Polymetallic Nodule Mining: Innovative Concepts for Commercialisation
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Published by Srl • Via Mario Donati, 6 • 20146 Milano (Italy)
published by srl • Via Mario Donati, 6 • 20146 Milano (Italy) NEWS ARISTA INDUSTRIES NEWS Arista Industries offers Omega-3 fatty acids, which are necessary for maintaining overall heart health and general wellness. It has been said that Omega-3 Oils help improve cardiovascular health and reduce the risk of heart disease and stroke, help lower triglyceride levels and reduce cholesterol. Arista offers various potencies of Omega-3 Fish Oil from Sardine and Anchovy as well Salmon, Tuna and Krill. The NEWS Omega-3 Vegetable Oils offered include Flax Seed, Perilla, Chia Seed, Sacha Inchi, Rose Hip Seed and Hemp Seed Oils. BIO-GEN EXTRACTS PVT. LTD Bio-gen Extracts Pvt. Ltd, established in the year 2000, is a GMP Certified, Bulk Actives & Nutraceuticals manufacturing company. The company inaugurated its EU GMP Compliant Manufacturing Unit last year. Bio-gen’s strong products are NEWS KAPPA BIOSCIENCE AS Glucosamine, Lycopene, Lutein, Beta Carotene, Soy Isoflavones, Citrus Kappa Bioscience AS is the innovative leader and Bioflavonoids, Green Tea Ext. first mover with its patent protected, high purity etc. ® all-trans vitamin K2 as menaquinone-7 (MK-7). We deliver our vitamin K2, branded as K2VITAL on various commercially suitable carriers, such as NEWS MCC, MCT & microencapsulated powder. Driven by our core vision to make Vitamin K2 MK-7 available for everyone, we own and manage the whole value chain – from production to sales. NEPTUNE TECHNOLOGIES & BIORESSOURCES Neptune Technologies & Bioressources is the NEWS first company to have developed, researched for almost two decades, and commercialized krill oil in the Healthcare industry, creating the NKO® Brand (Neptune Krill Oil™), considered as the Original Krill Oil. -
Overview of Tungsten Indicator Minerals Scheelite and Wolframite with Examples from the Sisson W-Mo Deposit, Canada
Overview of tungsten indicator minerals scheelite and wolframite with examples from the Sisson W-Mo deposit, Canada M. Beth McClenaghan1, M.A. Parkhill2, A.A. Seaman3, A.G. Pronk3, M. McCurdy1 & D.J. Kontak4 1Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8 (e-mail: [email protected]) 2New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 50, Bathurst, New Brunswick, Canada E2A 3Z1 3New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 6000, Fredericton, New Brunswick, Canada E3B 5H1 4Department of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada P3E 2C6 These short course notes provide an overview of published lit- Table 1. List of regional surveys and case studies conducted around erature on the use of scheelite and wolframite as indicator min- the world in which scheelite and/or wolframite in surficial sediments erals for W, Mo, and Au exploration. The use of scheelite and have been used as indicator minerals. wolframite in stream sediments is well documented for mineral Mineral Media Location Source of Information exploration but less so for using glacial sediments (Table 1). scheelite stream sediments Pakistan Asrarullah (1982) wolframite stream sediments Burma ESCAP Scretariat (1982) The Geological Survey of Canada has recently conducted a scheelite, wolframite stream sediments USA Theobald & Thompson (1960) glacial till and stream sediment indicator mineral case study scheelite stream sediments, soil Thailand Silakul (1986) around the Sisson W-Mo deposit in eastern Canada. scheelite stream sediments Greenland Hallenstein et al. (1981) Preliminary indicator mineral results from this ongoing study scheelite stream sediments Spain Fernández-Turiel et al. -
The H/F Ratio As an Indicator of Contrasted Wolframite Deposition Mechanisms
Ore Geology Reviews 104 (2019) 266–272 Contents lists available at ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev Short communication The H/F ratio as an indicator of contrasted wolframite deposition T mechanisms ⁎ Julie Anne-Sophie Michaud , Michel Pichavant Université d'Orléans/CNRS/ISTO/BRGM, UMR 7327, 1A rue de la Férollerie, 45100 Orléans, France ARTICLE INFO ABSTRACT Keywords: Understanding wolframite deposition mechanisms is a key to develop reliable exploration guides for W. In quartz Wolframite veins from the Variscan belt of Europe and elsewhere, wolframites have a wide range of compositions, from Hübnerite hübnerite- (MnWO4) to ferberite-rich (FeWO4). Deposition style, source of Mn and Fe, distance from the heat/ W deposition fluid source and temperature have been proposed to govern the wolframite H/F (hübnerite/ferberite ratio) Magmatic control defined as 100 at. Mn/(Fe + Mn). The Argemela mineralized district, located near the world-class Panasqueira W ore deposit W mine in Portugal, exposes a quartz-wolframite vein system in close spatial and genetic association with a rare- Veins metal granite. Wolframite is absent as a magmatic phase, but W-rich whole-rock chemical data suggest that the granite magma is the source of W. Wolframite occurs as large homogeneous hübnerites (H/F = 64–75%) co- existing with montebrasite, K-feldspar and cassiterite in the latest generation of intragranitic veins corre- sponding to magmatic fluids exsolved from the granite. Locally, early hübnerites evolve to late more Fe-rich compositions (H/F = 45–55%). In a country rock vein, an early generation of Fe-rich hübnerites (H/ F = 50–63%) is followed by late ferberites (H/F = 6–23%). -
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 -
UNIVERSITY of CALIFORNIA Santa Barbara Ancient Plant Use and the Importance of Geophytes Among the Island Chumash of Santa Cruz
UNIVERSITY OF CALIFORNIA Santa Barbara Ancient Plant Use and the Importance of Geophytes among the Island Chumash of Santa Cruz Island, California A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Anthropology by Kristina Marie Gill Committee in charge: Professor Michael A. Glassow, Chair Professor Michael A. Jochim Professor Amber M. VanDerwarker Professor Lynn H. Gamble September 2015 The dissertation of Kristina Marie Gill is approved. __________________________________________ Michael A. Jochim __________________________________________ Amber M. VanDerwarker __________________________________________ Lynn H. Gamble __________________________________________ Michael A. Glassow, Committee Chair July 2015 Ancient Plant Use and the Importance of Geophytes among the Island Chumash of Santa Cruz Island, California Copyright © 2015 By Kristina Marie Gill iii DEDICATION This dissertation is dedicated to my Family, Mike Glassow, and the Chumash People. iv ACKNOWLEDGEMENTS I am indebted to many people who have provided guidance, encouragement, and support in my career as an archaeologist, and especially through my undergraduate and graduate studies. For those of whom I am unable to personally thank here, know that I deeply appreciate your support. First and foremost, I want to thank my chair Michael Glassow for his patience, enthusiasm, and encouragement during all aspects of this daunting project. I am also truly grateful to have had the opportunity to know, learn from, and work with my other committee members, Mike Jochim, Amber VanDerwarker, and Lynn Gamble. I cherish my various field experiences with them all on the Channel Islands and especially in southern Germany with Mike Jochim, whose worldly perspective I value deeply. I also thank Terry Jones, who provided me many undergraduate opportunities in California archaeology and encouraged me to attend a field school on San Clemente Island with Mark Raab and Andy Yatsko, an experience that left me captivated with the islands and their history. -
Minerals and Mineral Products in Our Bedroom Bed Hematite
Minerals and Mineral Products in our Bedroom Make-Up Kit Muscovite Bed Talc Hematite: hinges, handles, Mica mattress springs Hematite: for color Chromite: chrome plating Bismuth Radio Barite Copper: wiring Plastic Pail Quartz: clock Mica Gold: connections Cassiterite: solder Toilet Bowl / Tub Closet Feldspar: porcelain Chromite: chrome plating Pyrolusite: coloring Hematite: hinges, handles (steel) Chromite: plumbing fixtures Quartz : mirror on door Copper: tubing Desk Toothpaste Hematite: hinges, handles (steel) Apatite: teeth Chromite: chrome plating Fluorite: toothpaste Mirror Rutile: to color false Hematite: handle, frame teeth yellow Chromite: plating Gold: fillings Gold: plating Cinnabar: fillings Quartz: mirror Towels Table Lamp Sphalerite: dyes Brass (an alloy of copper and Chromite: dyes zinc): base Quartz: bulb Water Pipe/Faucet/Shower bulb Wolframite: lamp filament Brass Copper: wiring Iron Nickel Minerals and Mineral Products in our Bedroom Chrome: stainless steel Bathroom Cleaner Department of Environment and Natural Resources Borax: abrasive, cleaner, and antiseptic MINES AND GEOSCIENCES BUREAU Deodorant Spray Can Cassiterite Chromite Copper Carpet Quartz Sphalerite: dyes Telephone Chromite: dyes Drinking Glasses Copper: wiring Sulfur: foam padding Quartz Chromite: plating Gold: red color Clock Silver: electronics Pentlandite: spring Graphite: batteries Refrigerator Quartz: glass, time keeper Hematite Television Chromite: stainless steel Chromite: plating Computer Galena Wolframite: monitor Wolframite: monitor Copper Copper: -
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. -
Vitafoods Europe 2018 - Stand by Stand Guide
Vitafoods Europe 2018 - Stand by Stand Guide Index of Exhibitors Table of Contents Abies Labs d.o.o. – O76 4 Activ’Inside – G55 4 Advanced Enzyme Technologies Limited – D67 5 AIBMR Life Sciences – B73 5 Alchem Internation / AlchemLife – L30 5 Algalif – E54 6 Allmicroalgae – M125 6 analyze and realize GmbH – E75 7 Aquavan Technology - L101 7 aT Center – K160 8 Atlantia Food Clinical Trials Ltd. – L120 8 Aurora Biofarma Nekkar Lab – R170 9 BakeryPro Italia/Panificio Zorzi – Q173 9 Baïa Food Co. – J86 9 BioCell Technology LLC – M50 10 Biohit Oyj – Q175 10 Bioiberica S.A.U – F50 10 Biotec BetaGlucans AS – F181 11 BIOSEARCH LIFE – H45 11 Berryceuticals bv – C172 12 bitop AG – T142 12 Bormioli Pharma – D40 13 Brudy Technology SL – K155 13 BUCHI Labortechnik AG – E77 13 CF Pharma (Ireland) Ltd – J179 14 Chen-chee Grains and Consumable Oils Co., Ltd – F146 14 Crius Life Sciences Pvt Ltd. – T132 15 Doctor’s Formulas – M32 15 Dayonix Pharma GmbH – L82 15 Ecuadorian Rainforest, LLC – B58 16 ecoduna AG – I164 16 ELADIET – N12 17 Energy Group A.S – T143 17 Evonik Industries AG – H20 17 Evolva – L149 18 Extractis – K63 18 FaberFarma division of Farmalabor srl – R170 19 F. Hunziker & Co AG – M64 19 FederSalus – R170 20 FlaNat Research Italia – N67 20 Foodarom – M76 20 Frutarom Health – C20 21 Fytexia – I81 21 GeneChem Inc. – I74 22 Giellepi SpA – D20 22 Glanbia Nutritionals – H82 22 Global Health Industries – I131 23 Gnosis Bioresearch SA – I40 23 GoldNutrition – Q169 24 Graminex LLC – D50 24 HANF FARM GmbH – O164 25 Hankintatukku Oy – M124 25 Health Sources Nutrition Company Limited – L102 25 Hempro International GmbH & Co. -
Colorado Ferberite and the Wolframite Series A
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OT1S SMITH, DIRECTOR .jf BULLETIN 583 \ ' ' COLORADO FERBERITE AND THE r* i WOLFRAMITE SERIES A BY FRANK L. HESS AND WALDEMAR T. SCHALLER WASHINGTON GOVERNMENT FEINTING OFFICE 1914 CONTENTS. THE MINERAL RELATIONS OF FERBERiTE, by Frank L. Hess.................. 7 Geography and production............................................. 7 Characteristics of the ferberite.......................................... 8 " Geography and geology of the Boulder district........................... 8 Occurrence, vein systems, and relations................................. 9 Characteristics of the ore.............................................. 10 Minerals associated with the ferberite................................... 12 Adularia.......................................................... 12 Calcite........................................................... 12 Chalcedony....................................................... 12 Chalcopyrite...................................................... 12 Galena........................................................... 12 Gold and silver.................................................... 12 Hamlinite (?).................................................... 14 Hematite (specular)................................................ 15 Limonite........................................................ 16 Magnetite........................................................ 17 Molybdenite..................................................... 17 Opal............................................................ -
Porphyry Deposits
PORPHYRY DEPOSITS W.D. SINCLAIR Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, K1A 0E8 E-mail: [email protected] Definition Au (±Ag, Cu, Mo) Mo (±W, Sn) Porphyry deposits are large, low- to medium-grade W-Mo (±Bi, Sn) deposits in which primary (hypogene) ore minerals are dom- Sn (±W, Mo, Ag, Bi, Cu, Zn, In) inantly structurally controlled and which are spatially and Sn-Ag (±W, Cu, Zn, Mo, Bi) genetically related to felsic to intermediate porphyritic intru- Ag (±Au, Zn, Pb) sions (Kirkham, 1972). The large size and structural control (e.g., veins, vein sets, stockworks, fractures, 'crackled zones' For deposits with currently subeconomic grades and and breccia pipes) serve to distinguish porphyry deposits tonnages, subtypes are based on probable coproduct and from a variety of deposits that may be peripherally associat- byproduct metals, assuming that the deposits were econom- ed, including skarns, high-temperature mantos, breccia ic. pipes, peripheral mesothermal veins, and epithermal pre- Geographical Distribution cious-metal deposits. Secondary minerals may be developed in supergene-enriched zones in porphyry Cu deposits by weathering of primary sulphides. Such zones typically have Porphyry deposits occur throughout the world in a series significantly higher Cu grades, thereby enhancing the poten- of extensive, relatively narrow, linear metallogenic tial for economic exploitation. provinces (Fig. 1). They are predominantly associated with The following subtypes of porphyry deposits are Mesozoic to Cenozoic orogenic belts in western North and defined according to the metals that are essential to the eco- South America and around the western margin of the Pacific nomics of the deposit (metals that are byproducts or poten- Basin, particularly within the South East Asian Archipelago. -
Stable Isotope Studies of Quartz-Vein Type Tungsten Deposits in Dajishan Mine, Jiangxi Province, Southeast China
Stable Isotope Geochemistry: A Tribute to Samuel Epstein © The Geochemical Society, Special Publication No.3, 1991 Editors: H. P. Taylor, Jr., J. R. O'Neil and I. R. Kaplan Stable isotope studies of quartz-vein type tungsten deposits in Dajishan Mine, Jiangxi Province, Southeast China YUCH-NING SHIEH Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907, U.S.A. and GUO-XIN ZHANG Institute of Geochemistry (Guangzhou Branch), Academia Sinica, Guangzhou, Guangdong 510640, People's Republic of China Abstract-The Dajishan tungsten deposits belong to the wolframite-quartz vein type. These occur as fissure-fillings in the contact zone between the Jurassic Yenshanian granites and Cambrian meta- sandstones and slates. Quartz, beryl, muscovite, wolframite, scheelite, and sulfides are the major minerals formed in the main stage of mineralization. Late-stage minerals include calcite, dolomite, quartz, fluorite, and scheelite (replacing wolframite). No granitic rocks are exposed at the surface, but drilling has revealed hidden granitic bodies ranging in composition from biotite granite and two- mica granite to muscovite granite and pegmatite. These may represent a differentiation series from a common magma. Exceedingly uniform 0180 values are found in the minerals from the main-stage veins: quartz = 11.1-12.7 (n = 27), muscovite = 8.4-10.0 (n = 22), wolframite = 4.1-5.3 (n = 15), scheelite = 4.2-5.5 (n = 4), suggesting that isotopic equilibrium apparently has attained and that relatively constant physico-chemical conditions prevailed throughout the main-stage of mineralization. Oxygen isotope fractionations for .quartz-wolframite, quartz-scheelite, and quartz-muscovite pairs give concordant isotopic temperatures of 320-390°C, consistent with results from fluid inclusion 018 oD studies. -
39015003286252.Pdf
raY a ... 3 4 _' J t+..,+1 /y s t O'C4 LOOM lescE NATUML- 010SIS OF THE TUNGSTEN EPOSITS OF THE UNITED STATES 4 Itoag tn February,. 1936 CONTENTS INTRODUCTION .. .. .............................. 1 LOCATION AND DISTRIBUTION ............................... 2 TYPES OF DEPOSITS OF COMMERCIAL TUNGSTEN ORE...........lO1 Pyrometasomatic deposits ................. ........ 10 Hypothermal deposits .................. S......0.12 Mesothermal deposits.......................... .12 Epithermal deposits...............................13 General features .... ............ .. .. .. 16 Non-Commercial Deposits .. .. ... .. ... ... .. .. .. ... .. 19 Segregation deposits .. .. ... .. .. ... .,.. .. .,.. .19 General features . ..... ....... .. .. .. 19 General features ......... ... .. .. .. .. .".". ."20 Associated minerals.. .. .". .. ."..".."""" 21 Commercial Deposits . .... * . .. .29.. Pyrometasomatic or contact-metamorphic deposits... .22 Location of deposits ............. "..... ... "". 23 Intrusive rocks. .. .23 CONTENTS (concluded) Sedimnrta~ry rocks. ... ......9" . 0 . .24 Process of contacte-metamorphism.0........ .... 24 Size and form of the deposits ................. 26 Zones of metamorphism.................. ".O".S" .26 Progression of the contact-metamorphism. ..... .27 General features and classification..g09.....28 Associated minerals............... "." " " ..... "29. Outcrop of tungsten veins.9......0.. 00"03 Downward extent of tungsten ve ins...........3 Gelaeenral.fatur.. .. .. ... .. .. ..... .. ........ 39 General features.......9. .