Barite Deposits of Virginia by R.AYMOND S
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Podiform Chromite Deposits—Database and Grade and Tonnage Models
Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S. -
A Review of Flotation Separation of Mg Carbonates (Dolomite and Magnesite)
minerals Review A Review of Flotation Separation of Mg Carbonates (Dolomite and Magnesite) Darius G. Wonyen 1,†, Varney Kromah 1,†, Borbor Gibson 1,† ID , Solomon Nah 1,† and Saeed Chehreh Chelgani 1,2,* ID 1 Department of Geology and Mining Engineering, Faculty of Engineering, University of Liberia, P.O. Box 9020 Monrovia, Liberia; [email protected] (D.G.W.); [email protected] (Y.K.); [email protected] (B.G.); [email protected] (S.N.) 2 Department of Electrical Engineering and Computer Science, University of Michigan, Ann Arbor, MI 48109, USA * Correspondence: [email protected]; Tel.: +1-41-6830-9356 † These authors contributed equally to the study. Received: 24 July 2018; Accepted: 13 August 2018; Published: 15 August 2018 Abstract: It is well documented that flotation has high economic viability for the beneficiation of valuable minerals when their main ore bodies contain magnesium (Mg) carbonates such as dolomite and magnesite. Flotation separation of Mg carbonates from their associated valuable minerals (AVMs) presents several challenges, and Mg carbonates have high levels of adverse effects on separation efficiency. These complexities can be attributed to various reasons: Mg carbonates are naturally hydrophilic, soluble, and exhibit similar surface characteristics as their AVMs. This study presents a compilation of various parameters, including zeta potential, pH, particle size, reagents (collectors, depressant, and modifiers), and bio-flotation, which were examined in several investigations into separating Mg carbonates from their AVMs by froth flotation. Keywords: dolomite; magnesite; flotation; bio-flotation 1. Introduction Magnesium (Mg) carbonates (salt-type minerals) are typical gangue phases associated with several valuable minerals, and have complicated processing [1,2]. -
HIGHLIGHTS of THIS ISSUE This Listing Does Not Affect the Legal Status of Any Document Published in This Issue
WEDNESDAY, OCTOBER 27, 1971 WASHINGTON, D.C. Volume 36 ■ Number 207 Pages 20569-20640 HIGHLIGHTS OF THIS ISSUE This listing does not affect the legal status of any document published in this issue. Detailed table of contents appears inside. PEANUTS— USDA regulation proclaiming 1972 marketing quotas and acreage allotments; effec tive 10-26-71 __________ ____ _____ - 20575 COTTON LOAN PROGRAM— USDA regulations on redemptions; effective 10-26-71-------------- 20577 BURLEY TOBACCO— USDA regulation on grade rates for advances to producers on 1971 crop; effective 10-26-71................ .........— .............. 20577 AIR CARRIERS— CAB regulation on use of rec ords on microfilm and microfiche; effective 10-27-71 ................. ......... ...................... 20579 CONTRACT APPEALS— NASA regulations; effec tive 11-15-71_________ _______________________ ___ 20580 UNFAIR TRADE PRACTICES— FTC cease and desist orders on false advertising (17 docu ments) ........................... ..............................20584-20596 ANTIBIOTIC DRUGS— FDA regulation revoking certification of 8 drugs; effective within 40 days unless stayed by objections____________ _____ ____ 20597 INCOME TAX— 1RS regulations relating to examinations of incomes of churches........... ......... 20599 AVAILABILITY OF RECORDS— EEOC rule setting schedule of fees; effective 10-27-71...... ............ 20600 COAL MINE HEALTH AND SAFETY— Interior Dept, regulations for transfer of miners with evidence of pneumoconiosis.................... 20600 Interior Dept, proposal of standards -
Gamblin Provides Is the Desire to Help Painters Choose the Materials That Best Support Their Own Artistic Intentions
AUGUST 2008 Mineral and Modern Pigments: Painters' Access to Color At the heart of all of the technical information that Gamblin provides is the desire to help painters choose the materials that best support their own artistic intentions. After all, when a painting is complete, all of the intention, thought, and feeling that went into creating the work exist solely in the materials. This issue of Studio Notes looks at Gamblin's organization of their color palette and the division of mineral and modern colors. This visual division of mineral and modern colors is unique in the art material industry, and it gives painters an insight into the makeup of pigments from which these colors are derived, as well as some practical information to help painters create their own personal color palettes. So, without further ado, let's take a look at the Gamblin Artists Grade Color Chart: The Mineral side of the color chart includes those colors made from inorganic pigments from earth and metals. These include earth colors such as Burnt Sienna and Yellow Ochre, as well as those metal-based colors such as Cadmium Yellows and Reds and Cobalt Blue, Green, and Violet. The Modern side of the color chart is comprised of colors made from modern "organic" pigments, which have a molecular structure based on carbon. These include the "tongue- twisting" color names like Quinacridone, Phthalocyanine, and Dioxazine. These two groups of colors have unique mixing characteristics, so this organization helps painters choose an appropriate palette for their artistic intentions. Eras of Pigment History This organization of the Gamblin chart can be broken down a bit further by giving it some historical perspective based on the three main eras of pigment history – Classical, Impressionist, and Modern. -
Barite (Barium)
Barite (Barium) Chapter D of Critical Mineral Resources of the United States—Economic and Environmental Geology and Prospects for Future Supply Professional Paper 1802–D U.S. Department of the Interior U.S. Geological Survey Periodic Table of Elements 1A 8A 1 2 hydrogen helium 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 lithium beryllium boron carbon nitrogen oxygen fluorine neon 6.94 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 13 14 15 16 17 18 sodium magnesium aluminum silicon phosphorus sulfur chlorine argon 22.99 24.31 3B 4B 5B 6B 7B 8B 11B 12B 26.98 28.09 30.97 32.06 35.45 39.95 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 potassium calcium scandium titanium vanadium chromium manganese iron cobalt nickel copper zinc gallium germanium arsenic selenium bromine krypton 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.93 58.69 63.55 65.39 69.72 72.64 74.92 78.96 79.90 83.79 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 rubidium strontium yttrium zirconium niobium molybdenum technetium ruthenium rhodium palladium silver cadmium indium tin antimony tellurium iodine xenon 85.47 87.62 88.91 91.22 92.91 95.96 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 cesium barium hafnium tantalum tungsten rhenium osmium iridium platinum gold mercury thallium lead bismuth polonium astatine radon 132.9 137.3 178.5 180.9 183.9 186.2 190.2 192.2 195.1 197.0 200.5 204.4 207.2 209.0 (209) (210)(222) 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 -
What Are Ochre and Umber?
What a「e O⊂hre and Umber? 100% Natu「al I「on Oxide Pigments 〃柵e most economic。l p毎men誌fn the血dustγ’’ ochre (PrOnOunCed o′-ker) is a natura一′ mineral′ earth pigment. Chemic訓y′ it is a hyd「ated ferric oxide′ Chemical formulation: FeO(OH). Och「e is inorganic, Chemica一一y ine「t′ nOn-reaCtive with cement′ mO「tar Or brick′ and New Riverside produces two grades ofOchre pigments that are caIled 548 0chre and NIROX412. 548 Ochre is s=ghtlydarke「・ NIROX412 is mo「e yel看ow and has a greater tint strength. ochre is mined and processed in Cartersv紺e′ GAatthe oniyyear-rOund Ochre mInlng and processing operation in the United States. How応O`hre used? Ochre can be used aIone as a singie pigmentto achieve a range ofcoIors from light bu什to dark bu什simpIy byvaryingthe addition rate. As a wayto achieve a broader range ofcoIorswith a higheryeIIow or red shade, Ochre mayaIso be blended with synthetic pigments and used as a cost effective base. 548 0chre is a brown-yeIIow′ refined natu「al iron OXide pigment (Fe203) with an average particIe Size of-3 microns. it isthe mosteconomicaI bu什 COIor in the pigment industry. Broad appIication use for aii cement appiications. 5櫛くわhIe Umber is a contro看led productfrom a manganese enriched fo「m ofgoethite, a natur訓yoccurrIng InOrganic iron oxide. it is a brown earth pigmentthat is darkerthan the Ochre because ofits manganese and iron oxide content. It is highiyvaiued as a pe「manent pigmenteither in the raw or burntstate. Umber is Iightfast, insoluble in water, 「eSistantto alkaIis and weak acids and non-reaCtive with cement, SOIvents, OiIs, and most resins. -
Reactivity of Dolomite in Water-Saturated Supercritical Carbon
Energy Conversion and Management 65 (2013) 564–573 Contents lists available at SciVerse ScienceDirect Energy Conversion and Management journal homepage: www.elsevier.com/locate/enconman Reactivity of dolomite in water-saturated supercritical carbon dioxide: Significance for carbon capture and storage and for enhanced oil and gas recovery ⇑ Xiuyu Wang a,1, Vladimir Alvarado b, Norbert Swoboda-Colberg a, John P. Kaszuba a,c, a Department of Geology and Geophysics, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA b Department of Chemical and Petroleum Engineering, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA c School of Energy Resources, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA article info abstract Article history: Carbon dioxide injection in porous reservoirs is the basis for carbon capture and storage, enhanced oil and Received 17 December 2011 gas recovery. Injected carbon dioxide is stored at multiple scales in porous media, from the pore-level as a Received in revised form 18 July 2012 residual phase to large scales as macroscopic accumulations by the injection site, under the caprock and Accepted 26 July 2012 at reservoir internal capillary pressure barriers. These carbon dioxide saturation zones create regions Available online 5 November 2012 across which the full spectrum of mutual CO2–H2O solubility may occur. Most studies assume that geo- chemical reaction is restricted to rocks and carbon dioxide-saturated formation waters, but this paradigm Keywords: ignores injection of anhydrous carbon dioxide against brine and water-alternating-gas flooding for Carbon capture and storage enhanced oil recovery. Enhanced oil recovery Enhanced gas recovery A series of laboratory experiments was performed to evaluate the reactivity of the common reservoir Fluid–rock interactions mineral dolomite with water-saturated supercritical carbon dioxide. -
CHALCOPYRITE Visiting
communication, 2000). The quarry is privately owned and permission must be obtained before CHALCOPYRITE visiting. 13. Groveland mine, near Felch. CuFeS2 Common as attractive microcrystals (DeMark, A widespread and common copper ore mineral 2000). occurring in veins, disseminations, or as replacement deposits. Northern Peninsula. Alpena County: 1. Lafarge Corporation, Great Lakes Region (formerly National Gypsum Company) quarry, Alpena: Rare, with calcite, dolomite, barite, sphalerite, marcasite, pyrite, and strontianite (Morris, 1983). 2. Paxton quarry, Paxton: With calcite, dolomite, quartz, sphalerite, pyrite, and marcasite (Morris, 1983). Baraga County: Ohio mines (Webster and Imperial mines), Imperial Heights near Michigamme: Associates are apatite, goethite, grunerite, graphite, palygorskite, carbonates, and Figure 56: A 1.3 mm chalcopyrite crystal on dolomite other sulfides (Morris, 1983; DeMark, 2000). from the Groveland mine, Dickinson County. Ramon Crystals on calcite rhombohedra. DeMark specimen, Dan Behnke photograph. Dickinson County: 1. Metronite quarry, 4 km east-northeast of Felch: In tremolite marble Gogebic County: 1. Eureka mine near Ramsay, (Randville Dolomite) along contact of aplite- sections 12 and 13, T47N, R46W: With pyrite and pegmatite dike and in marginal parts of the dike gold in quartz veins at contact between granite and itself (Heinrich, 1962b). 2. Rian’s quarry southeast the Palms slate (Dickey and Young, 1938). 2. of Felch: Similar occurrence (Pratt, 1954). 3. In Copp’s mine 10 km north of Marenisco: With iron formation of the Menominee iron range and galena, sphalerite, pyrite, and dolomite (Dana, also just north of Felch: Rare, usually associated 1892). 3. Roadside exposure on south side of with secondary pyrite (Pratt, 1954; Brower, 1968). -
Dolomite Deposit Near Marble Stevens County Washington
Dolomite Deposit Near Marble Stevens County Washington By CHARLES DEISS A CONTRIBUTION TO ECONOMIC GEOLOGY GEOLOGICAL SURVEY BULLETIN 1027-C A study of the geologic structure and petrology of a dolomite deposit UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1955 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract..-_ __________-_______-__-_-_______--_____---__-_-----____ 119 Introduction. _____________________________________________________ 120 Location of deposit-_--__-________-_-___--________-_-_____---____-- 120 Sedimentary rocks.________________________________________________ 121 Northport limestone- __--_--______--_-________-_-_______-._____ 122 Glacial drift... __________-________-__-___________--__---_-._ 122 Glacial lake deposits.__________________________________________ 123 [gneous rocks.___-_-__--__-_-_---_-___--_----__---__---._-_-__---_ 125 Lamprophyre dikes.____________--___-____-__----___-_----.__-- 125 Petrography of the dike rocks.-.__________-________----_-___ 126 Economic significance of the dikes___________________________ 128 Geologic structure.________________________________________________ 128 Faults ----------------------------------------------------- 129 Joints.-.-___-.__----_---_---__----__-_._-___-------_. 129 Structures in the quarry face.___________________________________ 130 Dolomite deposit-___-___---____-__--_.._---__--__---__-____-_-_---_ 130 Lithology of the dolomite...------._____________________________ 130 Breccia zones.________-_____-____-______-_--_____--_-__-__ 132 Chemical analyses.__---___-_________________________________-^ 132 Lithologic section and position of selected samples _________________ 132 Silica and other impurities.--_---______-_-_----_______-___-.__-_ 135 Origin of the dolomite._________________________________________ 138 Mining conditions and methods. -
A Color Mixing Guide. CREA Your Color Story with Colors You Practice in Advance and Love
Use the color cards in this kit as an optional tool as you create. Fill it up with favorite color blends as you work ORY through the workshop (and notes on OLOR ST TE A C how to achieve them again), or pre-plan A color mixing guide. CREA your color story with colors you practice in advance and love. The best way to design beautiful A quick intro to figuring out colors. color schemes is to play! I’m so excited and glad that you’ve decided to paint with me in this workshop. I really hope the information in this booklet is helpful. Don’t be afraid to outsource for further information, Pinterest is a great tool for color schemes, and you can find just about everything else on Google. Enjoy yourself and have fun! THE THE CRAFTER’S CRAFTER’S BOX BOX Mixing paint doesn’t have to be hard! Let’s be honest, mixing colors seems so complicated. I hear that all the time. And anyone who has tried their hand at blending colors and has ended up with several different shades of brown by accident knows what I’m saying. I’m hoping this guide will help walk you though this workshop and also give you the confidence to blend many different shades of brown on purpose. I should also mention that while I feel very knowledgeable about color theory in the application I use it, I’m not actually a master. If this guide isn’t helpful or is conflicting to your college level color theory course, feel free to gently place this in the trash. -
Color Chart Colorchart
Color Chart AMERICANA ACRYLICS Snow (Titanium) White White Wash Cool White Warm White Light Buttermilk Buttermilk Oyster Beige Antique White Desert Sand Bleached Sand Eggshell Pink Chiffon Baby Blush Cotton Candy Electric Pink Poodleskirt Pink Baby Pink Petal Pink Bubblegum Pink Carousel Pink Royal Fuchsia Wild Berry Peony Pink Boysenberry Pink Dragon Fruit Joyful Pink Razzle Berry Berry Cobbler French Mauve Vintage Pink Terra Coral Blush Pink Coral Scarlet Watermelon Slice Cadmium Red Red Alert Cinnamon Drop True Red Calico Red Cherry Red Tuscan Red Berry Red Santa Red Brilliant Red Primary Red Country Red Tomato Red Naphthol Red Oxblood Burgundy Wine Heritage Brick Alizarin Crimson Deep Burgundy Napa Red Rookwood Red Antique Maroon Mulberry Cranberry Wine Natural Buff Sugared Peach White Peach Warm Beige Coral Cloud Cactus Flower Melon Coral Blush Bright Salmon Peaches 'n Cream Coral Shell Tangerine Bright Orange Jack-O'-Lantern Orange Spiced Pumpkin Tangelo Orange Orange Flame Canyon Orange Warm Sunset Cadmium Orange Dried Clay Persimmon Burnt Orange Georgia Clay Banana Cream Sand Pineapple Sunny Day Lemon Yellow Summer Squash Bright Yellow Cadmium Yellow Yellow Light Golden Yellow Primary Yellow Saffron Yellow Moon Yellow Marigold Golden Straw Yellow Ochre Camel True Ochre Antique Gold Antique Gold Deep Citron Green Margarita Chartreuse Yellow Olive Green Yellow Green Matcha Green Wasabi Green Celery Shoot Antique Green Light Sage Light Lime Pistachio Mint Irish Moss Sweet Mint Sage Mint Mint Julep Green Jadeite Glass Green Tree Jade -
Deep Olive Speckle
PC-1 Saturation Cone 5-6 Metallic* over PC-29 Deep Olive Speckle PC-4 PC-25 PC-30 Palladium Textured Temmoku over Turquoise over Layering PC-29 over PC-29 Deep Olive PC-29 Deep Olive Speckle Deep Olive Speckle Speckle PC-12 PC-27 PC-32 Blue Midnight Tourmaline Albany Slip over over Brown* PC-29 PC-29 over Deep Olive Deep Olive PC-29 Speckle Speckle Deep Olive Speckle PC-23 PC-28 PC-33 Indigo Float Frosted Iron Lustre over Turquoise over PC-29 over PC-29 Deep Olive PC-29 Deep Olive Speckle Deep Olive Speckle Speckle PC-29 Layering Notes: Brush on two Cups: Josh Heim over PC-34 layers of base coat. Brush on two layers Clay: AMACO® Buff Stoneware Clay No. 46 Light Sepia of top coat. (Let dry between coats.) Firing: Test tiles have been fired to Cone 6 over PC-29 www.layeringpcs.info PC-29 Deep Olive Deep Olive Speckle Speckle Join the conversation www.facebook.com/groups/potterschoiceex vary may Color between printed copies. PC-35 PC-41 PC-52 Oil Spot Vert Lustre Deep Sienna over over Speckle PC-29 PC-29 over Deep Olive Deep Olive PC-29 Speckle Speckle Deep Olive Speckle PC-36 PC-42 PC-53 Ironstone Seaweed Ancient Jasper over over over PC-29 PC-29 PC-29 Deep Olive Deep Olive Deep Olive Speckle Speckle Speckle PC-37 PC-43 PC-55 Smoked Toasted Sage Chun Plum Sienna over over over PC-29 PC-29 PC-29 Deep Olive Deep Olive Deep Olive Speckle Speckle Speckle PC-39 PC-46 PC-59 Umber Float Lustrous Jade Deep over over Firebrick PC-29 PC-29 over Deep Olive Deep Olive PC-29 Speckle Speckle Deep Olive Speckle The Art & Creative Materials Institute AP (Approved PC-49 PC-60 Product) seal certifies this product to be safe for use Frosted Melon Salt Buff* by all ages.