Role of Sodium Carbonate in Scheelite Flotation – a Multi-Faceted Reagent
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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]. -
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. -
Geology of Tungsten Deposits in North-Central Chile
UNITED STATES DEPARTMENT OF THE INTERIOR J. A. Krug, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Bulletin 960-C GEOLOGY OF TUNGSTEN DEPOSITS IN NORTH-CENTRAL CHILE BY JAMES F. McALLISTER AND CARLOS RUIZ F. Prepared in cooperation with the DEPARTAMENTO DE MINAS Y PETROLED DE CHILE under the auspices of INTERDEPARTMENTAL COMMITTEE ON SCIENTIFIC AND CULTURAL COOPERATION, DEPARTMENT OF STATE Geologic Investigations in the American Republics, 1947 (Pages 89-108) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1948 For sale by the Superintendent of Documents, U. S. Government Printing Office, Washington 25, D. C. Price $1.75 CONTENTS Page Abstract____..______________________________._ 89 Introduction___________________________-__________ __________-___ 89 Geology_________________________________..._ 92 Rocks.____________________________________ 92 Structure____________________________________ 92 Minerals. _.---_.----_..---_.------_- _- -- 92 Type, size, and grade of ore deposits.------------._-----_-_-_-_-_ 93 Descriptions of mining properties__________-___-_-_-_---__--_---____- 94 Salamanca region____________________________________________ 94 Castaneda de Llamuco mine--___----------_-------_------__ 94 Picbe prospect... ________.- _ . 97 Domeyko region_______________________________________________ 97 El Durazno district.-..__-___.___--_____-__________...___ 97 Boliviana mine-..._________-____-._--._._-__-_--__-__. 99 Minillas property......____________________________________ 99 Vallenar region______________________________________________ 101 San Antonio mining property.______________________________ 102 Zapallo de Chehuque mining property_________*____-______- 104 Metric equivalents____-____-_____-_______-----_-__--_-_-_-__--_-- 106 Index.--.___-____-_._______________._______________ 107 Page PLATE 21. Geologic map of the Castaneda de Llamuco tungsten deposit. In pocket 22. Plan of workings, Castafieda de Llamuco mine. _-____-___ In pocket 23. -
Implications for Environmental and Economic Geology
UNIVERSITY OF CALIFORNIA RIVERSIDE Kinetics of the Dissolution of Scheelite in Groundwater: Implications for Environmental and Economic Geology A Thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Geological Sciences by Stephanie Danielle Montgomery March 2013 Thesis Committee: Dr. Michael A. McKibben, Chairperson Dr. Christopher Amrhein Dr. Timothy Lyons Copyright by Stephanie Danielle Montgomery 2013 The Thesis of Stephanie Danielle Montgomery is approved: _________________________________________ _________________________________________ _________________________________________ Committee Chairperson University of California, Riverside ABSTRACT OF THE THESIS Kinetics of the Dissolution of Scheelite in Groundwater: Implications for Environmental and Economic geology by Stephanie Danielle Montgomery Masters of Science, Graduate Program in Geological Sciences University of California, Riverside, March 2013 Dr. Michael McKibben, Chairperson Tungsten, an emerging contaminant, has no EPA standard for its permissible levels in drinking water. At sites in California, Nevada, and Arizona there may be a correlation between elevated levels of tungsten in drinking water and clusters of childhood acute lymphocytic leukemia (ALL). Developing a better understanding of how tungsten is released from rocks into surface and groundwater is therefore of growing environmental interest. Knowledge of tungstate ore mineral weathering processes, particularly the rates of dissolution of scheelite (CaWO4) in groundwater, could improve models of how tungsten is released and transported in natural waters. Our research focused on the experimental determination of the rates and products of scheelite dissolution in 0.01 M NaCl (a proxy for groundwater), as a function of temperature, pH, and mineral surface area. Batch reactor experiments were conducted within constant temperature circulation baths over a pH range of 3-10.5. -
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. -
Tungsten Minerals and Deposits
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 652 4"^ TUNGSTEN MINERALS AND DEPOSITS BY FRANK L. HESS WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Page. Introduction.............................................................. , 7 Inquiries concerning tungsten......................................... 7 Survey publications on tungsten........................................ 7 Scope of this report.................................................... 9 Technical terms...................................................... 9 Tungsten................................................................. H Characteristics and properties........................................... n Uses................................................................. 15 Forms in which tungsten is found...................................... 18 Tungsten minerals........................................................ 19 Chemical and physical features......................................... 19 The wolframites...................................................... 21 Composition...................................................... 21 Ferberite......................................................... 22 Physical features.............................................. 22 Minerals of similar appearance................................. -
Genesis of the Nanyangtian Scheelite Deposit in Southeastern Yunnan Province, China: Evidence from Mineral Chemistry, Fluid Incl
Acta Geochim (2018) 37(4):614–631 https://doi.org/10.1007/s11631-017-0257-0 ORIGINAL ARTICLE Genesis of the Nanyangtian scheelite deposit in southeastern Yunnan Province, China: evidence from mineral chemistry, fluid inclusions, and C–O isotopes 1 1 1 1 1 Qianru Cai • Yongfeng Yan • Guangshu Yang • Fuju Jia • Chao Li Received: 19 April 2017 / Revised: 22 November 2017 / Accepted: 26 December 2017 / Published online: 16 January 2018 Ó Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany, part of Springer Nature 2018 Abstract The Nanyangtian skarn-type scheelite deposit is the formation of the Nanyangtian deposit is related to an important part of the Laojunshan W–Sn polymetallic Laojunshan granitic magmatism. metallogenic region in southeastern Yunnan Province, China. The deposit comprises multiple scheelite ore bodies; Keywords Fluid inclusion Á C–O isotopes Á Skarn Á multilayer skarn-type scheelite ore bodies are dominant, Scheelite deposit Á Nanyangtian with a small amount of quartz vein-type ore bodies. Skarn minerals include diopside, hedenbergite, grossular, and epidote. Three mineralization stages exist: skarn, quartz– 1 Introduction scheelite, and calcite. The homogenization temperatures of fluid inclusions in hydrothermal minerals that formed in The Laojunshan W–Sn metallogenic district is an impor- different paragenetic phases were measured as follows: tant mineral resource base in Yunnan Province. Various 221–423 °C (early skarn stage), 177–260 °C (quartz– W–Sn polymetallic deposits surround the Laojunshan scheelite stage), and 173–227 °C (late calcite stage). The granitic pluton: the Nanyangtian-Chayeshan W metallo- measured salinity of fluid inclusions ranged from 0.18% to genic belt in the east, the Dazhushan-Xinzhai Sn–W met- 16.34% NaCleqv (skarn stage), 0.35%–7.17% NaCleqv allogenic belt in the north, and the Manjiazhai-Tongjie Zn– (quartz–scheelite stage), and 0.35%–2.24% NaCleqv (late Sn–In metallogenic belt in the southwest. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
Constraints of Molybdenite Re–Os and Scheelite Sm–Nd Ages on Mineralization Time of the Kukaazi Pb–Zn–Cu–W Deposit, Western Kunlun, NW China
Acta Geochim (2018) 37(1):47–59 https://doi.org/10.1007/s11631-017-0205-z ORIGINAL ARTICLE Constraints of molybdenite Re–Os and scheelite Sm–Nd ages on mineralization time of the Kukaazi Pb–Zn–Cu–W deposit, Western Kunlun, NW China 1 1,2 1 1 Chengbiao Leng • Yuhui Wang • Xingchun Zhang • Jianfeng Gao • 1,3 4 Wei Zhang • Xinying Xu Received: 29 March 2017 / Revised: 3 July 2017 / Accepted: 20 July 2017 / Published online: 26 July 2017 Ó Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany 2017 Abstract The Kukaazi Pb–Zn–Cu–W polymetallic similar REE patterns and Sm/Nd ratios to those of the deposit, located in the Western Kunlun orogenic belt, is a coeval granitoids in the region. Moreover, they also have newly discovered skarn-type deposit. Ore bodies mainly similar Sr and Nd isotopes [87Sr/86Sr = 0.7107–0.7118; occur in the forms of lenses and veins along beddings of the eNd(t) =-4.1 to -4.0] to those of such granitoids, imply- Mesoproterozoic metamorphic rocks. Three ore blocks, KI, ing that the tungsten-bearing fluids in the Kukaazi deposit KII, and KIII, have been outlined in different parts of the probably originate from the granitic magmas. Our results Kukaazi deposit in terms of mineral assemblages. The KI first defined that the Early Paleozoic granitoids could lead to ore block is mainly composed of chalcopyrite, scheelite, economic Mo–W–(Cu) mineralization at some favorable pyrrhotite, sphalerite, galena and minor pyrite, arsenopyrite, districts in the Western Kunlun orogenic belt and could be and molybdenite, whereas the other two ore blocks are prospecting exploration targets. -
Preliminary Model of Porphyry Copper Deposits
Preliminary Model of Porphyry Copper Deposits Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey Preliminary Model of Porphyry Copper Deposits By Byron R. Berger, Robert A. Ayuso, Jeffrey C. Wynn, and Robert R. Seal Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Berger, B.R., Ayuso, R.A., Wynn, J.C., and Seal, R.R., 2008, Preliminary model of porphyry copper deposits: U.S. Geological Survey Open-File Report 2008–1321, 55 p. iii Contents Introduction.....................................................................................................................................................1 Regional Environment ...................................................................................................................................3 -
Geology and Molybdenite Re–Os Age of the Dahutang Granite-Related Veinlets-Disseminated Tungsten Ore field in the Jiangxin Province, China
Ore Geology Reviews 53 (2013) 422–433 Contents lists available at SciVerse ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev Geology and molybdenite Re–Os age of the Dahutang granite-related veinlets-disseminated tungsten ore field in the Jiangxin Province, China Zhihao Mao a,⁎, Yanbo Cheng a,⁎, Jiajun Liu a, Shunda Yuan b, Shenghua Wu b, Xinkui Xiang c, Xiaohong Luo d a Faculty of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China b MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China c No. 916 Geological Team, Jiangxi Bureau of Geology, Mineral Resources, Exploration and Development, Jiujiang 332000, China d Northwestern Geological Team, Jiangxi Bureau of Geology, Mineral Resources, Exploration and Development, Shahe 332100, China article info abstract Article history: This is a brief research report about the recently-discovered and currently being explored Dahutang tungsten de- Received 15 October 2012 posit (or ore field) in northwestern Jiangxi, south-central China. The deposit is located south of the Middle–Lower Received in revised form 12 February 2013 Yangtze River valley Cu–Au–Mo–Fe porphyry–skarn belt (YRB). The mineralization is genetically associated with Accepted 13 February 2013 Cretaceous porphyritic biotite granite and fine-grained biotite granite and is mainly hosted within a Available online 19 February 2013 Neoproterozoic biotite granodiorite batholith.