INTRODUCTION to ORE-FORMING PROCESSES ITOA01 09/03/2009 14:30 Page Ii ITOA01 09/03/2009 14:30 Page Iii

Total Page:16

File Type:pdf, Size:1020Kb

INTRODUCTION to ORE-FORMING PROCESSES ITOA01 09/03/2009 14:30 Page Ii ITOA01 09/03/2009 14:30 Page Iii ITOA01 09/03/2009 14:30 Page ii ITOA01 09/03/2009 14:30 Page i INTRODUCTION TO ORE-FORMING PROCESSES ITOA01 09/03/2009 14:30 Page ii ITOA01 09/03/2009 14:30 Page iii Introduction to Ore-Forming Processes LAURENCE ROBB ITOA01 09/03/2009 14:30 Page iv © 2005 by Blackwell Science Ltd a Blackwell Publishing company 350 Main Street, Malden, MA 02148-50120 USA 108 Cowley Road, Oxford OX4 1JF, UK 550 Swanston Street, Carlton, Victoria 3053, Australia The right of Laurence Robb to be identified as the Author of this Work has been asserted in accordance with the UK Copyright, Designs, and Patents Act 1988. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs, and Patents Act 1988, without the prior permission of the publisher. First published 2005 by Blackwell Publishing Library of Congress Cataloging-in-Publication Data Robb, L.J. Introduction to ore-forming processes / Laurence Robb. p. cm. Includes bibliographical references and index. ISBN 0-632-06378-5 (pbk. : alk. paper) 1. Ores. I. Title. QE390.R32 2004 553′.1—dc22 2003014049 A catalogue record for this title is available from the British Library. 1 Set in 9/11–2 pt Trump Mediaeval by Graphicraft Limited, Hong Kong Printed and bound in the United Kingdom by TJ International, Padstow, Cornwall For further information on Blackwell Publishing, visit our website: http://www.blackwellpublishing.com ITOA01 09/03/2009 14:30 Page v Contents Preface vii 2.3 Formation of a magmatic aqueous phase 79 INTRODUCTION: MINERAL RESOURCES 1 2.4 The composition and Introduction and aims 1 characteristics of magmatic- A classification scheme for ore deposits 2 hydrothermal solutions 85 What makes a viable mineral deposit? 4 2.5 A note on pegmatites and their Some useful definitions and compilations 6 significance to granite-related Natural resources, sustainability, and ore-forming processes 93 environmental responsibility 11 2.6 Fluid–melt trace element Summary and further reading 15 partitioning 96 2.7 Water content and depth of PART 1 IGNEOUS PROCESSES emplacement of granites – relationships to ore-forming 1IGNEOUS ORE-FORMING PROCESSES 19 processes 101 1.1 Introduction 19 2.8 Models for the formation of 1.2 Magmas and metallogeny 20 porphyry-type Cu, Mo, and 1.3 Why are some magmas more fertile W deposits 106 than others? The “inheritance 2.9 Fluid flow in and around granite factor” 28 plutons 108 1.4 Partial melting and crystal 2.10 Skarn deposits 113 fractionation as ore-forming 2.11 Near-surface magmatic- processes 37 hydrothermal processes – the 1.5 Liquid immiscibility as an “epithermal” family of ore-forming process 54 Au–Ag–(Cu) deposits 117 1.6 A more detailed consideration 2.12 The role of hydrothermal fluids of mineralization processes in in mineralized mafic rocks 122 mafic magmas 57 Summary and further reading 125 1.7 A model for mineralization in layered mafic intrusions 71 PART 2 HYDROTHERMAL Summary and further reading 74 PROCESSES 2MAGMATIC-HYDROTHERMAL ORE-FORMING PROCESSES 75 3HYDROTHERMAL ORE-FORMING PROCESSES 129 2.1 Introduction 75 3.1 Introduction 129 2.2 Some physical and chemical 3.2 Other fluids in the Earth’s crust properties of water 76 and their origins 130 ITOA01 09/03/2009 14:30 Page vi vi CONTENTS 3.3 The movement of hydrothermal 4.6 Supergene enrichment of Cu fluids in the Earth’s crust 138 and other metals in near surface 3.4 Further factors affecting metal deposits 238 solubility 147 Summary and further reading 245 3.5 Precipitation mechanisms for metals in solution 153 5SEDIMENTARY ORE-FORMING PROCESSES 246 3.6 More on fluid/rock interaction – 5.1 Introduction 246 an introduction to hydrothermal 5.2 Clastic sedimentation and heavy alteration 166 mineral concentration – placer 3.7 Metal zoning and paragenetic deposits 247 sequence 174 5.3 Chemical sedimentation – banded 3.8 Modern analogues of ore-forming iron-formations, phosphorites, processes – the VMS–SEDEX and evaporites 266 continuum 177 5.4 Fossil fuels – oil/gas formation and 3.9 Mineral deposits associated coalification 287 with aqueo-carbonic metamorphic Summary and further reading 307 fluids 189 3.10 Ore deposits associated with connate fluids 197 PART 4 GLOBAL TECTONICS 3.11 Ore deposits associated with AND METALLOGENY near surface meteoric fluids (groundwater) 209 6ORE DEPOSITS IN A GLOBAL TECTONIC CONTEXT 311 Summary and further reading 214 6.1 Introduction 311 6.2 Patterns in the distribution of PART 3 SEDIMENTARY/ mineral deposits 312 SURFICIAL PROCESSES 6.3 Continental growth rates 312 6.4 Crustal evolution and metallogenesis 315 4SURFICIAL AND SUPERGENE ORE-FORMING 6.5 Metallogeny through time 319 PROCESSES 219 6.6 Plate tectonics and ore deposits – 4.1 Introduction 219 a summary 339 4.2 Principles of chemical weathering 220 Summary and further reading 343 4.3 Lateritic deposits 223 4.4 Clay deposits 233 References 345 4.5 Calcrete-hosted deposits 235 Index 368 ITOA01 09/03/2009 14:30 Page vii Preface There are many excellent texts, available at both treat economic geology as a vocational topic and introductory and advanced levels, that describe to provide instruction only to those individuals the Earth’s mineral deposits. Several describe the who wished to specialize in the discipline or to deposits themselves and others do so in com- follow a career in the minerals industries. In more bination with explanations that provide an under- recent years, changes in earth science curricula standing of how such mineral occurrences form. have resulted in a trend, at least in a good many Few are dedicated entirely to the multitude of parts of the world, in which economic geology has processes that give rise to the ore deposits of the been sidelined. A more holistic, process-orientated world. The main purpose of this book is to provide approach (earth systems science) has led to a wider a better understanding of the processes, as well as appreciation of the Earth as a complex interrelated the nature and origin, of mineral occurrences and system. Another aim of this book, therefore, is how they fit into the Earth system. It is intended to emphasize the range of processes responsible for use at a senior undergraduate level (third for the formation of the enormously diverse ore and fourth year levels), or graduate level (North deposit types found on Earth and to integrate America), and assumes a basic knowledge in a these into a description of Earth evolution and wide range of core earth science disciplines, as global tectonics. In so doing it is hoped that well as in chemistry and physics. Although meant metallogenic studies will increasingly be reinte- to be introductory, it is reasonably comprehen- grated into the university earth science curricula. sive in its treatment of topics, and it is hoped that Teaching the processes involved in the formation practicing geologists in the minerals and related of the world’s diminishing resource inventory industries will also find the book useful as a sum- is necessary, not only because of its practical mary and update of ore-forming processes. To this relevance to the real world, but also because such end the text is punctuated by a number of boxed processes form an integral and informative part case studies in which actual ore deposits, selected of the Earth system. as classic examples from around the world, are This book was written mainly while on a briefly described to give context and relevance to protracted sabbatical in the Department of Earth processes being discussed in the main text. Sciences at the University of Oxford. I am very Metallogeny, or the study of the genesis of ore grateful to John Woodhouse and the departmental deposits in relation to the global tectonic paradigm, staff who accommodated me and helped to provide is a topic that traditionally has been, and should the combination of academic rigor and quietitude remain, a core component of the university earth that made writing this book such a pleasure. In science curriculum. It is also the discipline that particular Jenny Colls, Earth Science Librarian, was underpins the training of professional earth scien- a tower of support in locating reference material. tists working in the minerals and related industries The “tea club” at the Banbury Road annexe pro- of the world. A tendency in the past has been to vided both stimulation and the requisite libations ITOA01 09/03/2009 14:30 Page viii viii PREFACE to break the monotony. The staff at Blackwell David Rickard, who undertook the onerous task managed to combine being really nice people with of reviewing the entire manuscript; his lucid a truly professional attitude, and Ian Francis, comments helped to eliminate a number of flaws Delia Sandford, Rosie Hayden, and Cee Pike were and omissions. Financial support for this project all a pleasure to work with. Dave Coles drafted came from BHP Billiton in London and the Geo- all the diagrams and I am extremely grateful for logical Society of South Africa Trust. My col- his forebearance in dealing amiably with a list of leagues at Wits were extremely supportive during figures that seemingly did not end. Several people my long absences, and I am very grateful to Spike took time to read through the manuscript for me McCarthy, Paul Dirks, Carl Anhauesser, Johan and in so doing greatly improved both the style Kruger, and Judith Kinnaird for their input in and content. They include John Taylor (copy- so many ways.
Recommended publications
  • 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
    [Show full text]
  • Thermal Annealing and Phase Transformation of Serpentine-Like Garnierite
    minerals Article Thermal Annealing and Phase Transformation of Serpentine-Like Garnierite Arun Kumar 1,2 , Michele Cassetta 1, Marco Giarola 3, Marco Zanatta 4 , Monique Le Guen 5, Gian Domenico Soraru 6 and Gino Mariotto 1,* 1 Department of Computer Science, University of Verona, 37134 Verona, Italy; [email protected] (A.K.); [email protected] (M.C.) 2 CNR-Institute for Microelectronics and Microsystems, Agrate Brianza, 20864 Agrate, Italy 3 Centro Piattaforme Tecnologiche (CPT), University of Verona, 37134 Verona, Italy; [email protected] 4 Department of Physics, University of Trento, 38123 Povo, Italy; [email protected] 5 Innovation Technology Direction, ERAMET IDEAS, 78190 Trappes, France; [email protected] 6 Department of Industrial Engineering, University of Trento, 38123 Povo, Italy; [email protected] * Correspondence: [email protected] Abstract: This study is focused on the vibrational and microstructural aspects of the thermally induced transformation of serpentine-like garnierite into quartz, forsterite, and enstatite occur- ring at about 620 ◦C. Powder specimens of garnierite were annealed in static air between room temperature and 1000 ◦C. The kinetic of the transformation was investigated by means of thermo- gravimetric and differential thermal analysis, and the final product was extensively characterized via micro-Raman spectroscopy and X-ray diffraction. Our study shows that serpentine-like garnierite consists of a mixture of different mineral species. Furthermore, these garnierites and their compo- sition can provide details based on the mineralogy and the crystalline phases resulting from the thermal treatment. Citation: Kumar, A.; Cassetta, M.; Giarola, M.; Zanatta, M.; Le Guen, M.; Keywords: garnierite; phase transformation; TGA/DSC; XRD; micro-Raman spectroscopy Soraru, G.D.; Mariotto, G.
    [Show full text]
  • DOGAMI MP-20, Investigations of Nickel in Oregon
    0 C\1 a: w a.. <( a.. en ::::> 0 w z <( __j __j w () en � INVESTIGATIONS OF NICKEL IN OREGON STATE OF OREGON DEPARTMENT OF GEOL.OGY AND MINERAL. IN OUSTRIES DONAL.D .A HUL.L. STATE GEOLOGIST 1978 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 State Office Building, Portland, Oregon 97201 MISCELLANEOUS PAPER 20 INVESTIGATIONS OF NICKEL IN OREGON Len Ramp, Resident Geologist Grants Pass Field Office Oregon Department of Geology and Mineral Industries Conducted in conformance with ORS 516.030 . •. 5 1978 GOVERNING BOARD Leeanne MacColl, Chairperson, Portland Talent Robert W. Doty STATE GEOLOGIST John Schwabe Portland Donald A. Hull CONTENTS INTRODUCTION -- - ---- -- -- --- Purpose and Scope of this Report Acknowledgments U.S. Nickel Industry GEOLOGY OF LATERITE DEPOSITS - -- - 3 Previous Work - - - - --- 3 Ultramafic Rocks - ----- --- 3 Composition - - -------- - 3 Distribution ------ - - - 3 Structure - 3 Geochemistry of Nickel ---- 4 Chemical Weathering of Peridotite - - 4 The soi I profile ------- 5 M i nero I ogy -- - ----- 5 Prospecting Guides and Techniques- - 6 OTHER TYPES OF NICKEL DEPOSITS - - 7 Nickel Sulfide Deposits- - - - - - 7 Deposits in Oregon 7 Other areas --- 8 Prospecting techniques 8 Silica-Carbonate Deposits - -- 8 DISTRIBUTION OF LATERITE DEPOSITS - ------ 9 Nickel Mountain Deposits - - ------ --------- 9 Location --------------- --- 9 Geology - ------- ----- 11 Ore deposits ----------- - -- 11 Soil mineralogy - ------- 12 Structure --- ---- ---- 13 Mining and metallurgy ------------ ---- 13 Production-
    [Show full text]
  • BRSUG Number Mineral Name Hey Index Group Hey No
    BRSUG Number Mineral name Hey Index Group Hey No. Chem. Country Locality Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-37 Copper Au) 1.1 4[Cu] U.K., 17 Basset Mines, nr. Redruth, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-151 Copper Au) 1.1 4[Cu] U.K., 17 Phoenix mine, Cheese Wring, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-280 Copper Au) 1.1 4[Cu] U.K., 17 County Bridge Quarry, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and South Caradon Mine, 4 miles N of Liskeard, B-319 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-394 Copper Au) 1.1 4[Cu] U.K., 17 ? Cornwall? Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-395 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-539 Copper Au) 1.1 4[Cu] North America, U.S.A Houghton, Michigan Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-540 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-541 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu,
    [Show full text]
  • USGS Open-File Report 2010-1333 and CGS SR
    Prepared in cooperation with the California Geological Survey; University of Oregon; University of Colorado; University of California, San Diego; and Jet Propulsion Laboratory, California Institute of Technology. Triggered Surface Slips in Southern California Associated with the 2010 El Mayor-Cucapah, Baja California, Mexico, Earthquake SALTON SEA Open-File Report 2010-1333 Jointly published as California Geological Survey Special Report 221 U.S. Department of Interior U.S. Geological Survey COVER Landsat satellite image (LE70390372003084EDC00) showing location of surface slip triggered along faults in the greater Salton Trough area. Red bars show the generalized location of 2010 surface slip along faults in the central Salton Trough and many additional faults in the southwestern section of the Salton Trough. Surface slip in the central Salton Trough shown only where verified in the field; slip in the southwestern section of the Salton Trough shown where verified in the field or inferred from UAVSAR images. Triggered Surface Slips in Southern California Associated with the 2010 El Mayor-Cucapah, Baja California, Mexico, Earthquake By Michael J. Rymer, Jerome A. Treiman, Katherine J. Kendrick, James J. Lienkaemper, Ray J. Weldon, Roger Bilham, Meng Wei, Eric J. Fielding, Janis L. Hernandez, Brian P. E. Olson, Pamela J. Irvine, Nichole Knepprath, Robert R. Sickler, Xiaopeng Tong, and Martin E. Siem Prepared in cooperation with the California Geological Survey; University of Oregon; University of Colorado; University of California, San Diego; and Jet Propulsion Laboratory, California Institute of Technology. Open-File Report 2010–1333 Jointly published as California Geological Survey Special Report 221 U.S. Department of Interior U.S.
    [Show full text]
  • Sonny Bono Salton Sea National Wildlife Refuge Complex
    Appendix J Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex Appendix J: Cultural Setting - Sonny Bono Salton Sea National Wildlife Refuge Complex The following sections describe the cultural setting in and around the two refuges that constitute the Sonny Bono Salton Sea National Wildlife Refuge Complex (NWRC) - Sonny Bono Salton Sea NWR and Coachella Valley NWR. The cultural resources associated with these Refuges may include archaeological and historic sites, buildings, structures, and/or objects. Both the Imperial Valley and the Coachella Valley contain rich archaeological records. Some portions of the Sonny Bono Salton Sea NWRC have previously been inventoried for cultural resources, while substantial additional areas have not yet been examined. Seventy-seven prehistoric and historic sites, features, or isolated finds have been documented on or within a 0.5- mile buffer of the Sonny Bono Salton Sea NWR and Coachella Valley NWR. Cultural History The outline of Colorado Desert culture history largely follows a summary by Jerry Schaefer (2006). It is founded on the pioneering work of Malcolm J. Rogers in many parts of the Colorado and Sonoran deserts (Rogers 1939, Rogers 1945, Rogers 1966). Since then, several overviews and syntheses have been prepared, with each succeeding effort drawing on the previous studies and adding new data and interpretations (Crabtree 1981, Schaefer 1994a, Schaefer and Laylander 2007, Wallace 1962, Warren 1984, Wilke 1976). The information presented here was compiled by ASM Affiliates in 2009 for the Service as part of Cultural Resources Review for the Sonny Bono Salton Sea NWRC. Four successive periods, each with distinctive cultural patterns, may be defined for the prehistoric Colorado Desert, extending back in time over a period of at least 12,000 years.
    [Show full text]
  • GEOPHYSICAL STUDY of the SALTON TROUGH of Soutllern CALIFORNIA
    GEOPHYSICAL STUDY OF THE SALTON TROUGH OF SOUTllERN CALIFORNIA Thesis by Shawn Biehler In Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy California Institute of Technology Pasadena. California 1964 (Su bm i t t ed Ma Y 7, l 964) PLEASE NOTE: Figures are not original copy. 11 These pages tend to "curl • Very small print on several. Filmed in the best possible way. UNIVERSITY MICROFILMS, INC. i i ACKNOWLEDGMENTS The author gratefully acknowledges Frank Press and Clarence R. Allen for their advice and suggestions through­ out this entire study. Robert L. Kovach kindly made avail­ able all of this Qravity and seismic data in the Colorado Delta region. G. P. Woo11ard supplied regional gravity maps of southern California and Arizona. Martin F. Kane made available his terrain correction program. c. w. Jenn­ ings released prel imlnary field maps of the San Bernardino ct11u Ni::eule::> quad1-angles. c. E. Co1-bato supplied information on the gravimeter calibration loop. The oil companies of California supplied helpful infor­ mation on thelr wells and released somA QAnphysical data. The Standard Oil Company of California supplied a grant-In- a l d for the s e i sm i c f i e l d work • I am i ndebt e d to Drs Luc i en La Coste of La Coste and Romberg for supplying the underwater gravimeter, and to Aerial Control, Inc. and Paclf ic Air Industries for the use of their Tellurometers. A.Ibrahim and L. Teng assisted with the seismic field program. am especially indebted to Elaine E.
    [Show full text]
  • Coachella Valley Water Management Plan 2010 Update
    COACHELLA VALLEY WATER MANAGEMENT PLAN 2010 UPDATE Final Report January 2012 Prepared for: Coachella Valley Water District Steve Robbins General Manager-Chief Engineer Patti Reyes Planning and Special Program Manager Prepared by: MWH 618 Michillinda Ave., Suite 200 Arcadia, CA 91007 Water Consult 535 North Garfield Avenue Loveland, CO 80537 Table of Contents Section Name Page Number Executive Summary ................................................................................................................ ES-1 ES-1 The Coachella Valley ...............................................................................................ES-1 ES-2 Water Management in the Coachella Valley ...........................................................ES-3 ES-3 Current Condition of Coachella Valley Groundwater Basin ...................................ES-4 ES-4 The 2002 Water Management Plan..........................................................................ES-5 ES-4.1 Goals and Objectives ......................................................................................ES-5 ES-4.2 Accomplishments Since 2002 .........................................................................ES-6 ES-5 2010 WMP Update ................................................................................................ES-13 ES-5.1 Population and Water Demand .....................................................................ES-13 ES-5.2 Future Water Supply Needs ..........................................................................ES-16 ES-5.3 What
    [Show full text]
  • Characterisation of Ni Silicate-Bearing Minerals by UV-Vis-NIR Spectrscopy
    This may be the author’s version of a work that was submitted/accepted for publication in the following source: Bayyareddy, Jagannadha, Frost, Ray,& Dickfos, Marilla (2009) Characterisation of Ni silicate-bearing minerals by UV-vis-NIR spec- trscopy: Effect of Ni substitution in hydrous Ni-Mg silicates. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy, 71(5), pp. 1762-1768. This file was downloaded from: https://eprints.qut.edu.au/15661/ c Copyright 2009 Elsevier Reproduced in accordance with the copyright policy of the publisher. Notice: Please note that this document may not be the Version of Record (i.e. published version) of the work. Author manuscript versions (as Sub- mitted for peer review or as Accepted for publication after peer review) can be identified by an absence of publisher branding and/or typeset appear- ance. If there is any doubt, please refer to the published source. https://doi.org/10.1016/j.saa.2008.06.030 QUT Digital Repository: http://eprints.qut.edu.au/ Reddy, B. Jagannadha and Frost, Ray L. and Dickfos, Marilla J. (2009) Characterisation of Ni silicate-bearing minerals by UV-Vis-NIR spectroscopy - Effect of Ni substitution in hydrous Ni-Mg silicates . Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 71:pp. 1762-1768. © Copyright 2009 Elsevier 1 2 Characterisation of Ni silicate-bearing minerals by UV-Vis-NIR spectroscopy 3 -Effect of Ni substitution in hydrous Ni-Mg silicates 4 5 B. Jagannadha Reddy, Ray L. Frost •and Marilla J. Dickfos 6 7 Inorganic Materials Research program, School of Physical and Chemical Sciences, 8 Queensland University of Technology, GPO Box 2434, Brisbane Queensland 4001, 9 Australia.
    [Show full text]
  • The Phase Diversity of Nickel Phyllosilicates from New Caledonia: an Investigation Using Transmission Electron Microscopy (TEM) STUDENT: Brittany A
    THE PHASE DIVERSITY OF NICKEL PHYLLOSILICATES FROM NEW CALEDONIA: AN INVESTIGATION USING TRANSMISSION ELECTRON MICROSCOPY (TEM) A THESIS SUBMITTED TO THE GRADUATE SCHOOL IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE MASTER OF SCIENCE BY BRITTANY CYMES DR. KIRSTEN NICHOLSON – ADVISOR BALL STATE UNIVERSITY MUNCIE, INDIANA MAY 2016 ABSTRACT THESIS: The Phase Diversity of Nickel Phyllosilicates from New Caledonia: An Investigation Using Transmission Electron Microscopy (TEM) STUDENT: Brittany A. Cymes DEGREE: Master of Science COLLEGE: Sciences and Humanities DATE: May, 2016 PAGES: 136 New Caledonia is a French territorial island in the Southwest Pacific with an economy heavily dependent upon nickel-mining, being the 5th largest producer worldwide. The nickel deposits result from tropical lateritic weathering of ophiolite units that were emplaced during the late Eocene. The ultramafic units weathered and continue to weather into bright green Ni-rich phyllosilicates colloquially referred to as „garnierite‟. Detailed investigations of „garnierite‟ using transmission electron microscopy (TEM) have been carried out in other locations to characterize important nanoscale features; however, none have been undertaken in New Caledonia. In this investigation, ten samples of „garnierite‟ from New Caledonia were examined with powder X-ray diffraction (XRD) and TEM with energy dispersive spectrometry (EDS). The XRD results show the phyllosilicate material to be comprised of highly disordered talc- and serpentine-like minerals with minor chlorite indicated by significantly broad reflections and two- i dimensional diffraction bands, consistent with published data. TEM analysis, however, revealed new information. Talc-like minerals occur as fluffy aggregates of crystals with lattices with approximately 10 Å d-spacing and significant crystallographic disorder and also as aggregates of larger crystals with more orderly lattices; these two varieties represent the kerolite-pimelite series and the talc- willemseite series, respectively.
    [Show full text]
  • Talc- and Serpentine-Like “Garnierites” from Falcondo Ni
    macla nº 15 . septiembre 2011 revista de la sociedad española de mineralogía 197 Talc- and Serpentine-like “Garnierites” from Falcondo Ni-laterite Deposit (Dominican Republic): a HRTEM approach / CRISTINA VILLANOVA-DE-BENAVENT (1,*), FERNANDO NIETO (2), JOAQUÍN A. PROENZA (1), SALVADOR GALÍ (1) (1) Departament de Cristal·lografia, Mineralogia i Dipòsits Minerals. Facultat de Geologia. Universitat de Barcelona. C/ Martí i Franquès s/n. 08028 Barcelona, Catalunya (España) (2) Departamento de Mineralogía y Petrología e Instituto Andaluz de Ciencias de la Tierra. Universidad de Granada-CSIC. Campus de • Fuerteventura s/n. 18002 Granada (España) INTRODUCTION. from Falcondo Ni-laterite deposit. These “garnierites” mainly occur as mm-cm results are compared to those previously vein fillings in fractures, but also as “Garnierites” represent significant Ni ore obtained through powder XRD and EMP coatings, boxworks and different kinds minerals in the lower horizons of many (CCiT, Universitat de Barcelona). of breccias, within the saprolite horizon Ni-laterite deposits worldwide (e.g. or near the unweathered peridotite, Freyssinet et al., 2005). They consist of Preliminary data allows to classify the close to the base of the lateritic profile. a green, fine-grained mixture of hydrous sampled “garnierites” into two groups, Ni-bearing magnesium phyllosilicates, which display two well distinguishable METHODOLOGY. including serpentine, talc, sepiolite, greenish colours in hand specimen: smectite and chlorite (e.g. Brindley and A representative sample, containing Hang, 1973; Springer, 1974; Brindley et • Bluish bright-green “garnierites” strongly serpentinized peridotite al., 1979). Thus, “garnierite” is a general display colloform textures under the (saprolite) cross-cut by talc-like and descriptive term and is not recognized optical microscope.
    [Show full text]
  • The Journal of R
    The Journal of r Volumemmoie 28 Noemmoi. emmoi2 Apriol 200 2 o Notes from the Laboratory Chocolate- brown Opal Inclutsfbns in Gemstones Natural Amethyst hi1 (iemmoiotiuMl Asstvi.it inn .nij C iem Tcstiiv* I .ahoivitoi'v oi Crrot Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London ECIN 8TN Tel: 020 7404 3334 Fax: 020 7404 8843 e-mail: [email protected] Website: www.gagtl.ac.uk President: Professor AT. Collins Vice-Presidents: N. W. Deeks, AE. Farn, RA Howie, D.G. Kent, RK. Mitchell Honorary Fellows: Chen Zhonghui, RA Howie, RT. Liddicoat [nr, K. Nassau Honorary Life Members: H. Bank, D.J. Callaghan, E.A [obbins, H. Tillander Council of Management: T.J. Davidson, RR Harding, 1. Mercer, J. Monnickendam, M.I. O'Donoghue, E. Stern, 1. Thomson, v.P. Watson Members' Council: AJ. Allnutt, S. Burgoyne, P. Dwyer-Hickey, S.A. Everitt, J. Greatwood, B. Jackson, L. Music, J.B. Nelson, P.G. Read, P.J. Wates, C.H. Winter Branch Chairmen: Midlands - G.M. Green, North West - D. M. Brady, Scottish - B. Jackson, South West - RM. Slater Examiners: AJ. Allnutt, M.Sc., PhD., FGA, L. Bartlett, B.5c., M.Phil., FGA, DGA, S. Coelho, B.5c., FGA, DGA, Prof. AT. Collins, B.Sc., Ph.D, A.G. Good, FGA, DGA, I. Greatwood, FGA, G.M. Howe, FGA, DGA, S. Hue Williams MA, FGA, DGA, B. Jackson, FGA, DGA, G.B. Jones, B.5c., Ph.D., FGA, Li Li Ping, FGA, DGA, M. Newton, B.Sc.,D.Phil., c.I.E. Oldershaw, B.Sc.
    [Show full text]