL 5014 Pigieon Blue RAL 7033 Grey RAL 1020 Olive Yellow RAL 5015 Sky Blue RAL 7034 Yellow Grey RAL 1021 Rape Yellow RAL 5017 Traffic Blue RAL 7035 Light Grey Platinum RAL 1023 Traffic Yellow RAL 5018 Turquiose Blue RAL 7036 Grey RAL 1024 Ochre Yellow RAL 5019 Capri Blue RAL 7037 Dusty Grey RAL 1027 Curry RAL 5020 Ocean Blue RAL 7038 Agate Grey RAL 1028 Melon Yellow RAL 5021 Water Blue RAL 7039 Quartz Grey -
Close-Out List February 2014 Quantities Are Limited
Close-Out List February 2014 Quantities are limited. All freight charges are to be paid by purchaser. ALL SHIPMENTS ARE TO BE PAID C.O.D. or Credit Card New Additions for 2014! PM Coat Trouser MFR# Description Color Lapel # Price Price 915 4831 Jean Yves White Parisian Stripe Two Button Notch White Notch 913 4829 Jean Yves Chocolate Parisian Stripe Two Button Notch Chocolate Notch 905 7322C Joseph Abboud Black Chalk Pin Stripe Two Button Notch Black Notch 904 7340C Joseph Abboud Black Two Button Notch Black Notch 521 100TCNA Raffinati White Bari Notch Full Dress White Notch Plain Black Fabric Coats 835 41910 Perry Ellis Evening Black Astaire Three Button Cardigan Black None 531 T565 Imp Black Eton Gaberdine (Coat & Pant Set) Black None 899 722RAZ32 After Six Black Razor Stand-Up Collar (32”) Black Fashion 851 8642C FCGI Black Matisse Diagonal Three Button Mandarin Overlap (33”) Black Fashion 849 A7800 Andrew Fezza Black Jupiter Ten Button Mandarin (38”) Black Fashion 904 7340C Joseph Abboud Black Two Button Notch Black Notch 862 88802 Ecko II Black Dream Lay Down Collar (32”) Black Notch 818 81116 Claiborne Black Sparkle Citi-Nites Three Button Notch Black Notch 817 81117 Claiborne Black Vertigo Four Button Notch w/Fly Front Black Notch 807 7102C Calvin Klein Black Three Button Notch Black Notch 799 311121 Chaps Ralph Lauren Black Barrington Four Button Notch Black Notch 789 F7852 Andrew Fezza Captain in Black Three Button Notch Black Notch 747 81112 Claiborne for Men Black Five Button Notch Long Coat Black Notch 525 9650C FCGI Black -
A Survey of the Gemstone Resources of China
A SURVEY OF THE GEMSTONE RESOURCES OF CHINA By Peter C. Keller and Wang Fuquan The People's Republic of China has recently hina has historically been a land of great mystery, placed a high priority on identifying and C with natural resources and cultural treasures that, developing its gemstone resources. Initial until recently, were almost entirely hidden from the out- exploration by teams of geologists side world. From the point of view of the geologist and throughout China has identified many gemologist, one could only look at known geological maps deposits with significant potential, of this huge country and speculate on the potential impact including amher, cinnabar, garnets, blue sapphires, and diamonds. Small amounts of China would have on the world's gem markets if its gem ruby have' qlso been found. Major deposits resources were ever developed to their full potential. of nephriteyade as well as large numbers of During the past few years, the government of the Peo- gem-bearing pegmatite dilces have been ple's Republic of China (P.R.C.)has opened its doors to the identified.Significant deposits of peridot outside world in a quest for information and a desire for are crirrently being exploited from Hebei scientific and cultural cooperation. It was in this spirit of Province. Lastly, turqrloise rivaling the cooperation that a week-long series of lectures on gem- finest Persian material has been found in stones and their origins was presented by the senior author large quantities in Hubei and Shaanxi and a colleague to over 100 geologists from all over China Provinces. -
Turquoise: the Cerrillos Mineral Gem
A Living History Museum Turquoise: The Cerrillos Mineral Gem The mines of Cerrillos, New Mexico produce a particularly beautiful blue/ green variety of turquoise, so stunning in fact that they have been mined for roughly the last 3,000 years! Chemically, it is a phosphate of aluminum carrying small quantities of copper and iron and a green mineral, variscite. These give the gemstone its color as well as its value and beauty. This is the only phosphate that is considered a precious stone. Ancestral Puebloans first started mining the Cerrillos hills circa 900 BCE, and it’s been mined ever since. This “gem” of a mineral has been found across the state, and archaeological evidence shows it’s been mined and fashioned into ornaments and jewelry for centuries, with remnants found at one of the most ancient sites in the state, Chetro Ketl at Chaco Canyon. Southwest indigenous groups call turquoise chalchihuitl, as did the ancient peoples of Mexico and Central America who used the same word to describe jade or green turquoise. One of the hills still being mined in Cerrillos still bears the name, Mount Chalchihuitl. Combined with shell and coral from the California coast acquired in trade, turquoise jewelry itself became a valued commodity. Spanish settlers didn’t have much interest in turquoise as they were looking for what they considered a more important prize, namely gold and silver. In fact, outside of local indigenous groups, other cultural groups weren’t much interested in it and it didn’t really gain popularity with the American cultural at large until the 1890s. -
Powder Denim Sky Teal Midnight Cerulean Navy Turquoise Cornflower Periwinkle Royal Opal Cmg 08458 Cmg 1 26 27 3 4 6 29 30 31 2 32 33
MARCH 2010 House Beautiful sp ring ALL COLO | A BOUT issue BLUE POWDER DENIM SKY TEAL MIDNIGHT CERULEAN NAVY TURQUOISE CORNFLOWER PERIWINKLE ROYAL OPAL CMG 08458 1 26 27 3 4 6 29 30 31 2 32 33 5 28 34 7 8 36 10 11 9 50 BLUE FABRICS 35 14 12 13 15 37 38 41 40 19 39 47 17 43 44 45 18 46 16 20 42 23 24 25 49 21 48 22 50 1 CLOQUE DE COTON 6 ARIPEKA 10 STRIATE IN AQUA. KaTE 14 CHRISSY IN DENIM. ViCTOria 18 FORMIA 22 DJEBEL 26 GASTAAD PLAID IN CaPri. 31 LA GAROUPE 35 LUCE 39 JUPON BOUQUET 43 OcELOT IN AZUL. KaT BURKI 47 KHAN CASHMERE IN COLOR 8. DOMINIQUE KIEffER IN HYdraNGEA. ROGERS GabriEL THROUGH STUdiO HaGAN HOME COLLECTION: IN RUSCELLO. DECORTEX IN GaLET. LELIEVRE THROUGH EriC COHLER FOR LEE JOfa: IN INdiGO. RALPH LaUREN IN NaVY. MadELINE WEINrib IN AZURE BLUE COLLECTION FOR IN BLUE MIX. HOLLAND BY RUBELLI THROUGH & GOffiGON: 203-532-8068. FOUR NYC: 212-475-4414. 212-888-3241. THROUGH BRUNSCHWIG STarK fabriC: 212-355-7186. 800-453-3563. HOME : 888-743-7470. ATELIER: 212-473-3000, X780. AND WarM WHITE. FORTUNY: STarK fabriC: 212-355-7186. & SHErrY: 212-355-6241. BERGAMO: 914-665-0800. & FILS: 914-684-5800. 212-753-7153. 7 MYRSINI 11 SIERRA MADRE 15 TANZANIA IN BLUE. CHarLES 23 CHEVRON BAR 27 VIOLETTA N IN MOONLIGHT. 32 WOOL SATEEN 36 AlTAI IN BLUETTE. 44 HINSON SUEDE 48 BARODA II IN INdiGO ON 2 FIORI IN ATLANTIC ON SEA MIST. -
Eg9601814 Supergene Alteration of Magnetite And
EG9601814 SUPERGENE ALTERATION OF MAGNETITE AND PYRITE AND THE ROLE OF THEIR ALTERATION PRODUCTS IN THE FIXATION OF URANIUM FROM THE CIRCULATING MEDIA. BY MA EL GEMMIZI Nuclear Materials A uthority Cairo- Egypt. ABSTRACT. In most of the Egyptian altered radioactive granites, highly magnetic heavy particles were found to be radioactive. They are a mixture of several iron oxide minerals which are products of supergene alteration of the pre-existing hypogene iron-bearing minerals especially magnetite and pyrite. The end products of this supergene alteration are mainly hydrated iron oxide minerals limonite hematite and geothite. During the alteration, deformation and defects in the minerals structure took place , thereby promoting diffusion of the substitutional and interstitial ions (uranium) to words these sites The mechanism of the alteration of the hypogene iron-bearing minerals; magnetite and pyrite to form the secondary minerals hematite, limonite and geothite; the role of these minerals in fixing uranium from the ciculating media as well as the applicability of these minerals as indicators to the radioactivity of the host rocks were discussed. INTRODUCTION It is quite common that in all the altered rocks magnetite and to some extent pyrite which are present as accessories are suffering from some degrees of alteration. Magnetite and pyrite in the altered granite of Wadi Nugrus, El Missikat and £1 Aradyia, Eastern Desert was found by (1 & 2) to possess several degrees of alteration and crystal deformation. This means that both minerals are sensitive to postdepositional environmental changes. The granites of the present study were described as altered granites overlained by metasediments and underlained by magmatic bodies which invaded the granites itself by sills. -
Color Matters
Color Matters Color plays a vitally important role in the world in which we live. Color can sway thinking, change actions, and cause reactions. It can irritate or soothe your eyes, raise your blood pressure or suppress your appetite. When used in the right ways, color can even save on energy consumption. As a powerful form of communication, color is irreplaceable. Red means "stop" and green means "go." Traffic lights send this universal message. Likewise, the colors used for a product, web site, business card, or logo cause powerful reactions. Color Matters! Basic Color Theory Color theory encompasses a multitude of definitions, concepts and design applications. There are enough to fill several encyclopedias. However, there are basic categories of color theory. They are the color wheel and the color harmony. Color theories create a logical structure for color. For example, if we have an assortment of fruits and vegetables, we can organize them by color and place them on a circle that shows the colors in relation to each other. The Color Wheel A color wheel is traditional in the field of art. Sir Isaac Newton developed the first color wheel in 1666. Since then, scientists and artists have studied a number of variations of this concept. Different opinions of one format of color wheel over another sparks debate. In reality, any color wheel which is logically arranged has merit. 1 The definitions of colors are based on the color wheel. There are primary colors, secondary colors, and tertiary colors. Primary Colors: Red, yellow and blue o In traditional color theory, primary colors are the 3 colors that cannot be mixed or formed by any combination of other colors. -
Raymond & Leigh Danielle Austin
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The Brown Iron Ores of West- Middle Tennessee
ORTONMFMORIAI LIBRARY Please do not destroy or throw away this publication. If you have no further use for it, write to the Geological Survey at Washington and ask for a frank to return It DEPARTMENT OF THE INTERIOR Hubert Work, Secretary U. S. GEOLOGICAL SURVEY George Otis Smith, Director Bulletin 795 D THE BROWN IRON ORES OF WEST- MIDDLE TENNESSEE BY ERNEST F. BURCHARD Prepared in cooperation with the Tennessee Geological Surrey Contributions to economic geology, 1927, Part I (Pages 63-112) Published October 20,1927 UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON 1927 ADDITIONAL COPIES OF THIS PUBLICATION MAT BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 15 CENTS PEE COPY CONTENTS Page Introduction 53 Earlier geologic work _ _ _______ 55 The early iron industry 57 Geography _ 58 Geology. _ - 60 Stratigraphy - 60 Structure_ _ _ ._ 64 The iron ores _ . __ _ _ 65 Distribution ______________________________ 65 Occurrence and character- ____________:______ 66 Position and form of deposits____________________ 66 Types of ore 66 Mineral composition.. __ ____ ______________ ' 67 Chemical composition___________________,__ __ 69 Topographic relations _ _ _ _ 71 Geologic relations _' ____ 72 Suggestions as to origin ______ _______________ 74 Typical deposits _ ____ __ 77 Stewart County : _ 77 Deposits near Bear Spring _________________ 78 Deposits near Stribling _ _ __________ 80 Montgomery County __ _ ______________ 84 Deposits near Louise _ _ _ __ 84 Dickson County ___________________________ -
Geology and Mineralogy of the Ape.X Washington County, Utah
Geology and Mineralogy of the Ape.x Germanium-Gallium Mine, Washington County, Utah Geology and Mineralogy of the Apex Germanium-Gallium Mine, Washington County, Utah By LAWRENCE R. BERNSTEIN U.S. GEOLOGICAL SURVEY BULLETIN 1577 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1986 For sale by the Distribution Branch, Text Products Section U.S. Geological Survey 604 South Pickett St. Alexandria, VA 22304 Library of Congress Cataloging-in-Publication Data Bernstein, Lawrence R. Geology and mineralogy of the Apex Germanium Gallium mine, Washington County, Utah (U.S. Geological Survey Bulletin 1577) Bibliography: p. 9 Supt. of Docs. no.: I 19.3:1577 1. Mines and mineral resources-Utah-Washington County. 2. Mineralogy-Utah-Washington County. 3. Geology-Utah-Wasington County. I. Title. II. Series: United States. Geological Survey. Bulletin 1577. QE75.B9 no. 1577 557.3 s 85-600355 [TN24. U8] [553' .09792'48] CONTENTS Abstract 1 Introduction 1 Germanium and gallium 1 Apex Mine 1 Acknowledgments 3 Methods 3 Geologic setting 3 Regional geology 3 Local geology 3 Ore geology 4 Mineralogy 5 Primary ore 5 Supergene ore 5 Discussion and conclusions 7 Primary ore deposition 7. Supergene alteration 8 Implications 8 References 8 FIGURES 1. Map showing location of Apex Mine and generalized geology of surrounding region 2 2. Photograph showing main adit of Apex Mine and gently dipping beds of the Callville Limestone 3 3. Geologic map showing locations of Apex and Paymaster mines and Apex fault zone 4 4. Scanning electron photomicrograph showing plumbian jarosite crystals from the 1,601-m level, Apex Mine 6 TABLES 1.