Copper Deposits in Sedimentary and Volcanogenic Rocks
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A Summary of Petroleum Plays and Characteristics of the Michigan Basin
DEPARTMENT OF INTERIOR U.S. GEOLOGICAL SURVEY A summary of petroleum plays and characteristics of the Michigan basin by Ronald R. Charpentier Open-File Report 87-450R This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Denver, Colorado 80225 TABLE OF CONTENTS Page ABSTRACT.................................................. 3 INTRODUCTION.............................................. 3 REGIONAL GEOLOGY.......................................... 3 SOURCE ROCKS.............................................. 6 THERMAL MATURITY.......................................... 11 PETROLEUM PRODUCTION...................................... 11 PLAY DESCRIPTIONS......................................... 18 Mississippian-Pennsylvanian gas play................. 18 Antrim Shale play.................................... 18 Devonian anticlinal play............................. 21 Niagaran reef play................................... 21 Trenton-Black River play............................. 23 Prairie du Chien play................................ 25 Cambrian play........................................ 29 Precambrian rift play................................ 29 REFERENCES................................................ 32 LIST OF FIGURES Figure Page 1. Index map of Michigan basin province (modified from Ells, 1971, reprinted by permission of American Association of Petroleum Geologists)................. 4 2. Structure contour map on top of Precambrian basement, Lower Peninsula -
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. -
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. -
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 -
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. -
Stability of Metallic Copper in the Near Surface Environment
OC ~l CXU ^J'JI. T KJ STATENS KÄRNBRÄNSLE NÄMND NATIONAL BOABD FOR SPENT NUCLEAR FUEL SKN REPORT 57 . Stability of Metallic Copper in the Near Surface Environment MARCH 1992 Where and how will we dispose of spent nuclear fuel? There is political consensus to dispose or spent nuclear fuel from Swedish nuclear power plants in Sweden. No decision has yet been reached on a site for the final repository in Sweden and neither has a method for disposal been determined. The disposal site and method must be selected with regard to safety and the environment as well as with regard to our responsibility to prevent the proliferation of materials which can be used to produce nuclear weapons. In 1983, a disposal method called KBS-3 was presented by the nuclear power utilities, through the Swedish Nuclear Fuel and Waste Management Company (SKB). In its 1984 resolution on permission to load fuel into the Forsmark 3 and Oskarshamn 3 reactors, the government stated that the KBS-3 method - which had been thoroughly reviewed by Swedish and foreign experts - "was, in its entirety and in all essentials, found to be acceptable in terms of safety and radiological protection." In the same resolution, the government also pointed out that a final position on a choice of method would require further research and development work. Who is responsible for the safe management of spent nuclear fuel? The nuclear power utilities have the direct responsibility for the safe handling and disposal of spent nuclear fuel. This decision is based on the following, general argument: those who conduct an activity arc responsible for seeing that the activity is conducted in a safe manner. -
New Data on the Hyrkkola Native Copper Mineralization: a Natural Analogue for the Long-Term Corrosion of Copper Canisters
NEW DATA ON THE HYRKKOLA NATIVE COPPER MINERALIZATION: A NATURAL ANALOGUE FOR THE LONG-TERM CORROSION OF COPPER CANISTERS N. MARCOS’, L. AHONEN’, R. BROS’, P. ROOS4, J. SUKS15 & V. OVERSBY6 ’ Helsinki University of Technology, Engineering Geology & GeoDhvsics Lab. I< .- P.O. Box 6200, FiN-02015 HUT Finknd Geoloeical Survev of Finland (GTK). P.O. Box 96. FIN-02151. Esooo. Finland ’ Envir&mental Geochemistry Laboratory, Department of EnvironmeAtal Safety Research, JAERI, Tokai, Ibaraki, 319-1 1 Japan University of Lund, 22185 Lund, Sweden Laboratory of Radiochemistry, P.O. Box 55 FIN-00014, Helsinki, Finland VMO Konsult, Stockholm, Sweden ABSTRACT The Hyrkkola U-Cu mineralization located in south-western Finland is reassessed with reference to the corrosion mechanisms affecting the stability of native copper and the time-scales of corrosion processes. The mineral assemblage native copper - copper sulfide occurs in open fractures at several depth intervals within granite pegmatites (GP). The surfaces of these open fractures have accumulations of uranophane crystals and other unidentified uranyl compounds. The secondary uranium minerals are mainly distributed around copper sulfide grains. Microscopic intergrowths of copper sulfides and uranyl compounds also have been observed. Groundwater samples were collected from the vicinity of the Cu samples. The hydrogeochemical features of these samples indicate that the present conditions are oxidising. The minimum age of U(V1) transport and deposition is about 200 000 years. This age is indicated by 234U/238Uand 230Th/234Uactivity ratios of uranophane. The age of the hexavalent uranium precipitation may be somewhat later than the last influxes and/or demobilisation of sulfur. The mineral assemblage native copper - copper oxide (cuprite) occurs only at one depth interval within altered granite pegmatite. -
A Fundamental Precambrian–Phanerozoic Shift in Earth's Glacial
Tectonophysics 375 (2003) 353–385 www.elsevier.com/locate/tecto A fundamental Precambrian–Phanerozoic shift in earth’s glacial style? D.A.D. Evans* Department of Geology and Geophysics, Yale University, P.O. Box 208109, 210 Whitney Avenue, New Haven, CT 06520-8109, USA Received 24 May 2002; received in revised form 25 March 2003; accepted 5 June 2003 Abstract It has recently been found that Neoproterozoic glaciogenic sediments were deposited mainly at low paleolatitudes, in marked qualitative contrast to their Pleistocene counterparts. Several competing models vie for explanation of this unusual paleoclimatic record, most notably the high-obliquity hypothesis and varying degrees of the snowball Earth scenario. The present study quantitatively compiles the global distributions of Miocene–Pleistocene glaciogenic deposits and paleomagnetically derived paleolatitudes for Late Devonian–Permian, Ordovician–Silurian, Neoproterozoic, and Paleoproterozoic glaciogenic rocks. Whereas high depositional latitudes dominate all Phanerozoic ice ages, exclusively low paleolatitudes characterize both of the major Precambrian glacial epochs. Transition between these modes occurred within a 100-My interval, precisely coeval with the Neoproterozoic–Cambrian ‘‘explosion’’ of metazoan diversity. Glaciation is much more common since 750 Ma than in the preceding sedimentary record, an observation that cannot be ascribed merely to preservation. These patterns suggest an overall cooling of Earth’s longterm climate, superimposed by developing regulatory feedbacks -
Michigan's Copper Country" Lets You Experience the Require the Efforts of Many People with Different Excitement of the Discovery and Development of the Backgrounds
Michigan’s Copper Country Ellis W. Courter Contribution to Michigan Geology 92 01 Table of Contents Preface .................................................................................................................. 2 The Keweenaw Peninsula ........................................................................................... 3 The Primitive Miners ................................................................................................. 6 Europeans Come to the Copper Country ....................................................................... 12 The Legend of the Ontonagon Copper Boulder ............................................................... 18 The Copper Rush .................................................................................................... 22 The Pioneer Mining Companies................................................................................... 33 The Portage Lake District ......................................................................................... 44 Civil War Times ...................................................................................................... 51 The Beginning of the Calumet and Hecla ...................................................................... 59 Along the Way to Maturity......................................................................................... 68 Down the South Range ............................................................................................. 80 West of the Ontonagon............................................................................................ -
Principles of Geochemical Prospecting
Principles of Geochemical Prospecting GEOLOGICAL SURVEY BULLETIN 1000-F CONTRIBUTIONS TO GEOCHEMICAL PROSPECTING FOR MINERALS PRINCIPLES OF GEOCHEMICAL PROSPECTING By H. E. HAWKES ABSTRACT Geochemical prospecting for minerals includes any method of mineral exploration based on systematic measurement of the chemical properties of a naturally occurring material. The purpose of the measurements is the location of geochemical anomalies or of areas where the chemical pattern indicates the presence of ore in the vicinity. Anomalies may be formed either at depth by igneous and metamorphic processes or at the earth's surface by agents of weathering, erosion, and surficial transportation. Geochemical anomalies of deep-seated origin primary anomalies may result from (1) apparent local variation in the original composition of the earth's crust, defining a distinctive "geochemical province" especially favor able for the occurrence of ore, (2) impregnation of rocks by mineralizing fluids related to ore formation, and (3) dispersion of volatile elements transported in gaseous form. Anomalies of surficial origin-^secondary anomalies take the form either of residual materials from weathering of rocks and ores in place or of material dispersed from the ore deposit by gravity, moving water, or glacial ice. The mobility of an element, or tendency for it to migrate in the.surficial environment, determines the characteristics of the geochemical anomalies it can form. Water is the principal transporting agency for the products of weathering. Mobility is, therefore, closely related to the tendency of an element to be stable in water-soluble form. The chemical factors affecting the mobility of elements include hydrogen-ion concentration, solubility of salts, coprecipitation, sorption, oxidation potential, and the formation of complexes and colloidal solutions. -
OCCASION This Publication Has Been Made Available to the Public on The
OCCASION This publication has been made available to the public on the occasion of the 50th anniversary of the United Nations Industrial Development Organisation. DISCLAIMER This document has been produced without formal United Nations editing. The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations Industrial Development Organization (UNIDO) concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries, or its economic system or degree of development. Designations such as “developed”, “industrialized” and “developing” are intended for statistical convenience and do not necessarily express a judgment about the stage reached by a particular country or area in the development process. Mention of firm names or commercial products does not constitute an endorsement by UNIDO. FAIR USE POLICY Any part of this publication may be quoted and referenced for educational and research purposes without additional permission from UNIDO. However, those who make use of quoting and referencing this publication are requested to follow the Fair Use Policy of giving due credit to UNIDO. CONTACT Please contact [email protected] for further information concerning UNIDO publications. For more information about UNIDO, please visit us at www.unido.org UNITED NATIONS INDUSTRIAL DEVELOPMENT ORGANIZATION Vienna International Centre, P.O. Box 300, 1400 Vienna, Austria Tel: (+43-1) 26026-0 · www.unido.org · [email protected] I \ < Z V ) Distr. l l ' ' v v LIMITED ID/WG.370/10 29 April 19 8 2 United Nations Industrial Development Organization ENGLISH * Workshop on Research, Utilization and Processing of ■> Non-Metallic Minerals vith Special. -
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.