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  • Geochemistry  (54)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Malden, MA [u.a.] : Blackwell Science
    Call number: 10/M 04.0217
    Description / Table of Contents: Part I: Introduction. - Part II: Environmental Chemist's Toolbox. - Part III: The Atmosphere. - Part IV: The Chemistry Of Continental Solids. - Part V: The Chemistry Of Continental Waters. - Part VI: The Oceans. - Part VII: Global Change
    Type of Medium: Monograph available for loan
    Pages: xxi, 296 S.
    Edition: 2nd ed.
    ISBN: 0632059052
    Classification:
    Geochemistry
    Location: Upper compact magazine
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  • 2
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 04.0253
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Until only a few years ago, I would never have imagined that a volume on the stable isotope geochemistry of elements like Mg, Fe or Cu would be written. In fact, a comic book of blank pages entitled The Stable Isotope Geochemistry of Fluorine would have been a more likely prospect. In volume 16 of this series, published in 1986, I wrote: Isotopic variations have been looked for but not found for heavy elements like Cu, Sn, and Fe .... Natural variations in isotopic ratios of terrestrial materials have been reported for other light elements like Mg and K, but such variations usually turn out to be laboratory artifacts. I am about ready to eat those words. We have known for many years that large isotopic fractionations of heavy elements like Pb develop in the source regions of TIMS machines. Nonetheless, most of us held fast to the conventional wisdom that no significant mass-dependent isotopic fractionations were likely to occur in natural or laboratory systems for elements that are either heavy or engaged in bonds with a dominant ionic character. With the relatively recent appearance of new instrumentation like MC-ICP-MS and heroic methods development in TIMS analyses, it became possible to make very precise measurements of the isotopic ratios of some of these non-traditional elements, particularly if they comprise three or more isotopes. It was eminently reasonable to reexamine these systems in this new light. Perhaps atomic weights could be refined, or maybe there were some unexpected isotopic variations to discover. There were around the turn of the present century, reports began appearing of biological fractionations of about 2-3 per mil for heavy elements like Fe and Cr and attempts were made to determine the magnitude of equilibrium isotope effects in these systems, both by experiment and semi-empirical calculations. Interest emerged in applying these effects to the study of environmental problems. Even the most recalcitrant skeptic now accepts the fact that measurable and meaningful variations in the isotopic ratios of heavy elements occur as a result of chemical, biological and physical processes. Most of the work discussed in this volume was published after the year 2000 and thus the chapters are more like progress reports rather than reviews. Skepticism now focuses on whether isotopic variations as small as 0.1 per mil are indeed as meaningful as some think, and the fact that measured isotopic fractionations of these non-traditional elements are frequently much smaller than predicted from theoretical considerations. In fact the large fractionations suggested by the calculations provide much of the stimulus for working in this discipline. Clearly some carefully designed experiments could shed light on some of the ambiguity. My optimism for the future of this burgeoning new field remains high because it is in very good hands indeed. Approximately three-quarters of the elements in the Periodic Table have two or more isotopes. RiM 16 and RiMG 43 were devoted to H, C, 0, and S isotope variations, and B isotope variations were discussed in RiM 33. The importance of these elements to geochemistry may be illustrated by a GeoRef search of 0 isotope publications, which yields over 25,000 papers, theses, and abstracts spanning over five decades. Isotopic variations of the remaining 56 elements that have two or more isotopes, however, remains relatively little explored, but is gaining rapid attention, in part driven by advances in analytical instrumentation in the last 5-10 years. Our goal for this volume was to bring together a summary of the isotope geochemistry of non-traditional stable isotope systems as is known through 2003 for those elements that have been studied in some detail, and which have a variety of geochemical properties. In addition, recognizing that many of these elements are of interest to workers who are outside the traditional stable isotope fields, we felt it was important to include discussions on the broad isotopic variations that occur in the solar system, theoretical approaches to calculating isotopic fractionations, and the variety of analytical methods that are in use. We hope, therefore, that this volume proves to be useful to not only the isotope specialist, but to others who are interested in the contributions that these non-traditional stable isotopes may make toward understanding geochemical and biological cycles.
    Type of Medium: Monograph available for loan
    Pages: XV, 454 S. , Ill., graph. Darst
    ISBN: 0-939950-67-7 , 978-0-939950-67-6
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 55
    Classification:
    Geochemistry
    Note: Chapter 1. Overview and General Concepts by Clark M. Johnson, Brian L. Beard and Francis Albarede, p. 1 - 24 Chapter 2. An Overview of Isotopic Anomalies in Extraterrestrial Materials and Their Nucleosynthetic Heritage by Jean Louis Birck, p. 25 - 64 Chapter 3. Applying Stable Isotope Fractionation Theory to New Systems by Edwin A. Schauble, p. 65 - 112 Chapter 4. Analytical Methods for Non-Traditional Isotopes by Francis AlbarÀde and Brian L. Beard, p. 113 - 152 Chapter 5. Developments in the Understanding and Application of Lithium Isotopes in the Earth and Planetary Sciences by Paul B. Tomascak, p. 153 - 196 Chapter 6. The Isotope Geochemistry and Cosmochemistry of Magnesium by Edward D. Young and Albert Galy, p. 197 - 230 Chapter 7. The Stable-Chlorine Isotope Compositions of Natural and Anthropogenic Materials by Michael A. Stewart and Arthur J. Spivack, p. 231 - 254 Chapter 8. Calcium Isotopic Variations Produced by Biological, Kinetic, Radiogenic and Nucleosynthetic Processes by Donald J. DePaolo, p. 255 - 288 Chapter 9. Mass-Dependent Fractionation of Selenium and Chromium Isotopes in Low-Temperature Environments by by Thomas M. Johnson and Thomas D. Bullen, p. 289 - 318 Chapter 10A. Fe Isotope Variations in the Modern and Ancient Earth and Other Planetary Bodies by Brian L. Beard and Clark M. Johnson, p. 319 - 358 Chapter 10B. Isotopic Constraints on Biogeochemical Cycling of Fe by Clark M. Johnson, Brian L. Beard, Eric E. Roden, Dianne K. Newman and Kenneth H. Nealson, p. 359 - 408 Chapter 11. The stable isotope geochemistry of copper and zinc by Francis Albarede, p. 409 - 428 Chapter 12. Molybdenum Stable Isotopes: Observations, Interpretations and Directions by Ariel D. Anbar, p. 429 - 454
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  • 3
    Monograph available for loan
    Monograph available for loan
    Pacific Grove, Calif. : Thomson-Brooks/Cole
    Call number: 10/M 04.0241
    Type of Medium: Monograph available for loan
    Pages: xiii, 514 S.
    ISBN: 0122290615
    Classification:
    Geochemistry
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  • 4
    Call number: 17/M 05.0250/1-5
    Pages: Vol. 1-5
    ISBN: 0471988472
    Classification:
    Geochemistry
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  • 5
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Call number: M 01.0275 ; M 02.0279 ; PIK N 454-99-0015 ; AWI G6-01-0087
    Type of Medium: Monograph available for loan
    Pages: xxix, 872 S.
    Edition: 1. ed., 2nd impr.
    ISBN: 044450155X
    Classification:
    Geochemistry
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: A 18 - must be ordered
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 10/N 01.0413 ; AWI G2-19-51789
    Type of Medium: Monograph available for loan
    Pages: XX, 455 Seiten , Illustrationen
    ISBN: 354066453X
    Classification:
    Geochemistry
    Language: English
    Note: Table of Contents: 1 The Solid Phase of Marine Sediments / DIETER K. FÜTTERER 1.1 Introduction 1.2 Sources and Components of Marine Sediments 1.2.1 Lithogenous Sediments 1.2.2 Biogenous Sediments 1.2.3 Hydrogenous Sediments 1.3 Classification of Marine Sediments 1.3.1 Terrigenous Sediments 1.3.2 Deep-Sea Sediments 1.4 Global Patterns of Sediment Distribution 1.4.1 Distribution Patterns of Shelf Sediments 1.4.2 Distribution Patterns of Deep-Sea Sediments 1.4.3 Distribution Patterns of Glay Minerals 1.4.4 Sedimentation Rates 2 Geophysical Perspectives in Marine Sediments 2.1 Physical Properties of Marine Sediments / MONIKA BREITZKE 2.1.1 Introduction 2.1.2 Porosity and Wet Bulk Density 2.1.2.1 Analysis by Weight and Volume 2.1.2.2 Gamma Ray Attenuation 2.1.2.3 Electrical Resistivity (Galvanic Method) 2.1.2.4 Electrical Resistivity (Inductive Method) 2.1.3 Permeability 2.1.4 Acoustic and Elastic Properties 2.1.4.1 Biot-Stoll Model 2.1.4.2 Full Waveform Ultrasonic Gore Logging 2.1.5 Sediment Classification 2.1.5.1 Full Waveform Gore Logs as Acoustic Images 2.1.5.2 P-and S-Wave Velocity, Attenuation, Elastic Moduli and Permeability 2.1.6 Sediment Echosounding 2.1.6.1 Synthetic Seismograms 2.1.6.2 Narrow-Beam Parasound Echosounder Recordings 2.2 Sedimentary Magnetism / ULRICH BLEIL 2.2.1 Introduction 2.2.2 Biogenie Magnetic Minerals in Marine Sediments 2.2.3 Reduction Diagenesis of Magnetic Minerals in Marine Environments 3 Quantification of Early Diagenesis: Dissolved Constituents in Marine Pore Water / HORST D. SCHULZ 3.1 Introduction: How to Read Pore Water Concentration Profiles 3.2 Calculation of Diffusive Fluxes and Diagenetic Reaction Rates 3.2.1 Steady State and Non-Steady State Situations 3.2.2 The Steady State Situation and Fick's First Law of Diffusion 3.2.3 Quantitative Evaluation of Steady State Concentration Profiles 3.2.4 The Non-Steady State Situation and Fick's Second Law of Diffusion 3.2.5 The Primary Redox-Reactions: Degradation of Organic Matter 3.3 Sampling of Pore Water for Ex-Situ Measurements 3.3.1 Obtaining Sampies of Sediment for the Analysis of Pore Water 3.3.2 Pore Water Extraction from the Sediment 3.3.3 Storage, Transport and Preservation of Pore Water 3.4 Analyzing Constituents in Pore Water, Typical Profiles 3.5 In-Situ Measurements 3.6 Influence of Bioturbation, Bioirrigation, and Advection 4 Organic Matter: The Driving Force for Early Diagenesis / JÜRGEN RULLKÖTTER 4.1 The Organic Carbon Cycle 4.2 Organic Matter Accumulation in Sediments 4.2.1 Productivity Versus Preservation 4.2.2 Primary Production of Organic Matter and Export to the Ocean Bottom 4.2.3 Transport of Organic Matter through the Water Column 4.2.4 The Influence of Sedimentation Rate on Organic Matter Burial 4.2.5 Allochthonous Organic Matter in Marine Sediments 4.3 Early Diagenesis 4.3.1 The Organic Carbon Content of Marine Sediments 4.3.2 Chemical Composition of Biomass 4.3.3 The Principle of Selective Preservation 4.3.4 The Formation of Fossil Organic Matter and its Bulk Composition 4.3.5 Early Diagenesis at the Molecular Level 4.3.6 Biological Markers (Molecular Fossils) 4.4 Organic Geochemical Proxies 4.4.1 Total Organic Carbon and Sulfur 4.4.2 Marine Versus Terrigenous Organic Matter 4.4.3 Molecular Paleo-Seawater Temperature and Climate Indicators 4.5 Analytical Techniques 4.5.1 Sam pie Requirements 4.5.2 Elemental and Bulk Isotope Analysis 4.5.3 Rock-Eval Pyrolysis and Pyrolysis Gas Chromatography 4.5.4 Organic Petrography 4.5.5 Bitumen Analysis 4.6 The Future of Marine Geochemistry of Organic Matter 5 Bacteria and Marine Biogeochemistry / Bo BARKER JORGENSEN 5.1 Role of Microorganisms 5.1.1 From Geochemistry to Microbiology - and back 5.1.2 Approaches in Marine Biogeochemistry 5.2 Life and Environments at Small Scale 5.2.1 Hydrodynamics of Low Reynolds Numbers 5.2.2 Diffusion at Small Scale 5.2.3 Diffusive Boundary Layers 5.3 Regulation and Limits of Microbial Processes 5.3.1 Substrate Uptake by Microorganisms 5.3.2 Temperature as a Regulating Factor 5.3.3 Other Regulating Factors 5.4 Energy Metabolism of Prokaryotes 5.4.1 Free Energy 5.4.2 Reduction-Oxidation Processes 5.4.3 Relations to Oxygen 5.4.4 Definitions of Energy Metabolism 5.4.5 Energy Metabolism of Microorganisms 5.4.6 Chemolithotrophs 5.4.7 Respiration and Fermentation 5.5 Pathways of Organic Matter Degradation 5.5.1 Depolymerization of Macromolecules 5.5.2 Aerobic and Anaerobic Mineralization 5.5.3 Depth Zonation of Oxidants 5.6 Methods in Biogeochemistry 5.6.1 Incubation Experiments 5.6.2 Radioactive Tracers 5.6.3 Example: Sulfate Reduction 5.6.4 Specific Inhibitors 5.6.5 Other Methods 6 Early Diagenesis at the Benthic Boundary Layer: Oxygen and Nitrate in Marine Sediments / CHRISTIAN HENSEN AND MATTHIAS ZABEL 6.1 Introduction 6.2 Oxygen and Nitrate Distribution in Seawater 6.3 The Role of Oxygen and Nitrate in Marine Sediments 6.3.1 Respiration and Redox Processes 6.3.1.1 Nitrification and Denitrification 6.3.1.2 Coupling of Oxygen and Nitrate to other Redox Pathways 6.3.2 Determination of Consumption Rates and Senthic Fluxes 6.3.2.1 Fluxes and Concentration Profiles Determined by In-Situ Devices 6.3.2.2 Ex-Situ Pore Water Data from Deep-Sea Sediments 6.3.2.3 Determination of Denitrification Rates 6.3.3 Oxic Respiration, Nitrification and Denitrification in Different Marine Environments 6.3.3.1 Quantification of Rates and Fluxes 6.3.3.2 Variation in Different Marine Environments: Case Studies 6.4 Summary 7 The Reactivity of Iron / RALF R. HAESE 7.1 Introduction 7.2 Pathways of Iron Input to Marine Sediments 7.2.1 Fluvial Input 7.2.2 Aeolian Input 7.3 Iron as a Limiting Nutrient for Primary Productivity 7.4 The Early Diagenesis of Iron in Sediments 7.4.1 Dissimilatary Iran Reductian 7.4.2 Solid Phase Ferric Iron and its Bioavailability 7.4.2.1 Properties of Iron Oxides 7.4.2.2 Bioavailability of Iron Oxides 7.4.2.3 Bioavailability of Sheet Silicate Sound Ferric lron 7.4.3 Iron and Manganese Redax Cycles 7.4.4 Iron Reactivity towards S, O2, Mn, NO3, P, HCO3, and Si-AI 7.4.4.1 lron Reduction by HS and Ligands 7.4.4.2 Iron Oxidation by O2, NO3, and Mn4+ 7.4.4.3 Iron-Sound Phosphorus 7.4.4.4 The Formation of Siderite 7.4.4.5 The Formation of lron Searing Aluminosilicates 7.4.5 Discussion: The Importance of Fe-and Mn-Reactivity in Various Enyironments 7.5 The Assay for Ferric and Ferrous Iron 8 Sulfate Reduction in Marine Sediments / SABINE KASTEN AND BO BARKER JØRGENSEN 8.1 Introduction 8.2 Sulfate Reduction and the Degradation of Organic Matter 8.3 Biotic and Abiotic Processes Coupled to Sulfate Reduction 8.3.1 Pyrite Formation 8.3.2 Effects of Sulfate Reduction on Sedimentary Solid Phases 8.4 Determination of Sulfate Reduction Rates 9 Marine Carbonates: Their Formation and Destruction / RALPH R. SCHNEIDER, HORST D. SCHULZ AND CHRISTIAN HENSEN 9.1 Introduction 9.2 Marine Environments of Carbonate Production and Accumulation 9.2.1 Shallow-Water Carbonates 9.2.2 Pelagic Calcareous Sediments 9.3 The Calcite-Carbonate-Equilibrium in Marine Aquatic Systems 9.3.1 Primary Reactions of the Calcite-Carbonate-Equilibrium with Atmospheric Contact in Infinitely Diluted Solutions 9.3.2 Primary Reactions of the Calcite-Carbonate-Equilibrium without Atmospheric Contact 9.3.3 Secondary Reactions of the Calcite-Carbonate-Equilibrium in Seawater 9.3.4 Examples for Calculation of the Calcite-Carbonate-Equilibrium in Ocean Waters 9.4 Carbonate Reservoir Sizes and Fluxes between Particulate and Dissolved Reservoirs 9.4.1 Production Versus Dissolution of Pelagic Carbonates 9.4.2 Inorganic and Organic Carbon Release trom Deep-Sea Sediments 10 Influences of Geochemical Processes on Stable Isotope Distribution in Marine Sediments / TORSTEN SICKERT 10.1 Introduction 10.2 Fundamentals 10.2.1 Principles of Isotopic Fractionation 10.2.2 Analytical Procedures 10.3 Geochemicallnfluences on 18O/16O Ratios 10.3.1 δ18O of Seawater 10.3.2 δ18O in Marine Carbonates 10.4 Geochemical Influences on 13C/12C Ratios 10.4.1
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  • 7
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 01.0571
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This volume was prepared for Short Course on Stable Isotope Geochemistry presented November 2-4, 2001 in conjunction with the annual meetings of the Geological Society of America in Boston, Massachusetts. This volume follows the 1986 Reviews in Mineralogy (Vol. 16) in approach but reflects significant changes in the field of Stable Isotope Geochemistry. In terms of new technology, new sub-disciplines, and numbers of researchers, the field has changed more in the past decade than in any other since that of its birth. Unlike the 1986 volume, which was restricted to high temperature fields, this book covers a wider range of disciplines. However, it would not be possible to fit a comprehensive review into a single volume. Our goal is to provide state-ofthe-art reviews in chosen subjects that have emerged or advanced greatly since 1986. The field of Stable Isotope Geochemistry was born of a good idea and nurtured by technology. In 1947, Harold Urey published his calculated values of reduced partition function for oxygen isotopes and his idea (a good one!) that the fractionation of oxygen isotopes between calcite and water might provide a means to estimate the temperatures of geologic events. Building on wartime advances in electronics, Alfred Nier then designed and built the dual-inlet, gassource mass-spectrometer capable of making measurements of sufficient precision and accuracy. This basic instrument and the associated extraction techniques, mostly from the 1950s, are still in use in many labs today. These techniques have become "conventional" in the sense of traditional, and they provide the benchmark against which the accuracy of other techniques is compared. The 1986 volume was based almost exclusively on natural data obtained solely from conventional techniques. Since then, revolutionary changes in sample size, accuracy, and cost have resulted from advances in continuous flow massspectrometry, laser heating, ion microprobes, and computer automation. The impact of new technology has differed by discipline. Some areas have benefited from vastly enlarged data sets, while others have capitalized on in situ analysis and/or micro- to nanogram size samples, and others have developed because formerly intractable samples can now be analyzed. Just as Stable Isotope Geochemistry is being reborn by new good ideas, it is still being nurtured by new technology. The organization of the chapters in this book follows the didactic approach of the 2001 short course in Boston. The first three chapters present the principles and data base for equilibrium isotope fractionation and for kinetic processes of exchange. Both inorganic and biological aspects are considered. The next chapter reviews isotope compositions throughout the solar system including massindependent fractionations that are increasingly being recognized on Earth. The fifth chapter covers the primitive compositions of the mantle and subtle variations found in basalts. This is followed by three chapters on metamorphism, isotope thermometry, fluid flow, and hydrothermal alteration. The next chapter considers water cycling in the atmosphere and the ice record. And finally, there are four chapters on the carbon cycle, the sulfur cycle, organic isotope geochemistry and extinctions in the geochemical record.
    Type of Medium: Monograph available for loan
    Pages: XIV, 662 S.
    ISBN: 0-939950-55-3 , 978-0-939950-55-3
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 43
    Classification:
    Geochemistry
    Note: Chapter 1. Equilibrium Oxygen, Hydrogen and Carbon Isotope Fractionation Factors Applicable to Geologic Systems by Thomas Chacko, David R. Cole, and Juske Horita, p. 1 - 82 Chapter 2. Rates and Mechanisms of Isotopic Exchange by David R. Cole and S Chakraborty, p. 83 - 224 Chapter 3. Fractionation of Carbon and Hydrogen Isotopes in Biosynthetic Processes by John M Hayes, p. 225 - 278 Chapter 4. Stable Isotope Variations in Extraterrestrial Materials by Kevin D. Mckeegan and Laurie A Leshinv, p. 279 - 318 Chapter 5. Oxygen Isotope Variations of Basaltic Lavas and Upper Mantle Rocks by John M. Eiler, p. 319 - 364 Chapter 6. Stable Isotope Thermometry at High Temperatures by John W. Valley, p. 365 - 414 Chapter 7. Stable Isotope Transport and Contact Metamorphic Fluid Flow by Lukas P. Baumgartner and John W. Valley, p. 415 - 468 Chapter 8. Stable Isotopes in Seafloor Hydrothermal Systems by Wayne C. Shanks III, p. 469 - 526 Chapter 9. Oxygen- and Hydrogen-Isotopic Ratios of Water in Precipitation: Beyond Paleothermometry by Richard B. Alley and Kurt M. Cuffey, p. 527 - 554 Chapter 10. Isotopic Evolution of the Biogeochemical Carbon Cycle During the Precambrian by David J. Des Marais, p. 555 - 578 Chapter 11. Isotopic Biogeochemistry of Marine Organic Carbon by Katherine H. Freeman, p. 579 - 606 Chapter 12. Biogeochemistry of Sulfur Isotopes by Don E. Canfield, p. 607 - 636 Chapter 13. Stratigraphic Variation in Marine Carbonate Carbon Isotope Ratios by Robert L. Ripperdan, p. 637 - 662
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  • 8
    Call number: S 92.0097(159)
    In: Report of investigation = Tutkimusraportti
    Type of Medium: Series available for loan
    Pages: 35 S. , graph. Darst., Kt.
    ISBN: 9516908853
    Series Statement: Report of investigation 159
    Classification:
    Geochemistry
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  • 9
    Call number: 9/M 07.0155
    In: Geological Society special publication
    Description / Table of Contents: The 32 research papers in this volume examine the mode and nature of igneous, metamorphic, tectonic, sedimentological and biological processes associated with the evolution of ophiolites in Earth's history. Divided into six sections, the book presents a wealth of new data and syntheses from ophiolites around the world. Introductory chapters review the distribution of ophiolites in space and time and present a synoptic discussion on their importance in Earth history. Papers in the second section present diverse data from Tethyan ophiolites and provide refined geodynamic models for their evolution. The following two sections present case studies documenting magmatic, metamorphic and tectonic processes in ophiolite genesis and hydrothermal and biogenic alteration of fossil oceanic crust. Mechanisms of ophiolite emplacement are explored in Section V with a focus on the Semail massif (Oman). The last section examines the regional occurrence and geodynamic significance of ophiolite belts on different continents. The book reflects the contemporary work of the international community in a most up-to-date treatment of process-oriented questions on the evolution of ophiolites.
    Type of Medium: Monograph available for loan
    Pages: VI, 717 S. , Ill., graph. Darst., Kt. , 26 cm
    ISBN: 1862391459
    Series Statement: Geological Society special publication 218
    Classification:
    Geochemistry
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  • 10
    Unknown
    [Kraków] : Society of Research on Environment Changes "GEOSPHERE"
    Call number: M 07.0054/1-2
    Pages: Part 1-2
    ISBN: 8391576523
    Classification:
    Geochemistry
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  • 11
    Series available for loan
    Series available for loan
    Hannover [u.a.] : Bundesanstalt für Geowissenschaften und Rohstoffe
    Associated volumes
    Call number: S 99.0136(26)
    In: Rohstoffwirtschaftliche Länderstudien
    Type of Medium: Series available for loan
    Pages: 80 S. , Ill., graph. Darst., Kt. , 30 cm
    ISBN: 3510959043
    Series Statement: Rohstoffwirtschaftliche Länderstudien 26
    Classification:
    Geochemistry
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  • 12
    Monograph available for loan
    Monograph available for loan
    Parkland, Fla. : Universal Publishers
    Call number: M 12.0050
    Type of Medium: Monograph available for loan
    Pages: XX, 562 S. : graph. Darst.
    ISBN: 1581126204
    Classification:
    Geochemistry
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  • 13
    Monograph available for loan
    Monograph available for loan
    Princeton, N.J. [u.a.] : Princeton Univ. Press
    Call number: 10/M 12.0302
    Description / Table of Contents: Contents: Chapter 1. Metabolic Synthesis Chapter 2. Chemical Biomarker Applications to Ecology and Paleoecology Chapter 3. Stable Isotopes and Radiocarbon Chapter 4. Analytical Chemical Methods and Instrumentation Chapter 5. Carbohydrates: Neutral and Minor Sugars Chapter 6. Proteins: Amino Acids and Amines Chapter 7. Nucleic Acids and Molecular Tools Chapter 8. Lipids: Fatty Acids Chapter 9. Isoprenoid Lipids: Steroids, Hopanoids, and Triterpenoids Chapter 10. Lipids: Hydrocarbons Chapter 11. Lipids: Alkenones, Polar Lipids, and Ether Lipids Chapter 12. Photosynthetic Pigments: Chlorophylls, Carotenoids, and Phycobilins Chapter 13. Lignins, Cutins, and Suberins Chapter 14. Anthropogenic Markers Appendix I. Atomic Weights of Elements Appendix II. Useful SI Units and Conversion Factors Appendix III. Physical and Chemical Constants Glossary Bibliography
    Type of Medium: Monograph available for loan
    Pages: xvii, 396 S. , Ill., graph. Darst. , 26 cm
    ISBN: 9780691134147
    Classification:
    Geochemistry
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  • 14
    Call number: 21/STR 12/07
    In: Scientific technical report
    Type of Medium: GFZ publications
    Pages: xii, 181 S. : Ill., graph. Darst.
    Series Statement: Scientific technical report / Deutsches GeoForschungsZentrum GFZ 12/07
    Classification:
    Geochemistry
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  • 15
    Monograph available for loan
    Monograph available for loan
    Chichester-Blackwell : Wiley
    Call number: 10/M 14.0031
    Description / Table of Contents: This book provides a comprehensive introduction to the field of geochemistry. The book first lays out the 'geochemical toolbox': the basic principles and techniques of modern geochemistry, beginning with a review of thermodynamics and kinetics as they apply to the Earth and its environs. These basic concepts are then applied to understanding processes in aqueous systems and the behavior of trace elements in magmatic systems. Subsequent chapters introduce radiogenic and stable isotope geochemistry and illustrate their application to such diverse topics as determining geologic time, ancient climates, and the diets of prehistoric peoples. The focus then broadens to the formation of the solar system, the Earth, and the elements themselves. Then the composition of the Earth itself becomes the topic, examining the composition of the core, the mantle, and the crust and exploring how this structure originated. A final chapter covers organic chemistry, including the origin of fossil fuels and the carbon cycle's role in controlling Earth's climate, both in the geologic past and the rapidly changing present.
    Type of Medium: Monograph available for loan
    Pages: VII, 660 S. : Ill., graph. Darst., Kt.
    ISBN: 9780470656686
    Classification:
    Geochemistry
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  • 16
    Call number: S 98.0095(2013-2)
    In: Tagungsbericht / Deutsche Wissenschaftliche Gesellschaft für Erdöl, Erdgas und Kohle
    Type of Medium: Series available for loan
    Pages: 273 S. : Ill., graph. Darst. , 1 CD-ROM
    Edition: Als Ms. gedr.
    ISBN: 9783941721326
    Series Statement: Tagungsbericht / Deutsche Wissenschaftliche Gesellschaft für Erdöl, Erdgas und Kohle 2013, 2
    Classification:
    Geochemistry
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  • 17
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 07.0421(398)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: VI, 213 S. : z.T. farb. Ill., graph. Darst., Kt.
    ISBN: 9781862396418
    Series Statement: Geological Society special publication 398
    Classification:
    Geochemistry
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  • 18
    Call number: S 90.0002(1763)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: vi, 429 S. + 1 CD-ROM
    ISBN: 9781411326224
    Series Statement: U.S. Geological Survey professional paper 1763
    Classification:
    Geochemistry
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  • 19
    Call number: S 91.0379(10)
    In: Hallesches Jahrbuch für Geowissenschaften. Reihe B, Geologie, Paläontologie, Mineralogie. Beiheft
    Type of Medium: Series available for loan
    Pages: 156 S.
    Series Statement: Hallesches Jahrbuch für Geowissenschaften : Reihe B, Geologie, Paläontologie, Mineralogie : Beiheft 10
    Classification:
    Geochemistry
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  • 20
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 01.0176
    Type of Medium: Monograph available for loan
    Pages: XV, 496 S.
    ISBN: 3540677720
    Classification:
    Geochemistry
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  • 21
    Call number: S 90.0002(1619)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, 41 S.
    ISBN: 0607930802
    Series Statement: U.S. Geological Survey professional paper 1619
    Classification:
    Geochemistry
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  • 22
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Press
    Call number: M 00.0524 ; AWI G6-02-0002 ; PIK W 111-00-0377
    Description / Table of Contents: Reducing carbon dioxide (CO2) emissions is imperative to stabilizing our future climate. Our ability to reduce these emissions, combined with an understanding of how much fossil fuel-derived CO2 the oceans and plants can absorb, is central to mitigating climate change. In The Carbon Cycle, leading scientists examine how atmospheric carbon dioxide concentrations have changed in the past and how this may effect the concentrations in the future. They look at the carbon budget and the "missing sink" for carbon dioxide. They offer approaches to modeling the carbon cycle, providing mathematical tools for predicting future levels of carbon dioxide. This comprehensive text incorporates findings from the recent IPCC reports. New insights, and a convergence of ideas and views across several disciplines, make this book an important contribution to the global change literature. It is an invaluable resource for students and researchers working in the field.
    Type of Medium: Monograph available for loan
    Pages: XVII, 292 S.
    Edition: 1st ed.
    ISBN: 0521583373
    Series Statement: Office for Interdisciplinary Earth Studies Global Change Institute 6
    Classification:
    Geochemistry
    Language: English
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  • 23
    Call number: S 99.0056(2000/2)
    In: Terra nostra
    Type of Medium: Series available for loan
    Pages: VI, 138 S.
    Series Statement: Terra nostra 2000,2
    Classification:
    Geochemistry
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  • 24
    Series available for loan
    Series available for loan
    Berlin : Fachbereich Geowiss., FU
    Associated volumes
    Call number: S 90.0061(206)
    In: Berliner geowissenschaftliche Abhandlungen
    Type of Medium: Series available for loan
    Pages: 111 S.
    ISBN: 3895820806
    Series Statement: Berliner geowissenschaftliche Abhandlungen : Reihe A, Geologie und Paläontologie 206
    Classification:
    Geochemistry
    Language: German
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  • 25
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    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 10/M 00.0311
    In: Handbook of exploration geochemistry
    Type of Medium: Monograph available for loan
    Pages: XXI, 549 S.
    ISBN: 0444504397
    Series Statement: Handbook of exploration geochemistry 7
    Classification:
    Geochemistry
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  • 26
    Call number: S 90.0002(1648)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: 38 S.
    ISBN: 0607977949
    Series Statement: U.S. Geological Survey professional paper 1648
    Classification:
    Geochemistry
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  • 27
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 10/M 03.0196
    Type of Medium: Monograph available for loan
    Pages: XI, 462 S.
    ISBN: 3540002480
    Classification:
    Geochemistry
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  • 28
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    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 10/M 02.0598
    In: Developments in geochemistry
    Type of Medium: Monograph available for loan
    Pages: xvii, 226 S.
    Edition: 1st ed.
    ISBN: 0444505695
    Series Statement: Developments in geochemistry 7
    Classification:
    Geochemistry
    Language: English
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  • 29
    Call number: 11/M 03.0435
    In: Springer series in materials science
    Type of Medium: Monograph available for loan
    Pages: XVIII, 561 S.
    ISBN: 3540642242
    Series Statement: Springer series in materials science 55
    Classification:
    Geochemistry
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  • 30
    Series available for loan
    Series available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0180
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Exactly 100 years before the publication of this volume, the first paper which calculated the half-life for the newly discovered radioactive substance U-X (now called 234Th), was published. Now, in this volume, the editors Bernard Bourdon, Gideon Henderson, Craig Lundstrom and Simon Turner have integrated a group of contributors who update our knowledge of U-series geochemistry, offer an opportunity for non-specialists to understand its basic principles, and give us a view of the future of this active field of research. In this volume, for the first time, all the methods for determining the uranium and thorium decay chain nuclides in Earth materials are discussed. It was prepared in advance of a two-day short course (April 3-4, 2003) on U-series geochemistry, jointly sponsored by GS and MSA and presented in Paris, France prior to the joint EGS/AGU/EUG meeting in Nice. The discovery of the 238U decay chain, of course, started with the seminal work of Marie Curie in identifying and separating 226Ra. Through the work of the Curies and others, all the members of the 238U decay chain were identified. An important milestone for geochronometrists was the discovery of 230Th (called Ionium) by Bertram Boltwood, the Yale scientist who also made the first age determinations on minerals using the U-Pb dating method (Boltwood in 1906 established the antiquity of rocks and even identified a mineral from Sri Lanka-then Ceylon as having an age of 2.1 billion years!) The application of the 238U decay chain to the dating of deep sea sediments was by Piggott and Urry in 1942 using the "Ionium" method of dating. Actually they measured 222Ra (itself through 222Rn) assuming secular equilibrium had been established between 230Th and 226Ra. Although 230Th was measured in deep sea sediments by Picciotto and Gilvain in 1954 using photographic emulsions, it was not until alpha spectrometry was developed in the late 1950's that 20Th was routinely measured in marine deposits. Alpha spectrometry and gamma spectrometry became the work horses for the study of the uranium and thorium decay chains in a variety of Earth materials. These ranged from 222Rn and its daughters in the atmosphere, to the uranium decay chain nuclides in the oceanic water column, and volcanic rocks and many other systems in which either chronometry or element partitioning, were explored. Much of what we learned about the 238U, 235U and 232Th decay chain nuclides as chronometers and process indicators we owe to these seminal studies based on the measurement of radioactivity. The discovery that mass spectrometry would soon usurp many of the tasks performed by radioactive counting was in itself serendipitous. It came about because a fundamental issue in cosmochemistry was at stake. Although variation in 235U/238U had been reported for meteorites the results were easily discredited as due to analytical difficulties. One set of results, however, was published by a credible laboratory long involved in quality measurements of high mass isotopes such as the lead isotopes. The purported discovery of 235U/238U variations in meteorites, if true, would have consequences in defining the early history of the formation of the elements and the development of inhomogeneity of uranium isotopes in the accumulation of the protoplanetary materials of the Solar System. Clearly the result was too important to escape the scrutiny of falsification implicit in the way we do science. The Lunatic Asylum at Caltech under the leadership of Jerry Wasserburg took on that task. Jerry Wasserburg and Jim Chen clearly established the constancy and Earth-likeness of 235U/238U in the samplable universe. In the hands of another member of the Lunatic Asylum, Larry Edwards, the methodology was transformed into a tool for the study of the 238U decay chain in marine systems. Thus the mass spectrometric techniques developed provided an approach to measuring the U and Th isotopes in geological materials as well as cosmic materials with the same refinement and accommodation for small sample size. Soon after this discovery the harnessing of the technique to the measurement of all the U isotopes and all the Th isotopes with great precision immediately opened up the entire field of uranium and thorium decay chain studies. This area of study was formerly the poaching ground for radioactive measurements alone but now became part of the wonderful world of mass spectrometric measurements. (The same transformation took place for radiocarbon from the various radioactive counting schemes to 'accelerator mass spectrometry.) No Earth material was protected from this assault. The refinement of dating corals, analyzing volcanic rocks for partitioning and chronometer studies and extensions far and wide into ground waters and ocean bottom dwelling organisms has been the consequence of this innovation. Although Ra isotopes, 210Pb and 210Po remain an active pursuit of those doing radioactive measurements, many of these nuclides have also become subject to the mass spectrometric approach. In this volume, for the first time, all the methods for determining the uranium and thorium decay chain nuclides in Earth materials are discussed. The range of problems solvable with this approach is remarkable-a fitting, tribute to the Curies and the early workers who discovered them for us to use.
    Type of Medium: Series available for loan
    Pages: xx, 656 S.
    ISBN: 0-939950-64-2 , 978-0-939950-64-5
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 52
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. Introduction to U-series Geochemistry by Bernard Bourdon, Simon Turner, Gideon M. Henderson and Craig C. Lundstrom, p. 1 - 22 Chapter 2. Techniques for Measuring Uranium-series Nuclides: 1992-2002 by Steven J. Goldstein and Claudine H. Stirling, p. 23 - 58 Chapter 3. Mineral-Melt Partitioning of Uranium, Thorium and Their Daughters by Jonathan Blundy and Bernard Wood, p. 59 - 124 Chapter 4. Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks by Michel Condomines, Pierre-Jean Gauthier, and Olgeir Sigmarsson, p. 125 - 174 Chapter 5. Uranium-series Disequilibria in Mid-ocean Ridge Basalts: Observations and Models of Basalt Genesis by Craig C. Lundstrom, p. 175 - 214 Chapter 6. U-series Constraints on Intraplate Basaltic Magmatism by Bernard Bourdon and Kenneth W. W. Sims, p. 215 - 254 Chapter 7. Insights into Magma Genesis at Convergent Margins from U-series Isotopes by Simon Turner, Bernard Bourdon and Jim Gill, p. 255 - 316 Chapter 8. The Behavior of U- and Th-series Nuclides in Groundwater by Donald Porcelli and Peter W. Swarzenski, p. 317 - 362 Chapter 9. Uranium-series Dating of Marine and Lacustrine Carbonates by R. L. Edwards, C. D. Gallup, and H. Cheng, p. 363 - 406 Chapter 10. Uranium-series Chronology and Environmental Applications of Speleothems by David A. Richards and Jeffrey A. Dorale, p. 407 - 460 Chapter 11. Short-lived U/Th Series Radionuclides in the Ocean: Tracers for Scavenging Rates, Export Fluxes and Particle Dynamics by J. K. Cochran and P. Masquè, p. 461 - 492 Chapter 12. The U-series Toolbox for Paleoceanography by Gideon M. Henderson and Robert F. Anderson, p. 493 - 532 Chapter 13. U-Th-Ra Fractionation During Weathering and River Transport by F. Chabaux, J. Riotte and O. Dequincey, p. 533 - 576 Chapter 14. The Behavior of U- and Th-series Nuclides in the Estuarine Environment by Peter W. Swarzenski, Donald Porcelli, Per S. Andersson and Joseph M. Smoakv, p. 577 - 606 Chapter 15. U-series Dating and Human Evolution by A. W. G. Pike and P. B. Pettitt, p. 607 - 630 Chapter 16. Mathematical-Statistical Treatment of Data and Errors for 230Th/U Geochronology by K. R. Ludwig, p. 631 - 656
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  • 31
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 02.0438
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: The editors and contributing authors of this volume participated in a short course on micas in Rome late in the year 2000. It was organised by Prof. Annibale Mottana and several colleagues (details in the Preface below) and underwritten by the Italian National Academy, Accademia Nationale dei Lincei (ANL). The Academy subsequently joined with the Mineralogical Society of America (MSA) in publishing this volume. MSA is grateful for their generous involvement. Micas are among the most common minerals in the Earth crust: 4.5% by volume. They are widespread in most if not all metamorphic rocks (abundance: 11 %), and common also in sediments and sedimentary and igneous rocks. Characteristically, micas form in the uppermost greenschist facies and remain stable to the lower crust, including anatectic rocks (the only exception: granulite facies racks). Moreover, some micas are stable in sediments and diagenetic rocks and crystallize in many types of lavas. In contrast, they are also present in association with minerals originating from the very deepest parts of the mantle-they are the most common minerals accompanying diamond in kimberlites. The number of research papers dedicated to micas is enormous, but knowledge of them is limited and not as extensive as that of other rock-forming minerals, for reasons mostly relating to their complex layer texture that makes obtaining crystals suitable for careful studies with modern methods time-consuming, painstaking work. Micas were reviewed extensively in 1984 (Reviews in Mineralogy 13, S.W. Bailey, editor). At that time, the "Micas" volume covered most if not all aspects of mica knowledge, thus producing a long shelf-life for this book. Yet, or perhaps because of that excellent review, mica research was vigorously renewed, and a vast array of new data has been gathered over the past 15 years. These data now need to be organized and reviewed. Furthermore, a Committee nominated by the International Mineralogical Association in the late 1970s concluded its long-lasting work (Rieder et al. 1998) by suggesting a new classification scheme which has stimulated new chemical and structural research on micas. To make a very long story short: the extraordinarily large, but intrinsically vague, mica nomenclature developed during the past two centuries has been reduced from 〉300 to just 37 species names and 6 series (see page xiii, preceding Chapter 1); the new nomenclature shows wide gaps that require data involving new chemical and structural work; the suggestion of using adjectival modifiers for those varieties that deviate away from end-member compositions requires the need for new and accurate measurements, particularly for certain light elements and volatiles; the use of polytype suffixes based on the modified Gard symbolism created better ways of determining precise stacking sequences. This resulted in new polytypes being discovered. Indeed, all this has happened over the past few years in an almost tumultuous way. It was on the basis of these developments that four scientists (B. Zanettin, A. Mottana, F.P. Sassi and C. Cipriani) applied to Accademia Nazionale dei Lincei-the Italian National Academy-for a meeting on micas. An international meeting was convened in Rome on November 2-3, 2000 with the title Advances on Micas (Problems, Methods, Applications in Geodynamics). The topics of this meeting were the crystalchemical, petrological, and historical aspects of the micas. The organizers were both Academy members (C. Cipriani, A. Mottana, F.P. Sassi, W. Schreyer, lB. Thompson Jr., and B. Zanettin) and Italian scientists well-known for their studies on layer silicates (Professors M.F. Brigatti and G. Ferraris). Financial support in additional to that by the Academy was provided by C.N.R. (the Italian National Research Council), M.U.R.S.T. (the Italian Ministry for University, Scientific Research and Technology) and the University of Rome III. Approximately 200 scientists attended the meeting, most of them Italians, but with a sizeable international participation. Thirteen invited plenary lectures and six oral presentations were given, and fourteen posters were displayed. The amount of information presented was large, although the organizers made it very clear that the meeting was to be limited to only a few of the major topics of mica studies. Other topics are promised for a later meeting. Oral and poster presentations on novel aspects of mica research are being printed in the European Journal of Mineralogy, as a part of an individual thematic issue: indeed thirteen papers have appeared in the November 2001 issue. The plenary lectures, which consisted mostly of reviews, are presented in expanded detail in this volume. This book is the first a co-operative project between Accademia Nazionale dei Lincei and Mineralogical Society of America. Hopefully, future projects will involve reviews of the remaining aspects of mica research, and other aspects of mineralogy and geochemistry. The entire meeting was made successful through a co-operative effort. The editing of this book was achieved by a co-operative effort of two Italian Academy members from one side, and by two American scientists from the other side, one of them (JBT) being also a member of Lincei Academy. The entire editing process benefited from the goodwill of many referees, both from those attending the Rome meeting and from several who did not. In all cases the reviewers were distinguished experts of the international community of mica scholars. Their work, as well as our editing work, were aided greatly by RiMG Series Editor, Professor Paul Ribbe, who continuously supported the effort with all his professional experience and friendly advice. We, the co-editors, thank them all very warmly, but take upon ourselves all remaining shortcomings: we are aware that some shortcomings may be present in spite of all our efforts to avoid them. Moreover, we are aware that there are puzzling aspects of micas that are unresolved. Please consider all these as possible avenues for future research!
    Type of Medium: Monograph available for loan
    Pages: xiii, 499 S.
    ISBN: 0-939950-58-8 , 978-0-939950-58-4
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 46
    Classification:
    Geochemistry
    Language: English
    Note: Crystal Chemistry Chapter 1. Mica crystal chemistry and the influence of pressure, temperature, and solid solution on atomistic models by Maria Franca Brigatti and Stephen Guggenheim, p. 1 - 98 Chapter 2. Behavior of micas at high pressure and high temperature by Pier Francesco Zanazzi and Alessandro Pavese, p. 99 - 116 Chapter 3. Structural features of micas by Giovanni Ferraris and Gabriella Ivaldi, p. 117 - 154 Chapter 4. Crystallographic basis of polytypism and twinning in micas by Massimo Nespolo and Slavomil Durovic, p. 155 - 280 Chapter 5. Investigation of micas using advanced transmission electron microscopy by Toshihiro Kogure, p. 281 - 312 Chapter 6. Optical and Mössbauer spectroscopy of iron in micas by M. Darby Dyar, p. 313 - 350 Chapter 7. Infrared spectroscopy of micas by Anton Beran, p. 351 - 370 Chapter 8. X-ray absorption spectroscopy of the micas by Annibale Mottana, Augusto Marcelli, Giannantonio Cibin, and M. Darby Dyar, p. 371 - 412 Metamorphic Petrology Chapter 9. Constraints on studies of metamorphic K-Na white micas by Charles V. Guidotti and Francesco P. Sassi, p. 413 - 448 Chapter 10. Modal spaces for pelitic schists by James B. Thompson, Jr., p. 449 - 462 Chapter 11. Phyllosilicates in very low-grade metamorphism: Transformation to micas by Péter Árkai, p. 463 - 478 Historical Perspective Chapter 12. Micas: Historical perspective by Curzio Cipriani, p. 479 - 499
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  • 32
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
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    Call number: ZS-090(420) ; ZSP-168-420
    In: Berichte zur Polar- und Meeresforschung
    Type of Medium: Series available for loan
    Pages: v, 177 S.
    ISSN: 1618-3193
    Series Statement: Berichte zur Polar- und Meeresforschung 420
    Classification:
    Geochemistry
    Language: German
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  • 33
    Call number: 21/STR 02/11
    In: Scientific Technical Report STR
    Type of Medium: GFZ publications
    Pages: VI, 113 S. : Ill., graph. Darst., Kt.
    Series Statement: Scientific Technical Report STR 02/11
    Classification:
    Geochemistry
    Language: German
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    Call number: M 02.0584
    Type of Medium: Monograph available for loan
    Pages: xv, 187 S.
    Classification:
    Geochemistry
    Language: English
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  • 35
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    Monograph available for loan
    Amsterdam : Elsevier
    Call number: M 02.0413
    Type of Medium: Monograph available for loan
    Pages: xiv, 714 S.
    Series Statement: Journal of geochemical exploration 69/70 : Special issue
    Classification:
    Geochemistry
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  • 36
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0179
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This volume highlights some of the frontiers in the study of plastic deformation of minerals and rocks. The research into the plastic properties of minerals and rocks had a major peak in late 1960s to early 1970s, largely stimulated by research in the laboratory of D. T. Griggs and his students and associates. It is the same time when the theory of plate tectonics was established and provided a first quantitative theoretical framework for understanding geological processes. The theory of plate tectonics stimulated the study of deformation properties of Earth materials, both in the brittle and the ductile regimes. Many of the foundations of plastic deformation of minerals and rocks were established during this period. Also, new experimental techniques were developed, including deformation apparatus for high-pressure and high-temperature conditions, electron micros-copy study of defects in minerals, and the X-ray technique of deformation fabric analysis. The field benefited greatly from materials science concepts of deformation that were introduced, including the models of point defects and their interaction with dislocations. A summary of progress is given by the volume Flow and Fracture of Rocks: The Griggs Volume, published in 1972 by the American Geophysical Union. Since then, the scope of Earth sciences has greatly expanded. Geodynamics became concerned with the Earth's deep interior where seismologists discovered heterogeneities and anisotropy at all scales that were previously thought to be typical of the crust and the upper mantle. Investigations of the solar system documented new mineral phases and rocks far beyond the Earth. Both domains have received a lot of attention from mineralogists (e.g., summarized in MSA's Reviews in Mineralogy, Volume 36, Planetary Materials and Volume 37, Ultra-High Pressure Mineralogy). Most attention was directed towards crystal chemistry and phase relations, yet an understanding of the deformation behavior is essential for interpreting the dynamic geological processes from geological and geophysical observations. This was largely the reason for a rebirth of the study of rock plasticity, leading to new approaches that include experiments at extreme conditions and modeling of deformation behavior based on physical principles. A wide spectrum of communities emerged that need to use information about mineral plasticity, including mineralogy, petrology, structural geology, seismology, geodynamics and engineering. This was the motivation to organize a workshop, in December 2002 in Emeryville, California, to bridge the very diverse disciplines and facilitate communication. This volume written for this workshop should help one to become familiar with a notoriously difficult subject, and the various contributions represent some of the important progress that has been achieved. The spectrum is broad. High-resolution tomographic images of Earth's interior obtained from seismology need to be interpreted on the bases of materials properties to understand their geodynamic significance. Key issues include the influence of deformation on seismic signatures, such as attenuation and anisotropy, and a new generation of experimental and theoretical studies on rock plasticity has contributed to a better understanding. Extensive space exploration has revealed a variety of tectonic styles on planets and their satellites, underlining the uniqueness of the Earth. To understand why plate tectonics is unique to Earth, one needs to understand the physical mechanisms of localization of deformation at various scales and under different physical conditions. Also here important theoretical and experimental studies have been conducted. In both fields, studies on anisotropy and shear localization, large-strain deformation experiments and quantitative modeling are critical, and these have become available only recently. Complicated interplay among chemical reactions (including partial melting) is a key to understand the evolution of Earth. This book contains two chapters on the developments of new techniques of experimental studies: one is large-strain shear deformation (Chapter 1 by Mackwell and Paterson) and another is deformation experiments under ultrahigh pressures (Chapter 2 by Durham et al.). Both technical developments are the results of years of efforts that are opening up new avenues of research along which rich new results are expected to be obtained. Details of physical and chemical processes of deformation in the crust and the upper mantle are much better understood through the combination of well controlled laboratory experiments with observations on "real" rocks deformed in Earth. Chapter 3 by Tullis and Chapter 4 by Hirth address the issues of deformation of crustal rocks and the upper mantle, respectively. In Chapter 5 Kohlstedt reviews the interplay of partial melting and deformation, an important subject in understanding the chemical evolution of Earth. Cordier presents in Chapter 6 an overview of the new results of ultrahigh pressure deformation of deep mantle minerals and discusses microscopic mechanisms controlling the variation of deformation mechanisms with minerals in the deep mantle. Green and Marone review in Chapter 7 the stability of deformation under deep mantle conditions with special reference to phase transformations and their relationship to the origin of intermediate depth and deep-focus earthquakes. In Chapter 8 Schulson provides a detailed description of fracture mechanisms of ice, including the critical brittle-ductile transition that is relevant not only for glaciology, planetology and engineering, but for structural geology as well. In Chapter 9 Cooper provides a review of experimental and theoretical studies on seismic wave attenuation, which is a critical element in interpreting distribution of seismic wave velocities and attenuation. Chapter 10 by Wenk reviews the relationship between crystal preferred orientation and macroscopic anisotropy, illustrating it with case studies. In Chapter 11 Dawson presents recent progress in poly-crystal plasticity to model the development of anisotropic fabrics both at the microscopic and macroscopic scale. Such studies form the basis for geodynamic interpretation of seismic anisotropy. Finally, in Chapter 12 Montagner and Guillot present a thorough review of seismic anisotropy of the upper mantle covering the vast regions of geodynamic interests, using a global surface wave data set. In Chapter 13 Bercovici and Karato summarize the theoretical aspects of shear localization. All chapters contain extensive reference lists to guide readers to the more specialized literature. Obviously this book does not cover all the areas related to plastic deformation of minerals and rocks. Important topics that are not fully covered in this book include mechanisms of semi-brittle deformation and the interplay between microstructure evolution and deformation at different levels, such as dislocation substructures and grain-size evolution ("self-organization"). However, we hope that this volume provides a good introduction for graduate students in Earth science or materials science as well as the researchers in these areas to enter this multidisciplinary field.
    Type of Medium: Monograph available for loan
    Pages: xii, 420 S..
    ISBN: 0-939950-63-4 , 978-0-939950-63-8
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 51
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. New Developments in Deformation Studies: High-Strain Deformation by Stephen J. Mackwell and Mervyn S. Paterson, p. 1 - 20 Chapter 2. New Developments in Deformation Experiments at High Pressure by William B. Durham, Donald J. Weidner, Shun-ichiro Karato, and Yanbin Wang, p. 21 - 50 Chapter 3. Deformation of Granitic Rocks: Experimental Studies and Natural Examples by Jan Tullis, p. 51 - 96 Chapter 4. Laboratory Constraints on the Rheology of the Upper Mantle by Greg Hirth, p. 97 - 120 Chapter 5. Partial Melting and Deformation by David L. Kohlstedt, p. 121 - 136 Chapter 6. Dislocations and Slip Systems of Mantle Minerals by Patrick Cordier, p. 137 - 180 Chapter 7. Instability of Deformation by Harry W. Green II and Chris Marone, p. 181 - 200 Chapter 8. Brittle Failure of Ice by Erland M. Schulson, p. 201 - 525 Chapter 9. Seismic Wave Attenuation: Energy Dissipation in Viscoelastic Crystalline Solids by Reid F. Cooper, p. 253 - 290 Chapter 10. Texture and Anisotropy by Hans-Rudolf Wenk, p. 291 - 330 Chapter 11. Modeling Deformation of Polycrystalline Rocks by Paul R. Dawson, p. 331 - 352 Chapter 12. Seismic Anisotropy and Global Geodynamics by Jean-Paul Montagner and Laurent Guillot, p. 353 - 386 Chapter 13. Theoretical Analysis of Shear Localization in the Lithosphere by David Bercovici and Shun-ichiro Karato, p. 387 - 420
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  • 37
    Call number: S 99.0046(32)
    In: Münchner geologische Hefte
    Type of Medium: Series available for loan
    Pages: xiii, 132 S.
    Series Statement: Münchner geologische Hefte : A, Allgemeine Geologie 32
    Classification:
    Geochemistry
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  • 38
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 11/M 03.0434
    In: Springer series in materials science
    Type of Medium: Monograph available for loan
    Pages: XIII, 368 S.
    ISBN: 3540664963
    Series Statement: Springer series in materials science 43
    Classification:
    Geochemistry
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  • 39
    Call number: S 91.0379(11)
    In: Hallesches Jahrbuch für Geowissenschaften. Reihe B, Geologie, Paläontologie, Mineralogie. Beiheft
    Type of Medium: Series available for loan
    Pages: 136 S.
    Series Statement: Hallesches Jahrbuch für Geowissenschaften : Reihe B, Geologie, Paläontologie, Mineralogie : Beiheft 11
    Classification:
    Geochemistry
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  • 40
    Call number: 21/STR 00/21
    In: Scientific technical report
    Type of Medium: GFZ publications
    Pages: III, 116, A-13 S.
    Series Statement: Scientific technical report / Geoforschungszentrum Potsdam 00/21
    Classification:
    Geochemistry
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  • 41
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 02.0543
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: The scientific discoveries that have been made with noble gas geochemistry are of such a profound and fundamental nature that earth science textbooks should be full of examples. Surprisingly, this really is not so. The "first discoveries" include presolar components in our _ solar system, extinct radionuclides, primordial volatiles in the Earth, the degassing history of Mars, secular changes in the solar wind, reliable present day mantle degassing fluxes, the fluxes of extraterrestrial material to Earth, groundwater paleotemperatures and the ages of the oldest landscapes on Earth. Noble gas geochemistry has scored so many such "firsts" or "home runs" that it should permeate a lot of earth science thinking and teaching. Yet rather surprisingly it does not. Noble gas geochemistry also is a broader and more versatile field than almost any other area of geochemistry. It pervades cosmochemistry, Earth sciences, ocean sciences, climate studies and environmental sciences. Yet most modern Earth, planetary and environmental science departments do not consider noble gas geochemistry to be at the top of their list in terms of hiring priorities these days. Furthermore, with the exception of Ar geochronologists, noble gas geochemists are a surprisingly rare breed. Why is the above the case? Perhaps the reasons lie in the nature of the field itself. First, although noble gas geochemists work on big problems, the context of their data is often woefully under-constrained so that it becomes hard to make progress beyond the first order fundamental discoveries. Noble gas data are often difficult to interpret. Although some concepts are straightforward and striking in their immediate implications (e.g. mantle 3He in the oceans), others are to this day shrouded in lack of clarity. The simple reason for this is that in many situations it is only the noble gases that offer any real insights at all and the context of other constraints simply does not exist. Some examples of the big issues being addressed by noble gases are as follows and I have deliberately posed these as major unresolved questions that only exist because noble gas geochemistry has opened windows through which to view large-scale issues and processes that otherwise would be obscure. (1) Is the presolar noble gas component present in a tiny fraction of submicroscopic meteoritic C or is it ubiquitously distributed? (2) How did solar noble gases get incorporated into the Earth? (3) How did solar noble gases survive the protracted accretion of the Earth via giant impacts? (4) What is the origin of the noble gas pattern in the Earth's atmosphere? (5) Why are the Earth and Mars almost opposites in terms of the relative isotopic differences between atmosphere and mantle? (6) What is the Eresent source of Earth's primordial helium? Can we ignore the core? (7) What is the 2~e/ 2Ne of the mantle, how was it acquired and why is it different from the atmosphere? (8) How does one reconcile the stronlJ fractionation in terrestrial Xe with data for other noble gases? (9) How much radiogenic Ar should the Earth have? How well do we know KIU? (10) Are the light isotopes of Xe the same in the mantle and the atmosphere? If not, why not? (11) How are noble gases transported through the creeping solid earth? (12) How does one explain the heat - helium paradox? (13) How incompatible are the noble gases during melting? (14) How are atmospheric components incorporated into volcanic samples? (15) How are the excess air components incorporated into groundwater? (16) Why are continental noble gas paleotemperature records offset from oceanic temperature records? Noble gas data tell us that the Earth and solar system represent very complex environments. When we make our simple first order conclusions and models we are only at the tip of the iceberg of discoveries that are needed to arrive at a thorough understanding of the behavior of volatiles in the solar system. Who wants to hear that things are complicated? Who wants to hire in a field that will involve decades of data acquisition and analysis in order to sort out the solar system? Sadly, too few these days. This is the stuff of deep scientific giants and bold, technically difficult long-term research programs. It is not for those who prefer superficiality and quick, glamorous, slick answers. Noble gas geochemists work in many areas where progress is slow and difficult even though the issues are huge. This probably plays a part in the limited marketability of noble gas geochemistry to the nonspecialist. Second, noble gases is a technically difficult subject. That is, noble gas geochemists need to be adept 11t technique development and this has to include skills acquired through innovation in the lab. Nobody can learn this stuff merely with a book or practical guide. Reading Zen and the Art of Motorcycle Maintenance (by Robert Pirsig) would give you a clearer picture. This magnificent MSA-GS volume is going to be enormously useful but on its own it won't make anybody into a noble gas geochemist. Although the mass spectrometry principles are not complex, the tricks involved in getting better data are often self taught or passed on by working with individuals who themselves are pushing the boundaries further. Furthermore, much of the exciting new science is linked with technical developments that allow us to move beyond the current measurement capabilities. Be they better crushing devices, laser resonance time of flight, multiple collection or compressor sources - the technical issues are central to progress. Lastly, noble gas geochemists need a broad range of other skills in order to make progress. They have to be good at mass spectrometry as already stated. However, nowadays they also need to be able to understand fields as different as mantle geochemistry, stellar evolution, cosmochemistry, crustal fluids, oceanography and glaciology. They are kind of "Renaissance" individuals. Therefore, if you are thinking broadly about hiring scientists who love science and stand a good chance of making a major difference to our understanding of the solar system, earth and its environment - I would recommend you hire a really good noble gas geochemist. However, the results may take a while. If you want somebody who will crank out papers at high speed and quickly increase the publication numbers of your department then you may need to think about somebody else. The two are not mutually exclusive but think hard about what is really important. There was no short course associated with this volume, although an attempt was undertaken to get the volume printed in time for the V. M. Goldschmidt conference in Davos, Switzerland (mid-August 2002) at which there was a major symposium on noble gases.
    Type of Medium: Monograph available for loan
    Pages: xviii, 844 S.
    ISBN: 0-939950-59-6 , 978-0-939950-59-1
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 47
    Classification:
    Geochemistry
    Note: Chapter 1. Preface: Noble Gases – Noble Science by Alex N. Halliday, p. 1 - 20 Chapter 2. An Overview of Noble Gas Geochemistry and Cosmochemistry by Donald Porcelli, Chris J. Ballentine, Rainer Wieler, p. 21 - 70 Chapter 3. Noble Gases in the Solar System by Rainer Wieler, p. 71 - 100 Chapter 4. Noble Gases in the Moon and Meteorites: Radiogenic Components and Early Volatile Chronologies by Timothy D. Swindle, p. 101 - 124 Chapter 5. Cosmic-Ray-Produced Noble Gases in Meteorites by Rainer Wieler, p. 125 - 170 Chapter 6. Martian Noble Gases by Timothy D. Swindle, p. 171 - 190 Chapter 7. Origin of Noble Gases in the Terrestrial Planets by Robert O. Pepin, Donald Porcelli, p. 191 - 246 Chapter 8. Noble Gas Isotope Geochemistry of Mid-Ocean Ridge and Ocean Island Basalts: Characterization of Mantle Source Reservoirs by David W. Graham, p. 247 - 318 Chapter 9. Noble Gases and Volatile Recycling at Subduction Zones by David R. Hilton, Tobias P. Fischer, Bernard Marty, p. 319 - 370 Chapter 10. The Storage and Transport of Noble Gases in the Subcontinental Lithosphere by Tibor J. Dunai, Donald Porcelli, p. 371 - 410 Chapter 11. Models for the Distribution of Terrestrial Noble Gases and the Evolution of the Atmosphere by Donald Porcelli, Chris J. Ballentine, p. 411 - 480 Chapter 12. Production, Release and Transport of Noble Gases in the Continental Crust by Chris J. Ballentine, Pete G. Burnard, p. 481 - 538 Chapter 13. Tracing Fluid Origin, Transport and Interaction in the Crust by Chris J. Ballentine, Ray Burgess, Bernard Marty, p. 539 - 614 Chapter 14. Noble Gases in Lakes and Ground Waters by Rolf. Kipfer, Werner. Aeschbach-Hertig, Frank. Peeters, Martin. Stute, p. 615 - 700 Chapter 15. Noble Gases in Ocean Waters and Sediments by Peter Schlosser, Gisela Winckler, p. 701 - 730 Chapter 16. Cosmic-Ray-Produced Noble Gases in Terrestrial Rocks: Dating Tools for Surface Processes by Samuel Niedermann, p. 731 - 784 Chapter 17. K-Ar and Ar-Ar Dating by Simon P. Kelley, p. 785 - 818 Chapter 18. (U-Th)/He Dating: Techniques, Calibrations, and Applications by Kenneth A. Farley, p. 819 - 844
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  • 42
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0059
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This book has been several years in the making, under the experienced and careful oversight of Ed Grew (University of Maine), who edited (with Larry Anovitz) a similar, even larger volume in 1996: Boron: Mineralogy, Petrology, and Geochemistry (RiMG Vol. 33, reprinted with updates and corrections, 2002). Many of the same reasons for inviting investigators to contribute to a volume on B apply equally to a volume on Be. Like B, Be poses analytical difficulties, and it has been neglected in many studies. However, with recent improvements in analytical technology, interest in Be and its cosmogenic isotopes has increased greatly. Chapter 1 (Grew) is an overview of Be studies in the earth sciences backed by an extensive reference list, and an annotated list of the 110 mineral species reported to contain essential Be as of 2002, together with commentary on their status. A systematic classification of Be minerals based on their crystal structure is presented in Chapter 9 (Hawthorne and Huminicki), while analysis of these minerals by the secondary ion mass spectroscopy is the subject of Chapter 8 (Hervig). Chapter 13 (Franz and Morteani) reviews experimental studies of systems involving Be. Chapter 2 (Shearer) reviews the behavior of Be in the Solar System, with an emphasis on meteorites, the Moon and Mars, and the implications of this behavior for the evolution of the solar system. Chapter 3 (Ryan) is an overview of the terrestrial geochemistry of Be, and Chapter 7 (Vesely, Norton, Skrivan, Majer, Kr·m, Navr·til, and Kaste) discusses the contamination of the environment by this anthropogenic toxin. The cosmogenic isotopes Be-7 and Be-10 have found increasing applications in the Earth sciences. Chapter 4 (Bierman, Caffee, Davis, Marsella, Pavich, Colgan and Mickelson) reports use of the longer lived Be-10 to assess erosion rates and other surficial processes, while Chapter 5 (Morris, Gosse, Brachfeld and Tera) considers how this isotope can yield independent temporal records of geomagnetic field variations for comparison with records obtained by measuring natural remnant magnetization, be a chemical tracer for processes in convergent margins, and can date events in Cenozoic tectonics. Chapter 6 (Kaste, Norton and Hess) reviews applications of the shorter lived isotope Be-7 in environmental studies. Beryllium is a lithophile element concentrated in the residual phases of magmatic systems. Residual phases include acidic plutonic and volcanic rocks, whose geochemistry and evolution are covered, respectively, in Chapters 11 (London and Evensen) and 14 (Barton and Young), while granitic pegmatites, which are well-known for their remarkable, if localized, Be enrichments and a wide variety of Be mineral assemblages, are reviewed in Chapter 10 (Cerny). Not all Be concentrations have obvious magmatic affinities; for example, one class of emerald deposits results from Be being introduced by heated brines (Chapters 13; 14). Pelitic rocks are an important reservoir of Be in the Earth's crust and their metamorphism plays a critical role in recycling of Be in subduction zones (Chapter 3), eventually, anatectic processes complete the cycle, providing a source of Be for granitic rocks (Chapters 11 and 12).
    Type of Medium: Monograph available for loan
    Pages: XII, 691 S.
    ISBN: 0-939950-62-6 , 978-0-939950-62-1
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 50
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. Mineralogy, Petrology and Geochemistry of Beryllium: An Introduction and List of Beryllium Minerals by Edward S. Grew, p. 1 - 76 Chapter 2. Behavior of Beryllium During Solar System and Planetary Evolution: Evidence from Planetary Materials by Charles K. Shearer, p. 77 - 120 Chapter 3. Trace-Element Systematics of Beryllium in Terrestrial Materials by Jeffrey G. Ryan, p. 121 - 146 Chapter 4. Rates and Timing of Earth Surface Processes From In Situ-Produced Cosmogenic Be-10 by Paul R. Bierman, Marc W. Caffee, P. Thompson Davis, Kim Marsella, Milan Pavich, Patrick Colgan, and David Mickelson, p. 147 - 206 Chapter 5. Cosmogenic Be-10 and the Solid Earth: Studies in Geomagnetism, Subduction Zone Processes, and Active Tectonics by Julie D. Morris, John Gosse, Stefanie Brachfeld, and Fouad Tera, p. 207 - 270 Chapter 6. Environmental Chemistry of Beryllium-7 by James M. Kaste, Stephen A. Norton, and Charles T. Hess, p. 271 - 290 Chapter 7. Environmental Chemistry of Beryllium by J. Vesely, S. A. Norton, P. Skrivan, V. Majer, P. Kram, T. Navr·til, and J. M. Kaste, p. 291 - 318 Chapter 8. Beryllium Analyses by Secondary Ion Mass Spectrometry by Richard L. Hervig, p. 319 - 332 Chapter 9. The Crystal Chemistry of Beryllium by Frank C. Hawthorne and Danielle M. C. Huminicki, p. 333 - 404 Chapter 10. Mineralogy of Beryllium in Granitic Pegmatites by Petr Cerny, p. 405 - 444 Chapter 11. Beryllium in Silicic Magmas and the Origin of Beryl-Bearing Pegmatites by David London and Joseph M. Evensen, p. 445 - 486 Chapter 12. Beryllium in Metamorphic Environments (Emphasis on Aluminous Compositions) by Edward S. Grew, p. 487 - 550 Chapter 13. Be-Minerals: Synthesis, Stability, and Occurrence in Metamorphic Rocks by Gerhard Franz and Giulio Morteani, p. 551 - 590 Chapter 14. Non-pegmatitic Deposits of Beryllium: Mineralogy, Geology, Phase Equilibria and Origin by Mark D. Barton and Steven Young, p. 591 - 691
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  • 43
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 03.0010
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Several years ago, John Rakovan and John Hughes (colleagues at Miami of Ohio), and later Matt Kohn (at South Carolina), separately proposed short courses on phosphate minerals to the Council of the Mineralogical Society of America (MSA). Council suggested that they join forces. Thus this volume, Phosphates: Geochemical, Geobiological, and Materials Importance, was organized. It was prepared in advance of a short course of the same title, sponsored by MSA and presented at Golden, Colorado, October 25-27. We are pleased to present this volume entitled Phosphates: Geochemical, Geobiological and Materials Importance. Phosphate minerals are an integral component of geological and biological systems. They are found in virtually all rocks, are the major structural component of vertebrates, and when dissolved are critical for biological activity. This volume represents the work of many authors whose research illustrates how the unique chemical and physical behavior of phosphate minerals permits a wide range of applications that encompasses phosphate mineralogy, petrology, biomineralization, geochronology, and materials science. While diverse, these fields are all linked structurally, crystal-chemically and geochemically. As geoscientists turn their attention to the intersection of the biological, geological, and material science realms, there is no group of compounds more germane than the phosphates. The chapters of this book are grouped into five topics: Mineralogy and Crystal Chemistry, Petrology, Biomineralization, Geochronology, and Materials Applications. In the first section, three chapters are devoted to mineralogical aspects of apatite, a phase with both inorganic and organic origins, the most abundant phosphate mineral on earth, and the main mineral phase in the human body. Monazite and xenotime are highlighted in a fourth chapter, which includes their potential use as solid-state radioactive waste repositories. The Mineralogy and Crystal Chemistry section concludes with a detailed examination of the crystal chemistry of 244 other naturally-occurring phosphate phases and a listing of an additional 126 minerals. In the Petrology section, three chapters detail the igneous, metamorphic, and sedimentary aspects of phosphate minerals. A fourth chapter provides a close look at analyzing phosphates for major, minor, and trace elements using the electron microprobe. A final chapter treats the global geochemical cycling of phosphate, a topic of intense, current geochemical interest. The Biomineralization section begins with a summary of the current state of research on bone, dentin and enamel phosphates, a topic that crosses disciplines that include mineralogical, medical, and dental research. The following two chapters treat the stable isotope and trace element compositions of modern and fossil biogenic phosphates, with applications to paleontology, paleoclimatology, and paleoecology. The Geochronology section focuses principally on apatite and monazite for U-ThPb, (U- Th)/He, and fission-track age determinations; it covers both classical geochronologic techniques as well as recent developments. The final section-Materials Applications-highlights how phosphate phases play key roles in fields such as optics, luminescence, medical engineering and prosthetics, and engineering of radionuclide repositories. These chapters provide a glimpse of the use of natural phases in engineering and biomedical applications and illustrate fruitful areas of future research in geochemical, geobiological and materials science. We hope all chapters in this volume encourage researchers to expand their work on all aspects of natural and synthetic phosphate compounds.
    Type of Medium: Monograph available for loan
    Pages: xv, 742 S.
    ISBN: 0-939950-60-X , 978-0-939950-60-7
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 48
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. The Crystal Structure of Apatite, Ca5(PO4)3(F,OH,Cl) by John M. Hughes and John Rakovan, p. 1 - 12 Chapter 2. Compositions of the Apatite-Group Minerals: Substitution Mechanisms and Controlling Factors by Yuanming Pana and Michael E. Fleet, p. 13 - 50 Chapter 3. Growth and Surface Properties of Apatite by John Rakovan, p. 51 - 86 Chapter 4. Synthesis, Structure and Properties of Monazite, Pretulite, and Xenotime by Lynn A. Boatner, p. 87 - 122 Chapter 5. The Crystal Chemistry of the Phosphate Minerals by Danielle M.C. Huminicki and Frank C. Hawthorne, p. 123 - 254 Chapter 6. Apatite in Igneous Systems by Philip M. Piccoli and Philip A. Candela, p. 255 - 292 Chapter 7. Apatite, Monazite, and Xenotine in Metamorphic Rocks by Frank S. Spear and Joseph M. Pyle, p. 293 - 336 Chapter 8. Electron Microprobe Analysis of REE in Apatite, Monazite and Xenotime: Protocols and Pitfalls by Joseph M. Pyle, Frank S. Spear, and David A. Wark, p. 337 - 362 Chapter 9. Sedimentary Phosphorites - An Example: Phosphoria Formation, Southeastern Idaho, U.S.A by Andrew C. Knudsen and Mickey E. Gunter, p. 363 - 390 Chapter 10. The Global Phosphorus Cycle by Gabriel M. Filippelli, p. 391 - 426 Chapter 11. Calcium Phosphate Biominerals by James C. Elliott, p. 427 - 454 Chapter 12. Stable Isotope Composition of Biological Apatite by Matthew J. Kohn and Thure E. Cerling, p. 455 - 488 Chapter 13. Trace Elements in Recent and Fossil Bone Apatite by Clive N. Trueman and Noreen Tuross, p. 489 - 522 Chapter 14. U-TH-Pb Dating of Phosphate Minerals by T. Mark Harrison, Elizabeth J. Catlos, and Jean-Marc Montel, p. 523 - 558 Chapter 15. (U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime by Kenneth A. Farley and Daniel F. Stockli, p. 559 - 578 Chapter 16. Fission Track Dating of Phosphate Minerals and the Thermochronology of Apatite by Andrew J.W. Gleadow, David X. Belton, Barry P. Kohn, and Roderick W. Brown, p. 579 - 630 Chapter 17. Biomedical Application of Apatites by Karlis A. Gross and Christopher C. Berndt, p. 631 - 672 Chapter 18. Phosphates as Nuclear Waste Forms by Rodney C. Ewing and LuMin Wang, p. 673 - 700 Chapter 19. Apatite Luminescence by Glenn A. Waychuna, p. 701 - 742
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  • 44
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: M 03.0197 ; 5/M 03.0372
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: 315 S.
    ISBN: 0875909825
    Series Statement: Geophysical monograph 124
    Classification:
    Geochemistry
    Location: Upper compact magazine
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  • 45
    Call number: 11/M 03.0009
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: This volume was produced in response to the need for a comprehensive introduction to the continually evolving state of the art of synchrotron radiation applications in low-temperature geochemistry and environmental science. It owes much to the hard work and imagination of the devoted cadre of sleep-deprived individuals who blazed a trail that many others are beginning to follow. Synchrotron radiation methods have opened new scientific vistas in the earth and environmental sciences, and progress in this direction will undoubtedly continue. The organization of this volume is as follows. Chapter 1 (Brown and Sturchio) gives a fairly comprehensive overview of synchrotron radiation applications in low temperature geochemistry and environmental science. The presentation is organized by synchrotron methods and scientific issues. It also has an extensive reference list that should prove valuable as a starting point for further research. Chapter 2 (Sham and Rivers) describes the ways that synchrotron radiation is generated, including a history of synchrotrons and a discussion of aspects of synchrotron radiation that are important to the experimentalist. The remaining chapters of the volume are organized into two groups. Chapters 3 through 6 describe specific synchrotron methods that are most useful for single-crystal surface and mineral-fluid interface studies. Chapters 7 through 9 describe methods that can be used more generally for investigating complex polyphase fine-grained or amorphous materials, including soils, rocks, and organic matter. Chapter 2 (Shearer) reviews the behavior of Be in the Solar System, with an emphasis on meteorites, the Moon and Mars, and the implications of this behavior for the evolution of the solar system. Chapter 3 (Ryan) is an overview of the terrestrial geochemistry of Be, and Chapter 7 (Vesely, Norton, Skrivan, Majer, Kr·m, Navr·til, and Kaste) discusses the contamination of the environment by this anthropogenic toxin. Chapter 3 (Fenter) presents the elementary theory of synchrotron X-ray reflectivity along with examples of recent applications, with emphasis on in situ studies of mineral-fluid interfaces. Chapter 4 (Bedzyk and Cheng) summarizes the theory of X-ray standing waves (XSW), the various methods for using XSW in surface and interfaces studies, and gives a brief review of recent applications in geochemistry and mineralogy. Chapter 5 (Waychunas) covers the theory and applications of grazing-incidence X-ray absorption and emission spectroscopy, with recent examples of studies at mineral surfaces. Chapter 6 (Hirschmugl) describes the theory and applications of synchrotron infrared microspectroscopy. Chapter 7 (Manceau, Marcus, and Tamura) gives background and examples of the combined application of synchrotron X-ray microfluorescence, microdiffraction, and microabsorption spectroscopy in characterizing the distribution and speciation of metals in soils and sediments. Chapter 8 (Sutton, Newville, Rivers, Lanzirotti, Eng, and Bertsch) demonstrates a wide variety of applications of synchrotron X-ray microspectroscopy and microtomography in characterizing earth and environmental materials and processes. Finally, Chapter 9 (Myneni) presents a review of the principles and applications of soft X-ray microspectroscopic studies of natural organic materials. All of these chapters review the state of the art of synchrotron radiation applications in low temperature geochemistry and environmental science, and offer speculations on future developments. The reader of this volume will acquire an appreciation of the theory and applications of synchrotron radiation in low temperature geochemistry and environmental science, as well as the significant advances that have been made in this area in the past two decades (especially since the advent of the third-generation synchrotron sources). We hope that this volume will inspire new users to "see the light" and pursue their research using the potent tool of synchrotron radiation.
    Type of Medium: Monograph available for loan
    Pages: XXII, 579 S.
    ISBN: 0-939950-61-8 , 978-0-939950-61-4
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 49
    Classification:
    Geochemistry
    Language: English
    Note: Chapter 1. An Overview of Synchrotron Radiation Applications to Low Temperature Geochemistry and Environmental Science by Gordon E. Brown, Jr. and Neil C. Sturchio, p. 1 - 116 Chapter 2. A Brief Overview of Synchrotron Radiation by T. K. Sham and Mark L. Rivers, p. 117 - 148 Chapter 3. X-ray Reflectivity as a Probe of Mineral-Fluid Interfaces: A User Guide by Paul A. Fenter, p. 149 - 220 Chapter 4. X-ray Standing Wave Studies of Minerals and Mineral Surfaces: Principles and Applications by Michael J. Bedzyk and Likwan Cheng, p. 221 - 266 Chapter 5. Grazing-incidence X-ray Absorption and Emission Spectroscopy by Glenn A. Waychunas, p. 267 - 316 Chapter 6. Applications of Storage Ring Infrared Spectromicroscopy and Reflection-Absorption Spectroscopy to Geochemistry and Environmental Science by Carol J. Hirschmugl, p. 317 - 340 Chapter 7. Quantitative Speciation of Heavy Metals in Soils and Sediments by Synchrotron X-ray Techniques by Alain Manceau, Matthew A. Marcus, and Nobumichi Tamura, p. 341 - 428 Chapter 8. Microfluorescence and MicrotomographyAnalyses of Heterogeneous Earth and Environmental Materials by Stephen R. Sutton, Paul M. Bertsch, Matthew Newville, Mark Rivers, Antonio Lanzirotti and Peter Eng, p. 429 - 484 Chapter 9. Soft X-ray Spectroscopy and Spectromicroscopy Studies of Organic Molecules in the Environment by Satish C. B. Myneni, p. 485 - 579
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  • 46
    Call number: M 04.0177
    Type of Medium: Monograph available for loan
    Pages: XVII, 836 S.
    ISBN: 3798512329
    Classification:
    Geochemistry
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  • 47
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 04.0341
    In: Reviews in mineralogy & geochemistry
    Description / Table of Contents: Our understanding of rock forming geological processes and thereby of geodynamic processes depends largely on a sound basis of knowledge of minerals. Due to the application of new analytical techniques, the number of newly discovered minerals increases steadily, and what used to be a simple mineral may have turned into a complex group. A continuous update is necessary, and the Reviews in Mineralogy and Geochemistry series excellently fulfills this requirement. The epidote minerals have not yet been covered and we felt that this gap should be filled. The epidote mineral group consists of important rock-forming minerals such as clinozoisite and epidote, geochemical important accessory minerals such as allanite, and minerals typical for rare bulk compositions such as hancockite. Zoisite, the orthorhombic polymorph of clinozoisite, is included here because of its strong structural and paragenetic similarity to the epidote minerals. Epidote minerals occur in a wide variety of rocks, from near-surface conditions up to high- and ultrahigh-pressure metamorphic rocks and as liquidus phases in magmatic systems. They can be regarded as the low-temperature and high-pressure equivalent of Ca-rich plagioclase, and thus are equally important as this feldspar for petrogenetic purposes. In addition, they belong to the most important Fe3+ bearing minerals, and give important information about the oxygen fugacity and the oxidation state of a rock. Last but not least, they can incorporate geochemically relevant minor and trace elements such as Sr, Pb, REE, V, and Mn. The epidote minerals are undoubtedly very important from a petrogenetic and geochemical point of view, and have received a lot of attention in the last years from several working groups in the field of experimental studies and spectroscopic work. As a result, the thermodynamic database of epidote minerals has been significantly enlarged during the last decade. Recent studies have revealed the importance of zoisite in subduction zone processes as a carrier of H2O and suggested zoisite to be the main H2O source in the pressure interval between about 2.0 and 3.0 GPa. Many studies have shown that an understanding of trace element geochemical processes in high-pressure rocks is impossible without understanding the geochemical influence of the epidote minerals. Recent advances in microanalytical techniques have also shown that epidote minerals record detailed information on their geological environment. W. A. Deer, R. A. Howie and J. Zussmann edited the last comprehensive review on this mineral group almost 20 years ago in 1986. In 1990, on the occasion of the 125th anniversary of the discovery of the famous Knappenwand locality in the Tauern/Austria, an epidote conference was held in Neukirchen/Austria organized by the Austrian Mineralogical Society by V. Höck and F. Koller. In 1999, there was a special symposium at the EUG 10 in Strasbourg, convened by R. Gieré and F. Oberli, entitled Recent advances in studies of the epidote group that highlighted the relevance of the epidote minerals for Earth science. However, there are many open questions in the community regarding the epidote minerals and there is a need for a new overview that brings together the recent knowledge on this interesting group of minerals. The present volume of the Reviews in Mineralogy and Geochemistry reviews the current state of knowledge on the epidote minerals with special emphasis on the advances that were made since the comprehensive review of Deer et al. (1986). We hope that it will serve to outline the open questions and direction of future research. In the Introduction, we review the structure, optical data and crystal chemistry of this mineral group, all of which form the basis for understanding much of the following material in the volume. In addition, we provide some information on special topics, such as morphology and growth, deformation behavior, and gemology. Thermodynamic properties (Chapter 2, Gottschalk), the spectroscopy of the epidote minerals (Chapter 3, Liebscher) and a review of the experimental studies (Chapter 4, Poli and Schmidt) constitute the first section of chapters. These fields are closely related, and all three chapters show the significant progress over the last years, but that some of the critical questions such as the problem of miscibility and miscibility gaps are still not completely solved. This section concludes with a review of fluid inclusion studies (Chapter 5, Klemd), a topic that turned out to be of large interest for petrogenetic interpretation, and leads to the description of natural epidote occurrences in the second section of the book. These following chapters review the geological environments of the epdiote minerals, from low temperature in geothermal fields (Chapter 6, Bird and Spieler), to common metamorphic rocks (Chapter 7, Grapes and Hoskin) and to high- and ultrahigh pressure (Chapter 8, Enami, Liou and Mattinson) and the magmatic regime (Chapter 9, Schmidt and Poli). Allanite (Chapter 10, Gieré and Sorensen) and piemontite (Chapter 11, Bonazzi and Menchetti), on which a large amount of information is now available, are reviewed in separate chapters. Finally trace element (Chapter 12, Frei, Liebscher, Franz and Dulski) and isotopic studies, both stable and radiogenic isotopes (Chapter 13, Morrison) are considered. We found it unavoidable that there is some overlap between individual chapters. This is an inherited problem in a mineral group such as the epidote minerals, which forms intensive solid solutions between the major components of rock forming minerals as well as with trace elements.
    Type of Medium: Monograph available for loan
    Pages: XVII, 628 S. , zahlr. Ill., graph. Darst
    ISBN: 0-939950-68-5 , 978-0-939950-68-3
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy & geochemistry 56
    Classification:
    Geochemistry
    Note: Chapter 1. Physical and Chemical Properties of the Epidote Minerals ≠ An Introduction by Gerhard Franz and Axel Liebscher, p. 1 - 82 Chapter 2. Thermodynamic Properties of Zoisite, Clinozoisite and Epidote by Matthias Gottschalk, p. 83 - 124 Chapter 3. Spectroscopy of Epidote Minerals by Axel Liebscher, p. 125 - 170 Chapter 4. Experimental Subsolidus Studies on Epidote Minerals by Stefano Poli and Max W. Schmidt, p. 171 - 196 Chapter 5. Fluid Inclusions in Epidote Minerals and Fluid Development in Epidote-Bearing Rocks by Reiner Klemd, p. 197 - 234 Chapter 6. Epidote in Geothermal Systems by Dennis K. Bird and Abigail R. Spieler, p. 235 - 300 Chapter 7. Epidote Group Minerals in Low≠Medium Pressure Metamorphic Terranes by Rodney M. Grapes and Paul W. O. Hoskin, p. 301 - 346 Chapter 8. Epidote Minerals in High P/T Metamorphic Terranes: Subduction Zone and High- to Ultrahigh-Pressure Metamorphism by M. Enami, J.G. Liou, and C. G. Mattinson, p. 347 - 398 Chapter 9. Magmatic Epidote by Max W. Schmidt and Stefano Poli, p. 399 - 430 Chapter 10. Allanite and Other REE-Rich Epidote-Group Minerals by Reto Gieré and Sorena S. Sorensen, p. 431 - 494 Chapter 11. Manganese in Monoclinic Members of the Epidote Group: Piemontite and Related Minerals by by Paola Bonazzi and Silvio Menchetti, p. 495 - 552 Chapter 12. Trace Element Geochemistry of Epidote Minerals by by Dirk Frei, Axel Liebscher, Gerhard Franz, and Peter Dulski, p. 553 - 606 Chapter 13. Stable and Radiogenic Isotope Systematics in Epidote Group Minerals by Jean Morrison, p. 607 - 628
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  • 48
    Series available for loan
    Series available for loan
    Braunschweig : Inst. für Geowiss. der Techn. Univ.
    Associated volumes
    Call number: S 93.0918(26)
    In: Braunschweiger geowissenschaftliche Arbeiten
    Type of Medium: Series available for loan
    Pages: XXII, 209 S. , Ill., graph. Darst., Kt.
    Series Statement: Braunschweiger geowissenschaftliche Arbeiten 26
    Classification:
    Geochemistry
    Note: Zugl.: Braunschweig, Techn. Univ., Diss., 2003
    Location: Lower compact magazine
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  • 49
    Call number: S 90.0002(1685)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, 54 S.
    ISBN: 0607990546
    Series Statement: U.S. Geological Survey professional paper 1685
    Classification:
    Geochemistry
    Location: Lower compact magazine
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  • 50
    Series available for loan
    Series available for loan
    Bonn : Alfred-Wegener-Stiftung
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    Call number: S 99.0056(5/01)
    In: Terra nostra
    Type of Medium: Series available for loan
    Pages: 90 S.
    Series Statement: Terra Nostra 5/01
    Classification:
    Geochemistry
    Location: Lower compact magazine
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  • 51
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 4/M 04.0552
    In: Lecture notes in earth sciences
    Description / Table of Contents: Contents: General Significance of Geochemical Models of Hydrothermal Systems.- Concepts, Classification and Chemistry of Geothermal Systems.- Theory of Chemical Modeling.- Specific Features of Coupled Fluid Flow and Chemical Reaction.- Fossil Hydrothermal Systems.- Recent Hydrothermal Systems.- Reservoir Management.
    Type of Medium: Monograph available for loan
    Pages: XI, 261 S. , Ill., graph. Darst., Kt.
    ISBN: 3540203389
    Series Statement: Lecture notes in earth sciences 103
    Classification:
    Geochemistry
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  • 52
    Call number: M 05.0481
    Description / Table of Contents: Contents: Physical properties of water. Near-critical behavior of aqueous systems.Aqueous solubility of volatile nonelectrolytes. Calculation of standard thermodynamic properties of aqueous electrolytes and nonelectrolytes.Hydrothermal solution structure: experiments and computer. Vapor-liquid equilibrium involving aqueous, binary nonelectrolytes. Binary homogeneous nucleation in selected aqueous vapor mixtures. Solute concentration effects on reaction thermodynamics in steam cycle fluids. Stable isotope partitioning in aqueous and hydrothermal systems to elevated temperatures. Transport properties in high temperature and pressure ionic solutions. Electrochemical processes in high-temperature aqueous solutions. Partitioning of electrolytes to steam and their solubilities in steam. Dissociation equilibria of weak acids and bases. Solubility and surface adsorption characteristics of metal oxides. Phase equilibria of water-salt systems at high temperatures and pressures. Kinetics and mechanisms of hydrothermal organic reactions. Water chemistry in commercial water-steam cycles. Hydrothermal synthesis of ceramic materials.
    Type of Medium: Monograph available for loan
    Pages: XII, 753 S. , Ill., graph. Darst.
    Edition: 1st ed.
    ISBN: 0125444613
    Classification:
    Geochemistry
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    Monograph available for loan
    Monograph available for loan
    Weinheim [u.a.] : Wiley-VCH
    Call number: 17/M 05.0598
    Type of Medium: Monograph available for loan
    Pages: XII, 940 S. , Ill., graph. Darst.
    Edition: 3., völlig überarb. und erw. Aufl.
    ISBN: 3527287027
    Classification:
    Geochemistry
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    Call number: 11/M 05.0587
    In: Texts on crystallography
    Type of Medium: Monograph available for loan
    Pages: XIV, 265 S. , Ill., graph. Darst.
    Edition: 1st publ.
    ISBN: 019850618X
    Series Statement: IUCr texts on crystallography 6
    Classification:
    Geochemistry
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