Psilomelane [(Bah2o)2Mn5o10]
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Geology and Mineral Deposits of the James River-Roanoke River Manganese District Virginia
Geology and Mineral Deposits of the James River-Roanoke River Manganese District Virginia GEOLOGICAL SURVEY BULLETIN 1008 Geology and Mineral ·Deposits oftheJatnes River-Roanoke River Manganese District Virginia By GILBERT H. ESPENSHADE GEOLOGICAL SURVEY BULLETIN 1008 A description of the geology anq mineral deposits, particularly manganese, of the James River-Roanoke River district UNITED STAT.ES GOVERNMENT, PRINTING. OFFICE• WASHINGTON : 1954 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---------------------------------------------------------- 1 Introduction______________________________________________________ 4 Location, accessibility, and culture_______________________________ 4 Topography, climate, and vegetation _______________ .,.. _______ ---___ 6 Field work and acknowledgments________________________________ 6 Previouswork_________________________________________________ 8 GeneralgeologY--------------------------------------------------- 9 Principal features ____________________________ -- __________ ---___ 9 Metamorphic rocks____________________________________________ 11 Generalstatement_________________________________________ 11 Lynchburg gneiss and associated igneous rocks________________ 12 Evington groUP------------------------------------------- 14 Candler formation_____________________________________ 14 Archer Creek formation________________________________ -
The Nature of Waste Associated with Closed Mines in England and Wales
The nature of waste associated with closed mines in England and Wales Minerals & Waste Programme Open Report OR/10/14 BRITISH GEOLOGICAL SURVEY MINERALS & WASTE PROGRAMME OPEN REPORT OR/10/14 The National Grid and other Ordnance Survey data are used with the permission of the The nature of waste associated Controller of Her Majesty’s Stationery Office. OS Topography © Crown with closed mines in England and Copyright. All rights reserved. BGS 100017897/2010 Wales Keywords Abandoned mine waste facilities; Palumbo-Roe, B and Colman, T England and Wales; mineral deposits; environmental impact; Contributor/editor European Mine Waste Directive. Cameron, D G, Linley, K and Gunn, A G Front cover Graiggoch Mine (SN 7040 7410), Ceredigion, Wales. Bibliographical reference Palumbo-Roe, B and Colman, T with contributions from Cameron, D G, Linley, K and Gunn, A G. 2010. The nature of waste associated with closed mines in England and Wales. British Geological Survey Open Report, OR/10/14. 98pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and the Environment Agency that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. The views and statements expressed in this report are those of the authors alone and do not necessarily represent the views of the Environment Agency. -
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 -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
The Mineral Industry of Burundi in 2016
2016 Minerals Yearbook BURUNDI [ADVANCE RELEASE] U.S. Department of the Interior January 2020 U.S. Geological Survey The Mineral Industry of Burundi By Thomas R. Yager In 2016, the production of mineral commodities—notably can be found in previous editions of the U.S. Geological Survey gold, tantalum, tin, and tungsten—represented only a minor Minerals Yearbook, volume III, Area Reports—International— part of the economy of Burundi (United Nations Economic Africa, which are available at https://www.usgs.gov/centers/ Commission for Africa, 2017). The legislative framework for nmic/africa-and-middle-east. the mineral sector in Burundi is provided by the Mining Code of Burundi (law No. 1/21 of October 15, 2013). The legislative Reference Cited framework for the petroleum sector is provided by the Mining United Nations Economic Commission for Africa, 2017, Burundi, in African and Petroleum Act of 1976. Data on mineral production are statistical yearbook 2017: United Nations Economic Commission for Africa, in table 1. Table 2 is a list of major mineral industry facilities. p. 113–117. (Accessed November 7, 2018, at https://www.uneca.org/sites/ More-extensive coverage of the mineral industry of Burundi default/files/PublicationFiles/asyb-2017.pdf.) TABLE 1 BURUNDI: PRODUCTION OF MINERAL COMMODITIES1 (Metric tons, gross weight, unless otherwise specified) Commodity2 2012 2013 2014 2015 2016 METALS Gold, mine, Au contente kilograms 500 400 500 500 500 Niobium and tantalum, mine, columbite-tantalite concentrate: Gross weight do. 258,578 73,518 105,547 53,093 r 31,687 Nb contente do. 51,000 14,000 21,000 10,000 r 6,200 Ta contente do. -
Alphab Etical Index
ALPHAB ETICAL INDEX Names of authors are printed in SMALLCAPITALS, subjects in lower-case roman, and localities in italics; book reviews are placed at the end. ABDUL-SAMAD, F. A., THOMAS, J. H., WILLIAMS, P. A., BLASI, A., tetrahedral A1 in alkali feldspar, 465 and SYMES, R. F., lanarkite, 499 BORTNIKOV, N. S., see BRESKOVSKA, V. V., 357 AEGEAN SEA, Santorini I., iron oxide mineralogy, 89 Boulangerite, 360 Aegirine, Scotland, in trachyte, 399 BRAITHWAITE, R. S. W., and COOPER, B. V., childrenite, /~kKERBLOM, G. V., see WILSON, M. R., 233 119 ALDERTON, D. H. M., see RANKIN, A. H., 179 Braunite, mineralogy and genesis, 506 Allanite, Scotland, 445 BRESKOVSKA, V. V., MOZGOVA, N. N., BORTNIKOV, N. S., Aluminosilicate-sodalites, X-ray study, 459 GORSHKOV, A. I., and TSEPIN, A. I., ardaite, 357 Amphibole, microstructures and phase transformations, BROOKS, R. R., see WATTERS, W. A., 510 395; Greenland, 283 BULGARIA, Madjarovo deposit, ardaite, 357 Andradite, in banded iron-formation assemblage, 127 ANGUS, N. S., AND KANARIS-SOTIRIOU, R., autometa- Calcite, atomic arrangement on twin boundaries, 265 somatic gneisses, 411 CANADA, SASKATCHEWAN, uranium occurrences in Cree Anthophyllite, asbestiform, morphology and alteration, Lake Zone, 163 77 CANTERFORD, J. H., see HILL, R. J., 453 Aragonite, atomic arrangements on twin boundaries, Carbonatite, evolution and nomenclature, 13 265 CARPENTER, M. A., amphibole microstructures, 395 Ardaite, Bulgaria, new mineral, 357 Cassiterite, SW England, U content, 211 Arfvedsonite, Scotland, in trachyte, 399 Cebollite, in kimberlite, correction, 274 ARVlN, M., pumpellyite in basic igneous rocks, 427 CHANNEL ISLANDS, Guernsey, meladiorite layers, 301; ASCENSION ISLAND, RE-rich eudialyte, 421 Jersey, wollastonite and epistilbite, 504; mineralization A TKINS, F. -
Petrology of Nepheline Syenite Pegmatites in the Oslo Rift, Norway: Zr and Ti Mineral Assemblages in Miaskitic and Agpaitic Pegmatites in the Larvik Plutonic Complex
MINERALOGIA, 44, No 3-4: 61-98, (2013) DOI: 10.2478/mipo-2013-0007 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Petrology of nepheline syenite pegmatites in the Oslo Rift, Norway: Zr and Ti mineral assemblages in miaskitic and agpaitic pegmatites in the Larvik Plutonic Complex Tom ANDERSEN1*, Muriel ERAMBERT1, Alf Olav LARSEN2, Rune S. SELBEKK3 1 Department of Geosciences, University of Oslo, PO Box 1047 Blindern, N-0316 Oslo Norway; e-mail: [email protected] 2 Statoil ASA, Hydroveien 67, N-3908 Porsgrunn, Norway 3 Natural History Museum, University of Oslo, Sars gate 1, N-0562 Oslo, Norway * Corresponding author Received: December, 2010 Received in revised form: May 15, 2012 Accepted: June 1, 2012 Available online: November 5, 2012 Abstract. Agpaitic nepheline syenites have complex, Na-Ca-Zr-Ti minerals as the main hosts for zirconium and titanium, rather than zircon and titanite, which are characteristic for miaskitic rocks. The transition from a miaskitic to an agpaitic crystallization regime in silica-undersaturated magma has traditionally been related to increasing peralkalinity of the magma, but halogen and water contents are also important parameters. The Larvik Plutonic Complex (LPC) in the Permian Oslo Rift, Norway consists of intrusions of hypersolvus monzonite (larvikite), nepheline monzonite (lardalite) and nepheline syenite. Pegmatites ranging in composition from miaskitic syenite with or without nepheline to mildly agpaitic nepheline syenite are the latest products of magmatic differentiation in the complex. The pegmatites can be grouped in (at least) four distinct suites from their magmatic Ti and Zr silicate mineral assemblages. -
Manganese Deposits of Western Utah
Manganese Deposits of Western Utah GEOLOGICAL SURVEY BULLETIN 979-A Manganese Deposits of Western Utah By MAX D. CRITTENDEN, JR. , MANGANESE DEPOSITS OF UTAH, PART 1 GEOLOGICAL SURVEY BULLETIN 979-A A report on known deposits west of the lllth meridian * UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 19S1 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 50 cents (paper cover) CONTENTS Fag* Abstract.__________________________________________________________ 1 Introduction._._____.__________----_______-______-_--_------.__-__ 1 History of mining and production__.._______.______.___.__-___-_____ 2 Occurrence and age of the deposits_________-_____-_.-__-__-_-__--_- 6 Mineralogy _--____._____---_--_---_------------------------------- 7 Descriptions of the manganese minerals....____.__--_____-__-..__ 8 Oxides...___-__.--_--------___-_-_.-- . _ 8 Carbonates.___-____.__-____________-_-___-----_--------__ 9 Silicate.,_ _____-----_____--__-_______-_---___-__--___._--. 9 Relative stability and manganese content______--_----------_----_ 10 Oxidation and enrichment._____________________________________ 10 Classification and origin of the deposits....______.__._____---.___.-_-_ 11 General discussion_____________________________________________ 11 Syngenetic deposits_-_--____-----_--------------_-------__-_-.- 13 Bedded depositS-__________-_____._____..__________________ 13 Spring -
Tin, Tungsten, and Tantalum Deposits of South Dakota
TIN, TUNGSTEN, AND TANTALUM DEPOSITS OF SOUTH DAKOTA. By FRANK L. HESS. INTRODUCTION. Many articles have been written 011 the tin deposits of the Black Hills, and an excellent paper by J. D. Irving a on the tungsten deposits at Lead was published in 1901. Nothing is known to have been pub lished on the tungsten deposits of the southern Black Hills, but several articles have been written on the deposits of tantalum. Nearly all the papers on these different deposits, however, are a num ber of years old, and later developments have given several of the deposits an aspect somewhat different from their appearance at the time they were described. It therefore seems well to give a brief account of observations made by the writer during a short reconnais sance trip in September, 1908, together with such reviews of the his tory and the literature of the region as may seem advisable. All the known deposits of tin, tungsten, and tantalum in South Dakota occur in the Black Hills, in Lawrence and Pennington coun ties, in the southwestern part of the State. Although designated as "hills," these elevations reach a height of 7,216 feet in Harney Peak, 500 feet above the highest of the Appalachians (Mount Mitchell, 6,711 feet) and almost a thousand feet above the highest of the White Mountains (Mount Washington, 6,279 feet). They are about 60 to 75 miles long by 50 miles wide, the longer axis lying nearly north and south. There is a considerable diversity of topography in the different parts of the area to be considered. -
Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia
minerals Article Chemical Composition and Petrogenetic Implications of Eudialyte-Group Mineral in the Peralkaline Lovozero Complex, Kola Peninsula, Russia Lia Kogarko 1,* and Troels F. D. Nielsen 2 1 Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 119991 Moscow, Russia 2 Geological Survey of Denmark and Greenland, 1350 Copenhagen, Denmark; [email protected] * Correspondence: [email protected] Received: 23 September 2020; Accepted: 16 November 2020; Published: 20 November 2020 Abstract: Lovozero complex, the world’s largest layered peralkaline intrusive complex hosts gigantic deposits of Zr-, Hf-, Nb-, LREE-, and HREE-rich Eudialyte Group of Mineral (EGM). The petrographic relations of EGM change with time and advancing crystallization up from Phase II (differentiated complex) to Phase III (eudialyte complex). EGM is anhedral interstitial in all of Phase II which indicates that EGM nucleated late relative to the main rock-forming and liquidus minerals of Phase II. Saturation in remaining bulk melt with components needed for nucleation of EGM was reached after the crystallization about 85 vol. % of the intrusion. Early euhedral and idiomorphic EGM of Phase III crystalized in a large convective volume of melt together with other liquidus minerals and was affected by layering processes and formation of EGM ore. Consequently, a prerequisite for the formation of the ore deposit is saturation of the alkaline bulk magma with EGM. It follows that the potential for EGM ores in Lovozero is restricted to the parts of the complex that hosts cumulus EGM. Phase II with only anhedral and interstitial EGM is not promising for this type of ore. -
Cycle Processing of Tantalum Bearing Minerals
Journal of Minerals & Materials Characterization & Engineering, Vol. 6, No.1, pp 69-77, 2007 jmmce.org Printed in the USA. All rights reserved Adaptable Technologies for Life – Cycle Processing of Tantalum Bearing Minerals Amuda, M. O. H., Esezobor, D. E., and Lawal, G. I. Department of Metallurgical and Materials Engineering University of Lagos, Lagos, Nigeria. Corresponding Author: [email protected] ABSTRACT Nigeria is richly endowed in convertible natural resources of which solid minerals are a member of the endowments. However, the country is basically a mono-product economy based on its vast oil deposit accounting for over 84% of foreign earnings and 25% of GDP. The triple challenges of the volatile nature of global oil politics, achieving the objectives of the millennium development goals and the national economy empowerment and development strategies calls for diversification into hitherto neglected solid mineral deposits to open a window of opportunities. One of the widely reported mineral deposits in the country with strong international influence is tantalum-bearing mineral. The mineral had in the past few decades experienced a strong growth in demand averaging 10% per annum since 1992 with total world consumption estimated at over 38 thousand tonne in 2005. The total annual supply of the ore concentrate in 2001 was 720 tonnes when demand was 26 thousand tonnes. Thus, pushing the price of the concentrate to an all time high of $165 / kg in 2001. This paper outlines the characteristics of the Nigerian tantalum reserves. It also presents the evaluation of the competing technologies for complete cycle processing of tantalum bearing minerals for adoption in the Nigeria solid mineral industry. -
Compositional Trend in the Specks of Tantalite, Tourmaline and Beryl Hosted Within Complex Basement Rocks Using Geophysical and Geochemical Methods of Exploration
IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861. Volume 3, Issue 4 (Mar. - Apr. 2013), PP 24-33 www.iosrjournals.org Compositional Trend in the Specks of Tantalite, Tourmaline and Beryl Hosted within Complex Basement Rocks Using Geophysical and Geochemical Methods of Exploration B. S. Badmus, O. D. Akinyemi, *A. M. Gbadebo, P. Babatunde, O. T. Olurin and S. A. Ganiyu Department of Physics, Federal University of Agriculture, Abeokuta, Nigeria *Department of Environmental Management and Toxicology, Federal University of Agriculture, Abeokuta, Abeokuta, Nigeria Abstract: Vertical Electrical Sounding (VES) using Schlumberger array was employed in data collection. Data acquisition was carried out along Oyan river bank with a total of twenty-three (23) soundings. This location was divided into two zones: VES 01 -09 and VES 10 -23. Rock samples hosting specks of tantalite, tourmaline and beryl were collected from the artisan pits within the study area and taken for geochemical analysis in the laboratory. The result of geochemical analyses revealed the quality of the solid minerals in terms of mineral compositions (major, trace and rare earth elements) while geophysical field measurement revealed the resistivity values, vertical and lateral distributions and depth of the solid minerals. The range of electrical resistivity values of these solid minerals as revealed by laboratory measurement is 19.4 - 31.1Ωm while that of the host rock is 10.0 – 100.0Ωm as obtained from field measurements. Specks of tantalite, tourmaline and beryl were suspected to be sparsely distributed in other VES locations except at VES02 and 09, where vast deposits were suspected.