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  • Printed Books(GFZ-OPAC)  (94)
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  • 1
    Call number: 9/M 07.0421(350)
    In: Geological Society special publication
    Description / Table of Contents: This volume brings together a collection of papers that summarize current ideas and recent progress in the study of granite-related mineralization systems. They provide a combination of field, experimental and theoretical studies. Papers are grouped according to the main granite-related ore systems: granite-pegmatite, skarn and greisen-veins, porphyry, orogenic gold, intrusion-related, epithermal and porphyry-related gold and base metal, iron oxide copper gold (IOCG), and special case studies. The studies provide a broad spread in terms of both space and time, highlighting granite-related ore deposits from Europe (Russia, Sweden, Croatia and Turkey), the Middle East (Iran), Asia (Japan and China) and South America (Brazil and Argentina) and spanning rocks from Palaeoproterozoic to Miocene in age.
    Type of Medium: Monograph available for loan
    Pages: 192 S. : Ill., graph. Darst., Kt.
    ISBN: 9781862393219
    Series Statement: Geological Society special publication 350
    Classification:
    Mineralogy
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  • 2
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 16/M 94.0515
    In: Springer series in optical sciences
    Type of Medium: Monograph available for loan
    Pages: XIII, 545 S.
    Edition: 3rd ed.
    ISBN: 3540568492
    Series Statement: Springer series in optical sciences vol. 36
    Classification:
    Mineralogy
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: M 95.0054 / Regal 11
    In: Reviews in mineralogy
    Description / Table of Contents: Volatile components, by which we mean those magma constituents which typically prefer to occur in the gaseous or super-critical fluid state, may influence virtually every aspect of igneous petrology. The study of volatile-bearing systems, both in nature and in the laboratory, has far exceeded the relative abundances of these components in igneous rocks, yet in many ways the words of Bowen (1928) are still broadly applicable: " ... to many petrologists a volatile component is exactly like a Maxwell demon; it does just what one may wish it to do." (Bowen, 1928, p. 282) What we hope to show in this volume are some areas of progress in understanding the behavior of magmatic volatiles and their influence on a wide variety of geological phenomena; in doing this it also becomes apparent that there remain many questions outstanding. The range of topics we have tried to cover is broad, going from atomisticscale aspects of volatile solubility mechanisms and attendant effects on melt physical properties, to the chemistry of volcanic gases and the concentrations of volatiles in magmas, to the global geochemical cycles of volatiles. The reader should quickly see that much progress has been made since Bowen voiced his concerns about Maxwell demons, but like much scientific progress, answers to old questions have prompted even greater numbers of new questions. The Voltiles in Magmas course was organized and transpired at the Napa Valley Sheraton Hotel in California, December 2-4, 1994, just prior to the Fall Meetings of the American Geophysical Union in San Francisco.
    Type of Medium: Monograph available for loan
    Pages: xvii, 517 S.
    ISBN: 0-939950-36-7 , 978-0-939950-36-2
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 30
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Volcanic-Gas Studies: Methods, Results, and Applications by Robert B. Symonds, William I. Rose, Gregg J. S. Bluth, and Terrence M. Gerlach, p. 1 - 66 Chapter 2. Analytical Methods for Volatiles in Glasses by Phillip D. Ihinger, Richard L. Hervig, and Paul F. McMillan, p. 67 - 122 Chapter 3. Development of the Burnham Model for Prediction of H2O Solubility in Magmas by C. Wayne Burnham, p. 123 - 130 Chapter 4. Water Solubility and Speciation Models by Paul F. McMillan, p. 131 - 156 Chapter 5. Experimental Studies of Carbon Dioxide in Silicate Melts: Solubility, Speciation, and Stable Carbon Isotope Behavior by Jennifer G. Blank, and Richard A. Brooker, p. 157 - 186 Chapter 6. Application of Experimental Results to C-O-H Species in Natural Melts by John R. Holloway and Jennifer G. Blank, p. 187 - 230 Chapter 7. Solubilities of Sulfur, Noble Gases, Nitrogen, Chlorine, and Fluorine in Magmas by Michael R. Carroll and James D. Webster, p. 231 - 280 Chapter 8. Pre-Eruptive Volatile Contents of Magmas by Marie C. Johnson, Alfred T. Anderson, Jr., and Malcolm J. Rutherford, p. 281 - 330 Chapter 9. The Effect of H2O, CO2 and F on the Density and Viscosity of Silicate Melts by Rebecca A. Lange, p. 331 - 370 Chapter 10. Diffusion in Volatile-Bearing Magmas by E. Bruce Watson, p. 371 - 412 Chapter 11a. Physical Aspects of Magmatic Degassing I. Experimental and Theoretical Constraints on Vesiculation by R. Stephen J. Sparks, Jenni Barclay, Claude Jaupart, Heidy M. Mader, and J. C. Phillips, p. 413 - 446 Chapter 11b. Physical Aspects of Magmatic Degassing II. Constraints on Vesiculation Processes from Textural Studies of Eruptive Products by Katherine V. Cashman, and Margaret T. Mangan, p. 447 - 478 Chapter 12. Earth Degassing and Large-Scale Geochemical Cycling of Volatile Elements by Albert Jambon, p. 479 - 518
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  • 4
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer Acad. Publishers
    Associated volumes
    Call number: 11/M 95.0325
    In: International tables for crystallography
    Type of Medium: Monograph available for loan
    Edition: 4th, revised ed
    ISBN: 0792329503
    Classification:
    Mineralogy
    Language: English
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  • 5
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge Univ. Pr.
    Associated volumes
    Call number: M 95.0470 ; 11/M 93.0961
    In: Cambridge topics in mineral physics and chemistry
    Type of Medium: Monograph available for loan
    Pages: XXIII, 551 S. : graph. Darst.
    Edition: 2nd ed.
    ISBN: 0521430771
    Series Statement: Cambridge topics in mineral physics and chemistry 5
    Classification:
    Mineralogy
    Language: English
    Location: Upper compact magazine
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  • 6
    Call number: 11/M 95.0041
    Type of Medium: Monograph available for loan
    Pages: 215 S.
    Edition: 3. Aufl., 61.-80. Tsd.
    ISBN: 3440040739
    Series Statement: Kosmos-Naturführer
    Classification:
    Mineralogy
    Language: German
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  • 7
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Chapman & Hall
    Associated volumes
    Call number: 11/M 95.0458 ; M 95.0459 ; M 95.0453
    In: The Mineralogical Society series
    Type of Medium: Monograph available for loan
    Pages: xi, 419 S.
    ISBN: 0412551004
    Series Statement: Mineralogical Society series 6
    Classification:
    Mineralogy
    Language: English
    Location: Reading room
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 8
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 96.0028 ; 11/M 96.0038
    In: Reviews in mineralogy
    Description / Table of Contents: The Mineralogical Society of America sponsored a short course for which this was the text at Stanford University December 9 and 10, 1995, preceding the Fall Meeting of the American Geophysical Union and MSA in San Fransisco, with about 100 professionals and graduate students in attendance. A silicate melt phase is the essential component of nearly all igneous processes, with dramatic consequences for the properties of the Earth's interior. Throughout Earth history and continuing to the present day, silicate melts have acted as transport agents in the chemical and physical differentiation of the Earth into core, mantle and crust. The occurrence of such magmatic processes leads to the definition of our planet as "active," and the resulting volcanism has a profound impact on the Earth's atmosphere, hydrosphere and biosphere. Although near-surface melts are observed directly during volcanic eruptions, the properties of magmas deep within the Earth must be characterized and constrained by laboratory experiments. Many of these experiments are designed to aid in developing an atomic level understanding of the structure and dynamics of silicate melts under the P- T conditions of the Earth's crust and mantle, which will make extrapolation from the laboratory results to the behavior of natural magmas as reliable as possible. Silicate melts are also the archetypal glass-forming materials. Because of the ready availability of raw materials, and the ease with which molten silicates can be vitrified, commercial "glass" has necessarily implied a silicate composition, over most of the history of glass technology. The properties of the melt, or "slag" in metallurgical extractions, determine the nature of the glass formed, and the needs of the glass industry have provided much of the impetus for understanding the structure-property relations of molten silicates as well as for the glasses themselves. It is now recognized that any liquid might become glassy, if cooled rapidly enough, and understanding the thermodynamic and kinetic aspects of the glass transition, or passage between the liquid and glassy states of matter, has become a subject of intense interest in fundamental physics and chemistry. Glasses have also been studied in many geochemical investigations, often as substitutes for the high temperature melts, with the results being extrapolated to the liquid state. In many cases, in situ techniques for direct investigation of these refractory systems have only recently become available. Much valuable information concerning the melt structure has been gleaned from such studies. Nevertheless, there are fundamental differences between the liquid and glassy states. In liquids, the structure becomes progressively more disordered with increasing temperature, which usually gives rise to major changes in all thermodynamic properties and processes. These changes must, in general, be investigated directly by in situ studies at high temperature. Studies of glass only represent a starting point, which reflect a frozen image of the melt "structure" at the glass transition temperature. This is generally hundreds of degrees below the near-liquidus temperatures of greatest interest to petrologists. Since the early 1980s, a much deeper understanding of the structure, dynamics, and properties of molten silicates has been developed within the geochemical community, applying techniques and concepts developed within glass science, extractive metallurgy and liquid state physics. Some of these developments have far-reaching implications for igneous petrology. The purpose of this Short Course and volume is to introduce the basic concepts of melt physics and relaxation theory as applied to silicate melts, then to describe the current state of experimental and computer simulation techniques for exploring the detailed atomic structure and dynamic processes which occur at high temperature, and finally to consider the relationships between melt structure, thermodynamic properties and rheology within these liquids. These fundamental relations serve to bridge the extrapolation from often highly simplified melt compositions studied in the laboratory to the multicomponent systems found in nature. This volume focuses on the properties of simple model silicate systems, which are usually volatile-free. The behavior of natural magmas has been summarized in a previous Short Course volume (Nicholls and Russell, editors, 1990: Reviews in Mineralogy, Vol. 24), and the effect of volatiles on magmatic properties in yet another (Carroll and Holloway, editors, 1994: Vol. 30). In the chapters by Moynihan, by Webb and Dingwell, and by Richet and Bottinga, the concepts of relaxation and the glass transition are introduced, along with techniques for studying the rheology of silicate liquids, and theories for understanding the transport and relaxation behavior in terms of the structure and thermodynamic properties of the liquid. The chapter by Dingwell presents applications of relaxation-based studies of melts in the characterization of their properties. Chapters by Stebbins, by Brown, Farges and Calas, and by McMillan and Wolf present the principal techniques for studying the melt structure and atomic scale dynamics by a variety of spectroscopic and diffraction methods. Wolf and McMillan summarize our current understanding of the effects of pressure on silicate glass and melt structure. Chapters by Navrotsky and by Hess consider the thermodynamic properties and mixing relations in simple and multicomponent aluminosilicate melts, both from a fundamental structural point of view and empirical chemical models which can be conveniently extrapolated to natural systems. The chapter by Chakraborty describes the diffusivity of chemical species in silicate melts and glasses, and the chapter by Poole, McMillan and Wolf discusses the application of computer simulation methods to understanding the structure and dynamics of molten silicates. The emphasis in this volume is on reviewing the current state of knowledge of the structure, dynamics and physical properties of silicate melts, along with present capabilities for studying the molten state under conditions relevant to melting within the Earth, with the intention that these techniques and results can then be applied to understanding and modeling both the nature of silicate melts and the role of silicate melts in nature.
    Type of Medium: Monograph available for loan
    Pages: xv, 616 S.
    ISBN: 0-939950-39-1 , 978-0-939950-39-3
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 32
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Structural Relaxation and the Glass Transition by Cornelius T. Moynihan, p. 1 - 20 Chapter 2. Relaxation in Silicate Melts: Some Applications by Donald B. Dingwell, p. 21 - 66 Chapter 3. Rheology and Configurational Entropy of Silicate Melts by P. Richet & Y. Bottinga, p. 67 - 94 Chapter 4. Viscoelasticity by Sharon L. Webb and Donald B. Dingwell, p. 95 - 120 Chapter 5. Energetics of Silicate Melts by Alexandra Navrotsky, p. 121 - 144 Chapter 6. Thermodynamic Mixing Properties and the Structure of Silicate Melts by Paul C. Hess, p. 145 - 190 Chapter 7. Dynamics and Structure of Silicate and Oxide Melts: Nuclear Magnetic Resonance Studies by Jonathan F. Stebbins, p. 191 - 246 Chapter 8. Vibrational Spectroscopy of Silicate Liquids by Paul F. McMillan and George H. Wolf, p. 247 - 316 Chapter 9. X-ray Scattering and X-ray Spectroscopy Studies of Silicate Melts by Gordon E. Brown, Jr., François Farges, and G. Calas, p. 317 - 410 Chapter 10. Diffusion in Silicate Melts by Sumit Chakraborty, p. 411 - 504 Chapter 11. Pressure Effects on Silicate Melt Structure and Properties by G. H. Wolf and Paul F. McMillan, p. 505 - 562 Chapter 12. Computer Simulations of Silicate Melts by Peter H. Poole, Paul F. McMillan, and George H. Wolf, p. 563 - 616
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  • 9
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Chapman & Hall
    Associated volumes
    Call number: 11/M 96.0355 ; M 96.0087
    In: The Mineralogical Society series
    Type of Medium: Monograph available for loan
    Pages: xiv, 372 S.
    ISBN: 0412610302
    Series Statement: Mineralogical Society series 7
    Classification:
    Mineralogy
    Language: English
    Location: Reading room
    Location: Upper compact magazine
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  • 10
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 05.0438 ; M 07.0130
    Type of Medium: Monograph available for loan
    Pages: xiii, 192 S. : zahlr. graph. Darst.
    Edition: 2nd ed.
    ISBN: 052184875X , 978-0-521-84875-6
    Classification:
    Mineralogy
    Location: Reading room
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