Geology, Mineralogy, Geochemistry, and Geothermometry of Kelley
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Hydrothermal and Metamorphic Berthierine
n27 CanadianMineralogist Vol. 30,pp. 1127-1142 (1992) HYDROTHERMALAND METAMORPHICBERTHIERINE FROM THE KIDD CREEK VOLCANOGENICMASSTVE SULFIDE DEPOSIT. TIMMINS, ONTARIO JOHNF.SLACK U.S.Geological Survey, Nationnl Center, Mail Stop954, Reston, Virginia 22092, U.S.A. WEI-TEH JIANG ANDDONALD R. PEACOR Depamnent of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, U.S.A. PATRICKM. OKITA* U.S.Geological Survey, National Center,Mail Stop954, Reston,Virginia 22092,U.S.A. ABSTRACT Berthierine,a 7 A pe-Al memberof the serpentinegroup, occursin the footwall stringerzone of the ArcheanKidd Creek massivesulfide deposit, Ontario, associated with quartz,muscovite, chlorite, pyrite, sphalerite,chalcopyrite, and local tourmaline' cassiterite,and halloysite. Berthierine has been identified by the lack of 14A basalreflections on X-ray powderdiffractionpattems, by its composition (electron-microprobedata), and by transmissionelectron microscopy (TEM). Peoogaphic and scanning eiectronmicroscopic (SEM) studiesreveal different types of berthierineocculrences, including interlayerswithin and rims on deformedchlorite, intergrowthswith muscoviteand halloysite,and discretecoarse grains. TEM imagesshow thick packetsof berthierineand chlorite that are parallel or relatedby low-angle boundaries,and layer terminationsof chlorite by berthierine; mixedJayer chlorite-berthierinealso is observed,intergrown with Fe-rich chlorite and berthierine.End-member (Mg-free) berthierineis presentin small domainsin two samples.The Kidd Creekberthierine is chemicallysimilar -
A Pictorial Summary of the Life and Work of George Patrick Leonard Walker
A pictorial summary of the life and work of George Patrick Leonard Walker SCOTT K. ROWLAND1* & R. S. J. SPARKS2 1Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East–West Road, Honolulu, Hawaii, USA 2Department of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK *Corresponding author (e-mail: [email protected]) Abstract: George Patrick Leonard Walker was one of the fathers of modern volcanology. He worked in many parts of the world and contributed to the understanding of a huge range of volca- nological processes. He was a field geologist at heart, and one of his greatest skills was the ability to quantify volcanological ideas – not with obscure statistical treatments or complex numerical models, but with clear graphical relationships supported by tremendous amounts of carefully col- lected field data. Here we present some glimpses of his life and work in photographs and diagrams. George Walker was born on 2 March 1926 in Iceland, as well as to India, Italy, the Azores and London. In 1939, when he was 13, the family Africa, among other locations. In 1978 George moved to Northern Ireland. In 1948 and 1949, moved to the University of Auckland and in 1982 respectively, George received his Bachelors and he moved to the University of Hawaii. Over the Masters degrees from Queen’s University, Belfast. span of his career he visited almost every volcanic In 1956 he completed his PhD at the University of region in the world, including Australia, the Azores, Leeds with a dissertation on secondary minerals in the Canary Islands, Chile, China, Costa Rica, igneous rocks of Northern Iceland. -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
7Th MID-EUROPEAN CLAY CONFERENCE 2014
MECC14 7th MID-EUROPEAN CLAY CONFERENCE 2014 16–19 SEPTEMBER 2014 • DRESDEN • GERMANY www.mecc2014.de PROGRAMME AND ABSTRACTBOOK ©: fotolia.com/Erik Schuhmann Particle Size Analysis down to the Nanometer Range NEW: Laser Diffraction Analyzer HORIBA LA-960 The new HORIBA LA-960 quickly and accurately measures fine particles starting from 10 nm. An outstanding feature is its high flexibility which applies to both measuring range and sample feeding. The LA-960 offers the possibility to use different dispersing media: typically water or alcohol but also non- polar organic solvents. BENEFITS n Extremely wide measurement range from 10 nm to 5 mm n Wet and dry measurements possible n Analysis according to the Mie Scattering Theory (scattering and diffraction) n Analysis cycles: < 1 minute (from sample to sample) n Efficient circulation system incl. ultrasonic probe n Change of measuring cells in seconds www.retsch-technology.com Particle Characterization with Dynamic Image Analysis and Laser Scattering RETSCH TECHNOLOGY provides innovative optical measurement systems for particle characterization with Dynamic Image Analysis or Laser Diffraction. The instruments cover a measuring range from 0.3 nm to 30 mm and are suitable for the characterization of powders, granules, bulk materials, suspensions, emulsions and colloidal systems. CAMSIZER P4 CAMSIZER XT LA-960 LA-300 SZ-100 Dynamic Image Analysis Dynamic Image Analysis Laser Diffraction Laser Diffraction Photon Correlation 20 µm - 30 mm 1 µm - 3 mm 10 nm - 5 mm 0.1 µm - 600 µm Spectroscopy www.retsch.com/camsizerp4 www.retsch.com/camsizerxt www.retsch.com/la960 www.retsch.com/la300 0.3 nm - 8 µm www.retsch.com/sz100 Retsch Technology GmbH | Haan | Germany | Phone +49 2104 2333-300 | E-Mail: [email protected] WWW.RETSCH-TECHNOLOGY.COM Retsch Tech-Advert-GB-LA960-148x210-140522.indd 1 26.05.2014 10:58:33 Table of Contents Organisation and Imprint ..................................................................................................... -
Alkalic-Type Epithermal Gold Deposit Model
Alkalic-Type Epithermal Gold Deposit Model Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. Department of the Interior U.S. Geological Survey Cover. Photographs of alkalic-type epithermal gold deposits and ores. Upper left: Cripple Creek, Colorado—One of the largest alkalic-type epithermal gold deposits in the world showing the Cresson open pit looking southwest. Note the green funnel-shaped area along the pit wall is lamprophyre of the Cresson Pipe, a common alkaline rock type in these deposits. The Cresson Pipe was mined by historic underground methods and produced some of the richest ores in the district. The holes that are visible along several benches in the pit (bottom portion of photograph) are historic underground mine levels. (Photograph by Karen Kelley, USGS, April, 2002). Upper right: High-grade gold ore from the Porgera deposit in Papua New Guinea showing native gold intergrown with gold-silver telluride minerals (silvery) and pyrite. (Photograph by Jeremy Richards, University of Alberta, Canada, 2013, used with permission). Lower left: Mayflower Mine, Montana—High-grade hessite, petzite, benleonardite, and coloradoite in limestone. (Photograph by Paul Spry, Iowa State University, 1995, used with permission). Lower right: View of north rim of Navilawa Caldera, which hosts the Banana Creek prospect, Fiji, from the portal of the Tuvatu prospect. (Photograph by Paul Spry, Iowa State University, 2007, used with permission). Alkalic-Type Epithermal Gold Deposit Model By Karen D. Kelley, Paul G. Spry, Virginia T. McLemore, David L. Fey, and Eric D. Anderson Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. -
Mars Field Geology, Biology, and Paleontology Workshop, Summary
MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston, Houston, Texas LPI Contribution No. 968 MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston Edited by Nancy Ann Budden Lunar and Planetary Institute Sponsored by Lunar and Planetary Institute National Aeronautics and Space Administration Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 968 Compiled in 1999 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautcis and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This volume may be cited as Budden N. A., ed. (1999) Mars Field Geology, Biology, and Paleontology Workshop: Summary and Recommendations. LPI Contribution No. 968, Lunar and Planetary Institute, Houston. 80 pp. This volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling. _________________ Cover: Mars test suit subject and field geologist Dean Eppler overlooking Meteor Crater, Arizona, in Mark III Mars EVA suit. PREFACE In November 1998 the Lunar and Planetary Institute, under the sponsorship of the NASA/HEDS (Human Exploration and Development of Space) Enterprise, held a workshop to explore the objectives, desired capabilities, and operational requirements for the first human exploration of Mars. -
Educators Guide
EDUCATORS GUIDE 02 | Supervolcanoes Volcanism is one of the most creative and destructive processes on our planet. It can build huge mountain ranges, create islands rising from the ocean, and produce some of the most fertile soil on the planet. It can also destroy forests, obliterate buildings, and cause mass extinctions on a global scale. To understand volcanoes one must first understand the theory of plate tectonics. Plate tectonics, while generally accepted by the geologic community, is a relatively new theory devised in the late 1960’s. Plate tectonics and seafloor spreading are what geologists use to interpret the features and movements of Earth’s surface. According to plate tectonics, Earth’s surface, or crust, is made up of a patchwork of about a dozen large plates and many smaller plates that move relative to one another at speeds ranging from less than one to ten centimeters per year. These plates can move away from each other, collide into each other, slide past each other, or even be forced beneath each other. These “subduction zones” are generally where the most earthquakes and volcanoes occur. Yellowstone Magma Plume (left) and Toba Eruption (cover page) from Supervolcanoes. 01 | Supervolcanoes National Next Generation Science Standards Content Standards - Middle School Content Standards - High School MS-ESS2-a. Use plate tectonic models to support the HS-ESS2-a explanation that, due to convection, matter Use Earth system models to support cycles between Earth’s surface and deep explanations of how Earth’s internal and mantle. surface processes operate concurrently at different spatial and temporal scales to MS-ESS2-e form landscapes and seafloor features. -
GSA TODAY December Vol
Vol. 5, No. 12 December 1995 INSIDE • New Members, Fellows, Student Associates, p. 247 GSA TODAY South-Central Section Meeting, p. 250 • A Publication of the Geological Society of America • Northeastern Section Meeting, p. 253 Seismic Images of the A B Core-Mantle Boundary Michael E. Wysession, Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130 C D ABSTRACT INTRODUCTION Seismology presents several ways While most geologists, including of providing images of the geologic specialists in the field of seismology, structures that exist in the lowermost study rocks at Earth’s surface, more mantle just above the core-mantle attention also is being paid to the boundary (CMB). An understanding planet’s other major boundary, that of the possibly complex geophysical between the core and mantle. With a E F processes occurring at this major density jump of 4.3 kg/m3 between discontinuity requires the combined the silicate lower mantle and the liquid efforts of many fields, but it is the iron outer core, as well as a tempera- role of seismology to geographically ture increase of possibly 1500 °C map out this largely uncharted terri- between the lower mantle adiabat and tory. Seismic phases that reflect, outer core, the core-mantle boundary diffract, and refract across the CMB (CMB) may well be Earth’s most signifi- can all be used to provide different cant and dramatic discontinuity. Our Figure 1. Images from a motion picture showing the propagation of seismic shear energy information in different ways. increasing knowledge of this highly through the mantle (Wysession and Shore, 1994). -
Carlin-Type Gold Deposits in Nevada: Critical Geologic Characteristics and Viable Models
©2005 Society of Economic Geologists, Inc. Economic Geology 100th Anniversary Volume pp. 451–484 Carlin-Type Gold Deposits in Nevada: Critical Geologic Characteristics and Viable Models JEAN S. CLINE,† University of Nevada, Las Vegas, 4505 Maryland Parkway, Box 454010, Las Vegas, Nevada 89154-4010 ALBERT H. HOFSTRA, Mineral Resources Program, U.S. Geological Survey, Mail Stop 973, Box 25046, Denver, Colorado 80225 JOHN L. MUNTEAN, Nevada Bureau of Mines and Geology, Mail Stop 178, University of Nevada, Reno, Nevada 89557-0088 RICHARD M. TOSDAL, AND KENNETH A. HICKEY Mineral Deposit Research Unit, University of British Columbia, 6339 Stores Road, Vancouver, British Columbia, Canada V6T 1Z4 Abstract Carlin-type Au deposits in Nevada have huge Au endowments that have made the state, and the United States, one of the leading Au producers in the world. Forty years of mining and numerous studies have pro- vided a detailed geologic picture of the deposits, yet a comprehensive and widely accepted genetic model re- mains elusive. The genesis of the deposits has been difficult to determine owing to difficulties in identifying and analyzing the fine-grained, volumetrically minor, and common ore and gangue minerals, and because of postore weathering and oxidation. In addition, other approximately contemporaneous precious metal deposits have overprinted, or are overprinted by, Carlin-type mineralization. Recent geochronological studies have led to a consensus that the Nevada deposits formed ~42 to 36 m.y. ago, and the deposits can now be evaluated in the context of their tectonic setting. Continental rifting and deposi- tion of a passive margin sequence followed by compressional orogenies established a premineral architecture of steeply dipping fluid conduits, shallow, low dipping “traps” and reactive calcareous host rocks. -
Sharon R. Allen Is a Physical Volcanologist Who Has Worked On
Sharon R. Allen is a physical volcanologist who Timothy H. Druitt is a volcanologist who works has worked on the processes and products of felsic on the processes and products of explosive volca effusive and explosive volcanism in both subaerial nism. His approaches include the field study of and submarine environments from a range of tec volcanic products, laboratory analogue experi tonic settings. She has been researching the South ments, and the petrology and chemistry of magmas. Aegean volcanic arc since 1993, first as a PhD He has used Santorini Volcano (Greece) as a natural student at Monash University (Australia), later as a laboratory for identifying fundamental questions postdoc at the University of Tasmania (UTAS) (Australia), and currently related to volcanism and for testing hypotheses. He obtained his PhD as a university associate at UTAS. Her scientific interests include subae at the University of Cambridge (UK) and is currently Professor of rial caldera forming eruptions, the dynamics of pyroclastic currents Volcanology at ClermontAuvergne University (France). He was Editor on land and when interacting with water, submarine pyroclastic erup inChief of the Bulletin of Volcanology for four years and received the tions and mechanisms for the formation of pumice in submarine set 2018 Norman L. Bowen Award of the American Geophysical Union. tings. Her approach includes field studies of volcanic products and laboratory analogue experimentation. Lorella Francalanci is a geochemist and volcano logist who investigates active volcanoes to reveal Olivier Bachmann is a professor of volcanology the preeruptive processes that are relevant to the and magmatic petrology at the Eidgenössische dynamics of volcanic eruptions. -
Italian Type Minerals / Marco E
THE AUTHORS This book describes one by one all the 264 mi- neral species first discovered in Italy, from 1546 Marco E. Ciriotti was born in Calosso (Asti) in 1945. up to the end of 2008. Moreover, 28 minerals He is an amateur mineralogist-crystallographer, a discovered elsewhere and named after Italian “grouper”, and a systematic collector. He gradua- individuals and institutions are included in a pa- ted in Natural Sciences but pursued his career in the rallel section. Both chapters are alphabetically industrial business until 2000 when, being General TALIAN YPE INERALS I T M arranged. The two catalogues are preceded by Manager, he retired. Then time had come to finally devote himself to his a short presentation which includes some bits of main interest and passion: mineral collecting and information about how the volume is organized related studies. He was the promoter and is now the and subdivided, besides providing some other President of the AMI (Italian Micromineralogical As- more general news. For each mineral all basic sociation), Associate Editor of Micro (the AMI maga- data (chemical formula, space group symmetry, zine), and fellow of many organizations and mine- type locality, general appearance of the species, ralogical associations. He is the author of papers on main geologic occurrences, curiosities, referen- topological, structural and general mineralogy, and of a mineral classification. He was awarded the “Mi- ces, etc.) are included in a full page, together cromounters’ Hall of Fame” 2008 prize. Etymology, with one or more high quality colour photogra- geoanthropology, music, and modern ballet are his phs from both private and museum collections, other keen interests. -
New Mineral Names*
American Mineralogist, Volume 77, pages II16-1 121, 1992 NEW MINERAL NAMES* JonN L. J,lrvrnon CANMET, 555 Booth Street,Ottawa, Ontario KlA 0G1, Canada Jacrr Pvztnwtcz Institute of Geological Sciences,University of Wroclaw, Cybulskiego30, 50-205 Wroclaw, Poland Camerolaite* wt0/0, corresponding to Na, ,u(ZnoroMnOo,o)ro ro - .4.03HrO, H. Sarp, P. Perroud (1991) (Ti38sNb0 07Fe' 04),3 e6Si8 08Or8 ideally Nau- Camerolaite,CuoAlr- . [HSbO.,SO4](OH),0(CO3). 2HrO, a new mineral from ZnTioSirO,, 4H,O. The mineral contains0.18-0.22 wto/o Cap Garonne mine, Var, France.Neues Jahrb. Mineral. F. Occurs as fan-shaped intergrowths of long prismatic Mon.,481-486. crystals,elongate [001], flattened [100], up to 7 mm long and 0.1 mm thick. Transparent, white to colorless,some Electron microprobe (ave. of eight) and CHN analyses grains with a silver tint; vitreous luster, elastic, crushes (for CO, and HrO) gaveCuO 40.56,AlrO3 14.54,SbrO5 into thin fibers along the elongation; uneven, splintery 13.55,SO3 4.75, CO2 6.26,F{2O 20.00, sum 99.66wto/o, fracture, white streak, yellow-green luminescencein the correspondingto Cu.,6,4,1, jeSo Co O,n ide- eesb' ol eeHrs 5, oo, electronmicroprobe beam, hardness 517-571 (ave.544) ally CuoAlr[HSbO4,SO4XOH),0(CO3).2HrO.Occurs as kglmm2 with a 20-g load (Mohs 5.5-6), no cleavage,{010} tufts and radiating aggregates(0.5-2 mm) of transparent, parting. D-"u" : 2.90, D"ut": 2.95 g/cm3 with Z : 2. blue-greenacicular crystalsup to 0.5 mm long and show- Colorlessin transmitted light, nonpleochroic, straight ex- ing {100} and {001}, flattenedon {100}, elongate[010].