A Technique for Measuring the Dielectric Properties of Minerals at Microwave Heating Frequencies Using an Open-Ended Coaxial Line

Total Page:16

File Type:pdf, Size:1020Kb

A Technique for Measuring the Dielectric Properties of Minerals at Microwave Heating Frequencies Using an Open-Ended Coaxial Line REPORT OF INVESTIGATIONS/1994 I PLEASE DO NOT REMOVE FRCM LIBRARY UBRARY SPOKANE RESEARCH CENTER RECttVED 4 U6 BUREAU OF MNES E. 315 AVE. SPOKANE, WA 86247 A Technique for ~easuringthe Dielectric Properties of Minerals at Microwave Heating Frequencies Using an Open-Ended Coaxial Line By J. B. Salsman and S. P. Holderfield U.S. Department of the Interior Mission Statement As the Nation's principal conservation agency, the Department of the Interior has responsibility for most of our nationally-owned public lands and natural resources. This includes fostering sound use of our land and water resources; protecting our fish, wildlife, and biological diversity; preserving the environmental and cultural valucs of our national parks and historical places; and providing for the enjoyment of life through outdoor recreation. The Department assesses our energy and mineral resources and works to ensure that their development is in the best interests of all our people by encouraging stewardship and citizen participa- tion in their care. The Department also has a major responsibility for American Indian reservation communities and for people who live in island territories under U.S. administration. Report of Investigatians 9519 A Technique for Measuring the Dielectric Properties of Minerals at Microwave Heating Frequencies Using an Open-Ended Coaxial Line By J. B. Salsman and S. P. Holderfield UNITED STATES DEPARTMENT OF THE INTERIOR Bruce Babbitt, Secretary BUREAU OF MINES This report is based on work done under an agreement between the University of Alabama and the U.S. Bureau of Mines. Internation$ Standard Sei-ial Number ISSN 1066-5552 CONTENTS Page Abstract ........................................................................... Introduction ....................................................................... Measurement of the dielectric properties of minerals .......................................... Thotyofmeaswement ............................................................. Determination~fC~andC,.......................................................... Selection of reference materials for determining capacitances .................................. Determination of density effects ....................................................... Mathematical relationships ........................................................... Equipment ......................................................................... Coaxialline ...................................................................... Networkanalyzer .................................................................. Heatingdevice .................................................................... Densitycharnber .................................................................. Experimentalprocedure ............................................................... Samplepreparation ............................................................... Calibration of network analyzer ....................................................... Dielectric property measurements ...................................................... Results ............................................................................ Conclusions ........................................................................ Referenws. ........................................................................ Appen&.-Abbreviations and symbols used in this report ...................................... ILLUSTRATIONS Equivalent circuit of a sample at the end of a coaxial lime ................................... Cross section of a typical coaxial line .................................................. End of the coaxial line where the spacer was placed ....................................... Cohal line constructed for this measurement method ..................................... Impedance standards constructed for calibration of test equipment ............................ Nettvork analyzer in Smith chart diplay mode ........................................... Heaters used in the measurement system to heat mineral samples to temperatures of 325 "C ......... Insulating box used to house the heating apparatus and mineral samples to alleviate sample oxidation dwhgtheheathgcycle ........................................................... Holding apparatus constructed for measuring dielectric properties of minerals as a function of temperature and density .......................................................... Density variation apparatus ......................................................... Complete measurement system ...................................................... Dielectric constant of chalcopyrite at diferent frequencies and temperatures ..................... Loss factor of chalcopyrite at different frequencies and temperatures ........................... Dielectric constant of chalcocite at different frequencies and temperatures ....................... Loss factor of chdcocite at different frequencies and temperatures ............................ Dielectric constant of chalcocite at different temperatures for two discrete frequencies .............. Loss factor of chalcocite tit different temperatures for two discrete frequencies ................... Dielectric constant of cobaltite at different temperatures and frequencies ........................ Loss factor of cobaltite at different temperatures and frequencies ............................. Dielectric constant of chalcopyrite .................................................... Loss factor of chalcopyrite .......................................................... 1. Comparison of dielectric constant and loss factor of measured and calculated data for a 0.2-N saline solution ....................................................................... mm millimeter GHz gigahertz pet percent pm micrometer g/cins gram per cubic cecenheter kHz kilohertz "6 degree Celsius MHz megahertz Reference to specific products does not imply endorsement by the US. Bureau of Mines, A TECHNIQUE FOR MmSURtNG THE DIELECTRIC PR8PEfa"TIES OF MINERALS AT MICROWAVE HMTING FREQUENCIES USING AN OPENWENDEDCOAXIAL LIME By J. 8. ~alsman'and S. P. ~oldertield~ ABSTRACT As part of the research effort on investigating the effects of microwave energy on the chernieal and physical properties of minerals and ores, the U,S, Bureau of Mines (USBM) Tuscaloosa Research Center has conducted research to measure the dielectric properties of these materials, The objective was to establish a reliable database for use in predicting the effects of microwave heahg on a wide rmp of minerals. The dielectric constants and loss factors of minerals, commonly referred to as the dielectric prop- erties, were determined utilizing the theory of microwave propagation through an open-endedl, ;air-filled line that was terminated at its open end with the particular mineral under investigation. Zo this phase of microwave research, the USBM measured the dielectric properties of powdered min- erals with medium to high electrical conductivities in the frequency range of 300 MHz to 3 GHz and as a function of temperature from 25 to 325 "C. Since the minerals were prepared as powders, tech- niques were used to relate the measured dielectric properties of the powdered minerals to the dielectric propertim of the mineral at its theoretical or natural density, "&&at enajneer, Tusrxrloosa Researeh Center, U.S. Bureau of Mines, Tuscaiochsa, AL (naw with Salt Lake Gity Research Center, U.S. Bureau af Mines, Salt Lake City, UJJUT), 'mernlca~enajneer, Tuscal- Research Center. INTRODUCTION Major research efforts are underway worldwide on the data is that until the recent development of advanced elec- use of microwave energy in various processing techniques. tronic equipment such as the network analyzer, it was Deterrents to these research efforts are the lack of suf- very difficult to develop successful measuring systems in ficient data on the electrical properties of materials (in- this frequency range. This range is too high for radio- cluding minerals), and the lack of personnel trained in frequency techniques and is at the low-frequency end of microwave heating technology. It is very likely that micro- the microwave spectrum. However, it is this frequency wave energy may offer many advantages to minerals bene- range that is of interest, for it includes the frequencies ficiation and processing techniques; however, it is difficult allocated by the Federal Communications Commission for to exploit these advantages without an understanding of use in industrial, scientific, medical, and domestic appli- the electrical properties of minerals. As part of its mission cations (915 MHz, 2.45 GHz, and 22 GHz); the widely to advance research in processing techniques, the U.S. used microwave heating frequencies are 915 MHz and Bureau of Mines (USBM) is studying the use of micro- 2.45 GHz. wave energy. Microwave technology is beginning to find many suc- The electrical properties of a mineral are those prop- cessful uses in industrial applications other than food prep- erties that characterize how that mineral is affected by aration or communications. Recent investigations of the an electric field, and these properties may, and often do, use of microwave energy as a heat source in materials- change with frequency. The electrical properties of min- processing techniques have shown several advantages over erals are also temperature dependent. At the microwave conventional methods of heating. For example, studies heating frequencies of 300 MHz to
Recommended publications
  • Abstract in PDF Format
    PGM Associations in Copper-Rich Sulphide Ore of the Oktyabr Deposit, Talnakh Deposit Group, Russia Olga A. Yakovleva1, Sergey M. Kozyrev1 and Oleg I. Oleshkevich2 1Institute Gipronickel JS, St. Petersburg, Russia 2Mining and Metallurgical Company “Noril’sk Nickel” JS, Noril’sk, Russia e-mail: [email protected] The PGM assemblages of the Cu-rich 6%; the Ni content ranges 0.8 to 1.3%, and the ratio sulphide ores occurring in the western exocontact Cu/S = 0.1-0.2. zone of the Talnakh intrusion and the Kharaelakh Pyrrhotite-chalcopyrite ore occurs at the massive orebody have been studied. Eleven ore top of ore horizons. The ore-mineral content ranges samples, weighing 20 to 200 kg, were processed 50 to 60%, and pyrrhotite amount is <15%. The ore using gravity and flotation-gravity techniques. As a grades 1.1 to 1.3% Ni, and the ratio Cu/S = 0.35- result, the gravity concentrates were obtained from 0.7. the ores and flotation products. In the gravity Chalcopyrite ore occurs at the top and on concentrates, more than 20,000 PGM grains were the flanks of the orebodies. The concentration of found and identified, using light microscopy and sulphides ranges 50 to 60%, and pyrrhotite amount EPMA. The textural and chemical characteristics of is <1%; the Ni content ranges 1.3 to 3.4%, and the PGM were documented, as well as the PGM ratio Cu/S = 0.8-0.9. distribution in different size fractions. Also, the The ore types are distinctly distinguished balance of Pt, Pd and Au distribution in ores and by the PGE content which directly depends on the process products and the PGM mass portions in chalcopyrite quantity, but not on the total sulphide various ore types were calculated.
    [Show full text]
  • LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, and COBALT ARSENIDE and SULFIDE ORE FORMATION Nicholas Allin
    Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2019 EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION Nicholas Allin Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geotechnical Engineering Commons EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION by Nicholas C. Allin A thesis submitted in partial fulfillment of the requirements for the degree of Masters in Geoscience: Geology Option Montana Technological University 2019 ii Abstract Experiments were conducted to determine the relative rates of reduction of aqueous sulfate and aqueous arsenite (As(OH)3,aq) using foils of copper, nickel, or cobalt as the reductant, at temperatures of 150ºC to 300ºC. At the highest temperature of 300°C, very limited sulfate reduction was observed with cobalt foil, but sulfate was reduced to sulfide by copper foil (precipitation of Cu2S (chalcocite)) and partly reduced by nickel foil (precipitation of NiS2 (vaesite) + NiSO4·xH2O). In the 300ºC arsenite reduction experiments, Cu3As (domeykite), Ni5As2, or CoAs (langisite) formed. In experiments where both sulfate and arsenite were present, some produced minerals were sulfarsenides, which contained both sulfide and arsenide, i.e. cobaltite (CoAsS). These experiments also produced large (~10 µm along longest axis) euhedral crystals of metal-sulfide that were either imbedded or grown upon a matrix of fine-grained metal-arsenides, or, in the case of cobalt, metal-sulfarsenide. Some experimental results did not show clear mineral formation, but instead demonstrated metal-arsenic alloying at the foil edges.
    [Show full text]
  • Key to Rocks & Minerals Collections
    STATE OF MICHIGAN MINERALS DEPARTMENT OF NATURAL RESOURCES GEOLOGICAL SURVEY DIVISION A mineral is a rock substance occurring in nature that has a definite chemical composition, crystal form, and KEY TO ROCKS & MINERALS COLLECTIONS other distinct physical properties. A few of the minerals, such as gold and silver, occur as "free" elements, but by most minerals are chemical combinations of two or Harry O. Sorensen several elements just as plants and animals are Reprinted 1968 chemical combinations. Nearly all of the 90 or more Lansing, Michigan known elements are found in the earth's crust, but only 8 are present in proportions greater than one percent. In order of abundance the 8 most important elements Contents are: INTRODUCTION............................................................... 1 Percent composition Element Symbol MINERALS........................................................................ 1 of the earth’s crust ROCKS ............................................................................. 1 Oxygen O 46.46 IGNEOUS ROCKS ........................................................ 2 Silicon Si 27.61 SEDIMENTARY ROCKS............................................... 2 Aluminum Al 8.07 METAMORPHIC ROCKS.............................................. 2 Iron Fe 5.06 IDENTIFICATION ............................................................. 2 Calcium Ca 3.64 COLOR AND STREAK.................................................. 2 Sodium Na 2.75 LUSTER......................................................................... 2 Potassium
    [Show full text]
  • Gomposition and Occurrence of Electrum Atthe
    L37 The Canadian M inerala g i st Vol.33,pp. 137-151(1995) GOMPOSITIONAND OCCURRENCEOF ELECTRUM ATTHE MORNINGSTAR DEPOSIT, SAN BERNARDINOCOUNTY, GALIFORNIA: EVIDENCEFOR REMOBILIZATION OF GOLD AND SILVER RONALD WYNN SIIEETS*, JAMES R. CRAIG em ROBERT J. BODNAR Depanmen of Geolngical Sciences, Virginin Polytechnic h stitate and Stale (Jniversity, 4A44 Dening Hall, Blacl<sburg, Virginin 24060, U.S-A,. Arsrnacr Elecfum, acanthiteand uytenbogaardtite have been examined from six depthswithin the tabular quartzt calcite sockwork and breccia-filled veins in the fault-zone-hostedMorning Star depositof the northeasternMojave Desert, Califomia. Six distinct types of electrum have been identified on the basis of minerat association,grain moryhology and composition. Two types, (1) p1'rite-hostedand (2) quartz-hostedelectrum, occur with acanthite after argentite and base-metalsulfide minerals in unoxidized portions of the orebody; the remaining forr types, (3) goethite-hostedelectrum, (4) electnrm cores, (5) electrumrims and (6) wire electrum,are associatedwith assemblagesof supergeneminerals in its oxidizedportions. Pyrite- hosted quartz-hostedand goethite-hostedelectrum range in compositionfrom 6l ta 75 utt.7oAu and have uniform textures and no zoning. In lower portions ofthe oxidized ore zone, electrum seemsto replacegoethite and occursas small grains on surfacesof the goethite.Textural evidencefavors supergeneremobilization of Au and Ag, which were depositedas electrum on or replacinggoethite. This type of electrumis identical in appearanceand compositionto prinary electrum,In the upper portions of the oxidized zone,secondary electum occursas a gold-rich rim on a core of elechum and as wire-like grains,both with acanthiteand uytenbogaardtite.Such secondaryelectrum contains from 78 to 93 wt./o Au. Textural relations and asso- ciated minerals suggestthat the primary electrum was hydrothermally depositedand partially remobilized by supergene processes.
    [Show full text]
  • Oxidation of Sulfide Minerals. V. Galena, Sphalerite and Chalcogite
    Canadian Mineralogist Vol. 18,pp. 365-372(1980) OXIDATIONOF SULFIDEMINERALS. V. GALENA,SPHALERITE AND CHALCOGITE H.F. STEGBR eup L.E. DESJARDINS Mineral SciencesLaboratories, Canada Centre lor Mineral and Energy Technology, Department ol Energy, Mines and Resources,Ottawa, Ontaio KIA OGI AssrRecr long-term stability of sulfide-bearing ores and concentrates.Part of this study was concerned Samples of galena, sphalerite and cbalcocite were with the nature of the products and kinetics of oxidized at 52oC and, 68Vo of relative humidity the oxidation of the commonly encountered periods to five weeks, and the prqd- in air for up sulfide minerals. The oxidation of pyrite, chal- for metal and sulfur-bearing ucts were analyzed pyrrhotite at 52oC and, 687o of. species. Galena is. oxidized to PbSOa, sphalerite copyrite and (RH) has already been in- to ZnSO. * FezO, if iron-bearing, and chalcocite relative humidity to CuO and CuS. The oxidation of galena and vestigated (Steger & Desjardins 1978). This re- sphalerite proceeds according to a linear rate potr summarizes the results of the study 9f tle law: that of chalcocite leads to the formation of a bxidation of galena, sphalerite and chalcocite coherent product layer impenetrable to Oz and HrO under the same conditions. vapor. The air oxidation of galena at relatively low without Keywords: air oxidation, oxidation products, sul- temperatures has been investigated fide minerals, galena, sphalerite, chalcocite. reaching a consensuson the nature of the oxida- tion product. Hagihara (1952), using a re- Sourvrlrnp flection electron-diffraction technique, and Kirkwood & Nutting (1965), using a trans- Nous avons 6tudi6 I'oxydation dans I'air d'6chan- mission electron-diffraction technique, found tillons de galdne, de sphal6rite et de chalcocite i this product to be PbSOo,whereas Leia et al.
    [Show full text]
  • Copper Deposits in Sedimentary and Volcanogenic Rocks
    Copper Deposits in Sedimentary and Volcanogenic Rocks GEOLOGICAL SURVEY PROFESSIONAL PAPER 907-C COVER PHOTOGRAPHS 1 . Asbestos ore 8. Aluminum ore, bauxite, Georgia 1 2 3 4 2. Lead ore. Balmat mine, N . Y. 9. Native copper ore, Keweenawan 5 6 3. Chromite-chromium ore, Washington Peninsula, Mich. 4. Zinc ore, Friedensville, Pa. 10. Porphyry molybdenum ore, Colorado 7 8 5. Banded iron-formation, Palmer, 11. Zinc ore, Edwards, N.Y. Mich. 12. Manganese nodules, ocean floor 9 10 6. Ribbon asbestos ore, Quebec, Canada 13. Botryoidal fluorite ore, 11 12 13 14 7. Manganese ore, banded Poncha Springs, Colo. rhodochrosite 14. Tungsten ore, North Carolina Copper Deposits in Sedimentary and Volcanogenic Rocks By ELIZABETH B. TOURTELOT and JAMES D. VINE GEOLOGY AND RESOURCES OF COPPER DEPOSITS GEOLOGICAL SURVEY PROFESSIONAL PAPER 907-C A geologic appraisal of low-temperature copper deposits formed by syngenetic, diagenetic, and epigenetic processes UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director First printing 1976 Second printing 1976 Library of Congress Cataloging in Publication Data Tourtelot, Elizabeth B. Copper deposits in sedimentary and volcanogenic rocks. (Geology and resources of copper) (Geological Survey Professional Paper 907-C) Bibliography: p. Supt. of Docs. no.: I 19.16:907-C 1. Copper ores. 2. Rocks, Sedimentary. 3. Rocks, Igneous. I. Vine, James David, 1921- joint author. II. Title. III. Series. IV. Series: United States Geological Survey Professional Paper 907-C. TN440.T68 553'.43 76-608039 For sale by the Superintendent of Documents, U.S.
    [Show full text]
  • 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.
    [Show full text]
  • Sediment-Hosted Copper Deposits of the World: Deposit Models and Database
    Sediment-Hosted Copper Deposits of the World: Deposit Models and Database By Dennis P. Cox1, David A. Lindsey2 Donald A. Singer1, Barry C. Moring1, and Michael F. Diggles1 Including: Descriptive Model of Sediment-Hosted Cu 30b.1 by Dennis P. Cox1 Grade and Tonnage Model of Sediment-Hosted Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Reduced-Facies Cu 30b.2 By Dennis P. Cox1 Grade and Tonnage Model of Reduced Facies Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Redbed Cu 30b.3, by David A. Lindsey2 and Dennis P. Cox1 Grade and Tonnage Model of Redbed Cu by Dennis P. Cox1 and Donald A. Singer1 Descriptive Model of Revett Cu 30b.4, by Dennis P. Cox1 Grade and Tonnage Model of Revett Cu by Dennis P. Cox1 and Donald A. Singer1 Open-File Report 03-107 Version 1.3 2003, revised 2007 Available online at http://pubs.usgs.gov/of/2003/of03-107/ Any use of trade, product or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY 1 345 Middlefield Road, Menlo Park, CA 94025 2 Box 25046, Denver Federal Center, Denver, CO 80225 Introduction This publication contains four descriptive models and four grade-tonnage models for sediment hosted copper deposits. Descriptive models are useful in exploration planning and resource assessment because they enable the user to identify deposits in the field and to identify areas on geologic and geophysical maps where deposits could occur.
    [Show full text]
  • Analysis of the Oxidation of Chalcopyrite,Chalcocite, Galena
    PLEASE 00 Nor REMOVE FRCM LIBRARY Bureau of Mines Report of Investigations/1987 Analysis of the Oxidation of Chalcopyrite, Chalcocite, Galena, Pyrrhotite, Marcasite, and Arsenopyrite By G. W. Reimers and K. E. Hjelmstad UBRARY ""OKANERESEARC H CENTER .... RECEIVED OCT 021 1981 US BUREAU Of MINES t 315 MONTGOMBlY ",'IE. SPOICANl,. WI>. 99201 UNITED STATES DEPARTMENT OF THE INTERIOR Report of Investigations 9118 Analysis of the Oxidation of Chalcopyrite, Chalcocite, Galena!' Pyrrhotite, Marcasite, and Arsenopyrite By G. W. Reimers and K. E. Hjelmstad UNITED STATES DEPARTMENT OF THE INTERIOR Donald Paul Hodel, Secretary BUREAU OF MINES David S. Brown, Acting Director Library of Congress Cataloging in Publication Data : Reimers, G. W. (George W.) Analysis of the oxidation of chalcopyrite, chalcocite, galena, pyr­ rhotite, marcasite, and arsenopyrite. (Bureau of Mines report of investigations; 9118) Bibliography: p. 16 . Supt. of Docs. no.: 128.23: 9118. 1. Pyrites. 2. Oxidation. I. Hjelmstad, Kenneth E. II . Title. III. Series: Reportofinvestiga­ tions (United States. Bureau of Mines) ; 9118. TN23.U43 [QE389.2] 622 s [622'.8] 87-600136 CONTENTS Abst 1 Introduction ••••••••• 2 Equipment and test • .,.,.,.,.,.,., .•. .,., ..... .,.,.,.,., ... ., . ., ........ ., .... ., ..... ., .. ., . .,. 3 Samp Ie ., .. ., ., ., ., ., ., ., ., ., ., ., .. ., .• ., .. ., ..... ., •.••• ., . ., ., ..•. ., ., ., . ., ., ., ., • ., ., ., ., • 4 Results and discussion .. ., . .,.,.,. ........ .,., ...... ., ., .... " . ., . .,.,., . .,., . .,., ,.,.., ., . .,
    [Show full text]
  • Chalcocite Cu2s C 2001-2005 Mineral Data Publishing, Version 1
    Chalcocite Cu2S c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudo-orthorhombic. Point Group: 2/m or m. Crystals are short prismatic [001], thick to tabular {001}, to 12 cm across, and prismatic [100], to 25 cm long; {001} is striated k [100]. Massive, compact, fine powdery. Twinning: Common on {110} yielding pseudohexagonal stellate forms; also on {032}, {112}. Seen as lamellar twinning in polished section. Physical Properties: Cleavage: Indistinct on {110}. Fracture: Conchoidal. Tenacity: Brittle, somewhat sectile. Hardness = 2.5–3 VHN = 84–87 (100 g load). D(meas.) = 5.5–5.8 D(calc.) = 5.80 Optical Properties: Opaque. Color: Blackish lead-gray. Streak: Blackish lead-gray. Luster: Metallic. Anisotropism: Weak. R1–R2: (400) 37.0–36.8, (420) 37.8–37.4, (440) 37.7–37.6, (460) 37.0–37.2, (480) 36.2–36.2, (500) 35.6–35.4, (520) 34.7–34.4, (540) 33.7–33.5, (560) 32.5–32.5, (580) 32.1–31.8, (600) 31.3–31.2, (620) 30.8–30.7, (640) 30.0–30.0, (660) 29.5–30.0, (680) 29.2–29.7, (700) 29.0–29.6 ◦ Cell Data: Space Group: P 21/c or Pc. a = 11.82 b = 27.05 c = 13.43 β =90 Z=96 X-ray Powder Pattern: Bristol, Connecticut, USA (close to djurleite). 1.8800 (100), 2.4030 (70), 1.9746 (70), 1.8811 (70), 2.4074 (50), 3.276 (35), 2.7256 (35) Chemistry: (1) (2) (3) Cu 79.67 79.50 79.86 Fe 0.14 0.17 S 20.16 20.05 20.14 SiO2 0.09 0.17 Total 100.06 99.89 100.00 (1) Butte, Montana, USA; Fe present as pyrite.
    [Show full text]
  • Chalcocite Several Centimeters Wide Were Found (Butler and Burbank, 1929)
    Veinlets of solid chalcocite several centimeters wide were found (Butler and Burbank, 1929). 2. CHALCOCITE Isle Royale mine: In fissures with “ankerite” and Cu2S “specularite.” Lane (1911) reports veins of Widespread, but historically not significant as an chalcocite, bornite, chalcopyrite, “whitneyite,” ore mineral in Michigan, except at the White Pine pyrrhotite(?), natrolite, analcime, and “adularia.” 3. deposit; in fissure veins cutting various rocks of Centennial mine: Disseminated in the Calumet and the native copper lodes and locally disseminated in Hecla Conglomerate. 4. Champion mine: In the lodes themselves; also present in a variety of veinlets with silver. Some as very fine-grained metalliferous veins. Twelve chalcocite deposits pulverulent material consisting of hexagonal have been located on the Keweenaw Peninsula, the platelets less than 0.5 mm across (Koenig, 1902). most notable being the Mount Bohemia and 5. Portage mine: In fissure veins with quartz and Gratiot Lake deposits (Robertson, 1975; Maki, orange calcite. 6. Wolverine mine. 7. Osceola 1999). Maki (1999) estimates the Gratiot Lake mine: As complex microcrystals and crusts on deposit may contain as much as 4.5 million metric prehnite from the No. 10 shaft (Falster, 1978). 8. tons of ore with an average grade of 2.3% copper. East slope Six Mile Hill, southwest of Houghton: Northern Peninsula. Networks of veins with copper, calcite, epidote, prehnite, datolite, and a considerable amount of chalcocite (Rominger, 1895). 9. Laurium mine: (Morris, 1983). Iron County: Sherwood and Buck iron mines: With other sulfides and uraninite (Vickers, 1956b; James et al., 1968). Figure 54: Chalcocite crystals from the White Pine mine, White Pine, Ontonagon County.
    [Show full text]
  • Some Copper Sulphide Parageneses from the Raipas Formation of Northern Norway by F
    Some copper sulphide parageneses from the Raipas formation of Northern Norway BY F. M. VOKES With 3 plates and 8 text-figures. Contents: Page Page Abstract 74 Copper paragenesis 81 Introduction 75 The Ulveryggen deposit 81 Raipas formation — general geo Gråde of deposit 82 logy 77 The ore 82 Repparfjord window — general Minoralogy 84 geology 77 Paragenesis 95 Copper sulphide deposits in the Temperatures 96 Repparfjord window 78 Chemistry 96 Pyritic paragenesis 78 Raipas mine, Alta 96 Bratthammer mine 79 Other deposits 104 The Porsa mines 79 Summary and conclusions 105 Abstract. The Precambrian Raipas formation of Northern Norway contains copper deposits showing two distinct parageneses. The first is a type common in the Scandinavian Precambrian and Caledonian ores, i. e. chalcopyrite-pyrite-pyrrhotite (the «pyritic paragenesis»). The other is much less common and consists of the association bornite-chalcopyrite-neodigenite-(chalcocite). This is termed the «copper paragenesis». The mineralogies of deposits showing both these paragenetical types from Raipas areas in Vest-Finnmark are described, with the greatest emphasis on two deposits showing the «copper paragenesis». Especial attention is given to the question of the origin of the CII2S mineral. It is concluded that this is mainly neodigenite and most probably of hypogene origin, an important point when 75 Fig. 1. Map showing the outcrops of the Raipas formation in Finnmark and the locations of the mines mentioned in the text. Geology after Holtedahl and Dons, 1953. Kart som viser kjente områder med Raipas-formasjon i Finnmark og beliggenheten av gruvene som nevnes i teksten. Geologien er tatt fra Holtedahls og Dons kart, 1953.
    [Show full text]