Thermally Assisted Grinding of Cassiterite Associated with Pollimetallic Ore: a Comparison Between Microwave and Conventional Furnaces
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The Krásno Sn-W Ore District Near Horní Slavkov: Mining History, Geological and Mineralogical Characteristics
Journal of the Czech Geological Society 51/12(2006) 3 The Krásno Sn-W ore district near Horní Slavkov: mining history, geological and mineralogical characteristics Sn-W rudní revír Krásno u Horního Slavkova historie tìby, geologická a mineralogická charakteristika (47 figs, 1 tab) PAVEL BERAN1 JIØÍ SEJKORA2 1 Regional Museum Sokolov, Zámecká 1, Sokolov, CZ-356 00, Czech Republic 2 Department of Mineralogy and Petrology, National Museum, Václavské nám. 68, Prague 1, CZ-115 79, Czech Republic The tin-tungsten Krásno ore district near Horní Slavkov (Slavkovský les area, western Bohemia) belongs to the most important areas of ancient mining in the Czech Republic. The exceptionally rich and variable mineral associations, and the high number of mineral species, make this area one of the most remarkable mineralogical localities on a worldwide scale. The present paper reviews the data on geological setting of the ore district, individual ore deposits and mining history. Horní Slavkov and Krásno were known as a rich source of exquisite quality mineral specimens stored in numerous museum collections throughout Europe. The old museum specimens are often known under the German locality names of Schlaggenwald (= Horní Slavkov) and Schönfeld (=Krásno). The megascopic properties and paragenetic position of selected mineral classics are reviewed which include arsenopyrite, fluorapatite, fluorite, hübnerite, chalcopyrite, carpholite, cassiterite, quartz, molybdenite, rhodochrosite, sphalerite, topaz and scheelite. Key words: Sn-W ores; tin-tungsten mineralization; mining history; ore geology; mineralogy; Slavkovský les; Krásno, Horní Slavkov ore district; Czech Republic. Introduction valleys dissected parts of the area. In the ore district area, the detailed surface morphology is modified by large de- In the mining history of Central Europe, Bohemia and pressions caused by the collapse of old underground Moravia are known as important source of gold, silver, workings and by extensive dumps. -
Taylor Creek Tin Distrisl
tions such as Paramount Canyon, the veins TaylorCreek tin distrisl- may reach three to four centimeters in width and a few meters in height and length. A dis- seminated cassiterite halo has been noted stratigraphy,structure, around the veins in Squaw Creek. A recently discoveredrhyolite porphyry has andtiming of mineralizationintensely altered the surrounding country rock near NM-59 where the road crossesthe Conti- byTed L. Egglestonand David L Norman,New Mexico lnstitute of Miningand Technology, Socorro, NM nental Divide. This porphyry is locally quartz- sericite altered and contains as much as I go pyrite. Similar intrusives have been mapped Introduction The Taylor Creek tin district is located in by Woodard (1982) southeast of the Taylor Primary tin depositscommonly are found in the north-central Black Range some 80 km Creek region. granitic plutonic environments where the tin west of Truth or Consequences,New Mexico occurs as cassiterite in greisen veins and as (fig. l). Cassiteritenuggets were first found in Regional geology disseminations in altered granite (Taylor, placers (Fries, 1940a). in the district in 1909 The tin-bearing Taylor Creek Rhyolite is 1979).In southwest New Mexico, however, tin Shortly wood tin thereafter, cassiterite and located in the Mogollon-Datil volcanic field, a occurs as cassiterite in hematite-cassiterite were porphyritic found in vein depositsin rhy- mid-Tertiary volcanic field consisting of inter- veins which cut Tertiary rhyolite domes and placer (Hill, olite lavas as well as in deposits mediate to -
The Mineralogical Fate of Arsenic During Weathering Of
THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY A Thesis Presented to the faculty of the Department of Geology California State University, Sacramento Submitted in partial satisfaction of the requirements for the degree of MASTER OF SCIENCE in Geology by Tamsen Leigh Burlak SPRING 2012 © 2012 Tamsen Leigh Burlak ALL RIGHTS RESERVED ii THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY A Thesis by Tamsen Leigh Burlak Approved by: __________________________________, Committee Chair Dr. Charles Alpers __________________________________, Second Reader Dr. Lisa Hammersley __________________________________, Third Reader Dr. Dave Evans ____________________________ Date iii Student: Tamsen Leigh Burlak I certify that this student has met the requirements for format contained in the University format manual, and that this thesis is suitable for shelving in the Library and credit is to be awarded for the project. _______________________, Graduate Coordinator ___________________ Dr. Dave Evans Date Department of Geology iv Abstract of THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY by Tamsen Leigh Burlak Mine waste piles within the historic gold mining site, Empire Mine State Historic Park (EMSHP) in Grass Valley, California, contain various amounts of arsenic and are the current subject of remedial investigations to characterize the arsenic present. In this study, electron microprobe, QEMSCAN (Quantitative Evaluation of Minerals by SCANning electron microscopy), and X-ray absorption spectroscopy (XAS) were used collectively to locate and identify the mineralogical composition of primary and secondary arsenic-bearing minerals at EMSHP. -
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalj of the U. S. Atomic Energy Commission and is published with the permission of the , » Commission Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota By DOUGLAS M. SHERllDAN, HAL G. STEPHENS, MORTIMER H. STAATZ and JAMES J. NORTON PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Page Page Abstract.__________________________________________ 1 Geology Continued Introduction _______________________________________ 1 Peerless pegmatite Continued Location_____________________________________ 1 Chemical composition......____________ 17 History and production________________________ 2 Origin________ ____________________ _. 18 Past and present investigations.__________________ 3 Mineral deposits_____________________________ 21 Acknowledgments__________________________ 4 Mica__ _________ _________________________ 21 Mine workings _____________________________________ -
The Forming Conditions of Alyaskitovoe Tin-Tungsten Deposit, Russia
0393-000066 The forming conditions of Alyaskitovoe tin-tungsten deposit, Russia Corresponding author: Elena Anikina, IGEM RAS, [email protected] Co-authors: Gennady Gamyanin, IGEM RAS, [email protected] The Alyaskitovoe Sn-W deposit is located at the boundary between the Kular-Nersko terrane and the Verkhoyansk fold-thrust belt. It is localized in the tin-tungsten sublatitudinal metallogenic zone. The deposit area is composed of Upper Triassic sandstone-shale intruded by granite porphyry stock (98 MA Rb-Sr). Stock refers to the formation of young Li-F granites (P2O5 = 0.22- 0.56%, F = 0.12-0.21%, Sr = 9224-688g/t, Li = 47-252g/t, Rb = 61-194g/t). Stock and enclosing hornfels dissected by series of steeply dipping quartz veins meridional strike (L = up to 700 m, M = 0.4-0.6 m). Veins are accompanied by wallrock changes. It is greisenization in granitoids (up to 3 m) and tourmalinization – in hornfels (0.5 m). Several paragenetic associations are identified. Metasomatic: molybdenite-apatite1-tourmaline1- quartz-muscovite, tourmaline2-apatite2-fluorite-arsenopyrite-hydromica. Ore: cassiterite- wolframite-tourmaline-arsenopyrite-quartz, pyrrhotite-stannite-sphalerite-pyrite, molybdenite- matildite-aramayoite-galena-(Bi-andorite) Sb-gustovite, hubnerite-Ag-sulfoantimonite-calcite- quartz. Fluid inclusions (FI) in quartz of greisen and ore veins were studied. Temperature of homogenization of greisen inclusions is 460-480°C. FI contain weakly concentrated solutions (4.9- 3.3 wt.% NaCl-equiv), the gas phase is presented СО2 (29.6-78,2 mol.%), СН4 (11.1-21.8 mol.%). FI in quartz of ore veins contain a liquid phase with concentration 9.2-3.3 wt.% NaCl-equiv and homogenization temperatures of 290-380°С. -
Cassiterite Recovery from a Sulfide Ore Flotation Tailing by Combined Gravity and Flotation Separations
Physicochem. Probl. Miner. Process., 57(1), 2021, 206-215 Physicochemical Problems of Mineral Processing ISSN 1643-1049 http://www.journalssystem.com/ppmp © Wroclaw University of Science and Technology Received August 11, 2020; reviewed; accepted November 29, 2020 Cassiterite recovery from a sulfide ore flotation tailing by combined gravity and flotation separations Limin Zhang, Sultan an Khoso, Mengjie Tian, Wei Sun School of Minerals Processing and Bioengineering, Central South University, Changsha 410083, China Key Laboratory of Hunan Province for Clean and Efficient Utilization of Strategic Calcium-containing Mineral Resources, Central South University, Changsha 410083, China Corresponding author: [email protected] (Mengjie Tian) Abstract: Cassiterite (SnO2), which is the most important Sn-containing mineral, is extensively found in large quantities in discarded tailings. The recovery of cassiterite from discarded sulfide ore flotation tailings can reduce resource wastage and environmental pollution. The gravity separation technique can recover multiple valuable minerals, such as cassiterite, whose densities considerably differ from those of their associated gangue minerals. However, its recovery efficiency rapidly decreases as the mineral particle grain size decreases. To recover the finer valuable mineral particles from gravity separation tailings, flotation separation can be used as a supplementary method. In this study, the gravity and flotation separation techniques are combined to recover cassiterite from a sulfide ore tailing. The Sn grade and recovery of the final concentrate is 31.40% and 88.05%, respectively, thus indicating a highly efficient recovery of cassiterite by using the combined gravity and flotation separation technique. This study can be an important reference for recovering cassiterite from low-Sn-grade tailings. -
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. -
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................................. -
Clarke Jeff a 201709 Mscproj
THE CHARACTERIZATION OF ARSENIC MINERAL PHASES FROM LEGACY MINE WASTE AND SOIL NEAR COBALT, ONTARIO by Jeff Clarke A research project submitted to the Department of Geological Sciences and Geological Engineering In conformity with the requirements for the degree of Master of Science in Applied Geology Queen’s University Kingston, Ontario, Canada (July, 2017) Copyright © Jeff Clarke, 2017 i ABSTRACT The Cobalt-Coleman silver (Ag) mining camp has a long history of mining dating back to 1903. Silver mineralization is hosted within carbonate veins and occurs in association with Fe-Co-Ni arsenide and sulpharsenide mineral species. The complex mineralogy presented challenges to early mineral processing methods with varying success of Ag recovery and a significant amount of arsenic (As) in waste material which was disposed in the numerous tailings deposits scattered throughout the mining camp, and in many instances disposed of uncontained. The oxidation and dissolution of As-bearing mineral phases in these tailings and legacy waste sites releases As into the local aquatic environment. Determining the distribution of primary and secondary As mineral species in different legacy mine waste materials provides an understanding of the stability of As. Few studies have included detailed advanced mineralogical characterization of As mineral species from legacy mine waste in the Cobalt area. As part of this study, a total of 28 samples were collected from tailings, processed material near mill sites and soils from the legacy Nipissing and Cart Lake mining sites. The samples were analyzed for bulk chemistry to delineate material with strongly elevated As returned from all sample sites. This sampling returned highly elevated As with up to 6.01% As from samples near mill sites, 1.71% As from tailings and 0.10% As from soils. -
Heinrich&Candela TOG2 For
Research Collection Book Chapter Fluids and Ore Formation in the Earth's Crust Author(s): Heinrich, Christoph A.; Candela, Philip A. Publication Date: 2014 Permanent Link: https://doi.org/10.3929/ethz-b-000095425 Originally published in: 13, http://doi.org/10.1016/B978-0-08-095975-7.01101-3 Rights / License: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library This is the Green Open Access version of: Heinrich C.A., and Candela P.A. (2014) Fluids and Ore Formation in the Earth's Crust. In: Holland H.D. & Turekian K.K. (eds.) Treatise on Geochemistry, 2nd Edition, vol. 13 (Geochemistry of Mineral Deposits, S. D. Scott, ed.), p. 1-28. Original publication see http://dx.doi.org/10.1016/B978-0-08-095975-7.01101-3 Fluids and Ore Formation in the Earth’s Crust Christoph A. Heinrich1 and Philip A. Candela2 1 ETH Zurich, Department of Earth Sciences, and University of Zurich, Faculty of Mathematics and Natural Sciences, Clausiusstr. 25, 8092 Zurich, Switzerland 2 Laboratory for Mineral Deposits Research, Department of Geology, University of Maryland, College Park, MD,20742, USA Synopsis Ore deposits are rock volumes containing selected elements in sufficient concentration and quantity that they can Be extracted economically. Except for Fe and Al, all technically important metals and other elements are scarce, in total constituting less that 1% of the Earth’s crust. Depending on the element and its mineralogy, a 10- to 10,000-fold enrichment is required for economic extraction today. -
The Genetic Association Between Quartz Vein- and Greisen-Type
minerals Article The Genetic Association between Quartz Vein- and Greisen-Type Mineralization at the Maoping W–Sn Deposit, Southern Jiangxi, China: Insights from Zircon and Cassiterite U–Pb Ages and Cassiterite Trace Element Composition Li-Li Chen, Pei Ni *, Bao-Zhang Dai *, Wen-Sheng Li, Zhe Chi and Jun-Yi Pan State Key Laboratory for Mineral Deposits Research, Institute of Geo–Fluids, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China * Correspondence: [email protected] (P.N.); [email protected] (B.-Z.D.); Tel.: +86-25-8968-0883 (P.N.); +86-25-8368-6649 (B.-Z.D.) Received: 28 May 2019; Accepted: 3 July 2019; Published: 4 July 2019 Abstract: The large-scale Maoping W–Sn deposit in the Gannan metallogenic belt of the eastern Nanling Range, South China, spatially associated with the Maoping granite pluton, hosts total ore reserves of 103,000 t WO3 and 50,000 t Sn. Two different types of mineralization developed in this deposit: Upper quartz vein-type mineralization, mostly within the Cambrian metamorphosed sandstone and slate, and underneath greisen-type mineralization within the Maoping granite. Cassiterites from both types of mineralization coexist with wolframite. Here we report for the first time in situ U–Pb data on cassiterite and zircon of the Maoping deposit obtained by LA-ICP-MS. Cassiterite from quartz vein and greisen yielded weighted average 206Pb/238U ages of 156.8 1.5 Ma ± and 156.9 1.4 Ma, respectively, which indicates that the two types of mineralization formed roughly ± at the same time. In addition, the two mineralization ages are consistent with the emplacement age of the Maoping granite (159.0 1.5 Ma) within error, suggesting a close temporal and genetic link ± between W–Sn mineralization and granitic magmatism. -
Cassiterite Solubility and Tin Speciation in Supercritical Chloride Solutions
Fluid-Mineral Interactions: A Tribute to H. P. Eugster © The Geochemical Society, Special Publication No.2, 1990 Editors: R. J. Spencer and I-Ming Chou Cassiterite solubility and tin speciation in supercritical chloride solutions GLENN A. WILSON* and HANS P. EUGSTERt Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland 21218, U.S.A. Abstract-In order to model the evolution of hydrothermal cassiterite deposits, a quantitative un- derstanding of the chemistry of cassiterite-fluid reactions under supercritical conditions is needed. To obtain this information, the solubility of cassiterite in HCl solutions was measured in closed- system experiments from 400 to 700°C, 1.5 kb, with the oxygen fugacity controlled by nickel-nickel oxide (NNO) and hematite-magnetite (HM). From the measured total chloride and tin concentrations, and the conditions of electrical neutrality at P and T, a set of equations was established for each run. By solving the equations simultaneously and finding the best-fit solution for all runs at the same set of P and T conditions, data were obtained on the identity of the dominant aqueous tin-chloride species and the equilibrium constants for the cassiterite dissolution reaction, X 4-X Sn02 + XH+ + nCl- <=± SnCl;,'-n + '2 H20 + -4- O2, where X is the oxidation state of aqueous tin and n is the ligation number of the tin-chloride species. With the 10, ofNNO at 400 to 600°C, it was found that SnCI+and SnClg are dominant in solution, and at 700°C only SnClg was detected. With the 10, ofHM at 500 and 600°C, SnClj was found to be dominant.