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  • 1
    Online Resource
    Online Resource
    Cary :Oxford University Press, Incorporated,
    Keywords: Analytical geochemistry. ; Quantum chemistry. ; Mineralogical chemistry. ; Chemical bonds. ; Electronic books.
    Description / Table of Contents: 1. Introduction 2. Experimental Methods 3. Theoretical Methods 4. Application of Quantum Mechanical Methods to Simple Inorganic "Molecules" of Relevance to Mineralogy and to Oxide Minerals 5. Applications to Silicate, Carbonate, and Borate Minerals and Related Species 6. Applications of Bonding Models to Sulfide Minerals 7. Applications in Mineral Physics and Chemistry 8. Applications to Geochemical Problems 9. The Future.
    Type of Medium: Online Resource
    Pages: 1 online resource (529 pages)
    Edition: 1st ed.
    ISBN: 9780195364569
    DDC: 551.9
    Language: English
    Note: Intro -- CONTENTS -- 1. INTRODUCTION -- 1.1 Historical perspective-ionic and atomistic approaches -- 1.2 Crystal-field theory and the geochemistry of the transition metals -- 1.3 Quantum chemistry -- 1.4 Solid-state quantum physics (band theory and related approaches) -- 1.5 Quantum geochemistry -- 1.6 Models and methods -- 2. EXPERIMENTAL METHODS -- 2.1 Diffraction effects -- 2.1.1 X-ray diffraction -- 2.1.2 Neutron diffraction -- 2.1.3 Electron diffraction and associated phenomena -- 2.2 Electron and x-ray spectroscopy -- 2.2.1 Photoelectron spectroscopy (and Auger electron spectroscopy) -- 2.2.2 X-ray emission spectroscopy -- 2.2.3 X-ray absorption spectroscopy (including EXAFS and XANES) -- 2.3 Optical (uv-visible-near-ir) spectroscopy -- 2.3.1 Electronic (optical) absorption spectroscopy -- 2.3.2 Reflectance (diffuse and specular) spectroscopy -- 2.4 Vibrational spectroscopy -- 2.4.1 Theoretical basis -- 2.4.2 Infrared spectroscopy -- 2.4.3 Raman spectroscopy -- 2.4.4 Reporting of data -- 2.5 Nuclear spectroscopy -- 2.5.1 Nuclear quadrupole resonance -- 2.5.2 Nuclear magnetic resonance -- 2.5.3 The Mössbauer effect -- 2.6 Other methods -- 2.6.1 Electron spin resonance -- 2.7 Concluding remarks -- 3. THEORETICAL METHODS -- 3.1 Elements of quantum mechanics -- 3.2 Details of Hartree-Fock-Roothaan calculations: Choice of basis set -- 3.2.1 Minimum basis sets -- 3.2.2 Extended basis sets: Double-& -- #950 -- bases -- 3.2.3 Extended basis sets: Polarized bases -- 3.2.4 Extended basis sets: Other approaches -- 3.2.5 Basis set and calculated properties -- 3.3 Improvements on the Hartree-Fock wave function -- 3.4 Dependence of computation time on basis-set size (and property calculated) for Hartree-Fock-Roothaan and configuration-interaction calculations. , 3.5 Prediction of properties other than equilibrium geometries from Hartree-Fock-Roothaan calculations -- 3.6 Evaluation of spectral and other experimental parameters using Hartree-Fock-Roothaan calculations -- 3.7 Approximate Hartree-Fock methods -- 3.8 Hartree-Fock band-structure calculations -- 3.9 Elements of density-functional theory -- 3.10 The multiple-scattering or scattered-wave X-& -- #945 -- method -- 3.11 Density-functional band theory -- 3.12 Theoretical ionic models-the modified electron-gas approach -- 3.13 Simulation methods -- 3.14 Combined local-density-functional molecular dynamics approach -- 3.15 Relationships between localized and delocalized approaches -- 3.15.1 Orbital and band energies -- 3.15.2 Incorporation of external atoms of the solid into cluster calculations -- 3.16 Concluding remarks on different theoretical approaches -- 4. APPLICATION OF QUANTUM-MECHANICAL METHODS TO SIMPLE INORGANIC "MOLECULES" OF RELEVANCE TO MINERALOGY, AND TO OXIDE MINERALS -- 4.1 The inorganic molecules SiO, SiO[sub(2)], Si[sub(2)]O[sub(2)], and Si[sub(3)]O[sub(3)] -- 4.2 The SiF[sub(4)] molecule -- 4.2.1 Geometric structure of SiF[sub(4)] -- 4.2.2 Electronic structure of SiF[sub(4)] - electron spectroscopy -- 4.2.3 Electronic structure of SiF[sub(4)] - x-ray-absorption spectra -- 4.2.4 Electronic structure of SiF[sub(4)] - [sup(29)]Si NMR spectra -- 4.3 Major oxide minerals -- 4.3.1 MgO (periclase) -- 4.3.2 Al[sub(2)]O[sub(3)] (corundum) -- 4.3.3 SiO[sub(2)] [silica polymorphs -- also Si(OH)[sub(4)], SiO[sub(4)] [sup(-4)], (SiH[sub(3)])[sub(2)]O, and (OH)[sub(3)]SiOSi(OH)[sub(3)]] -- 4.4 Transition-metal oxides -- 4.4.1 Titanium oxides -- 4.4.2 Manganese oxides -- 4.4.3 Iron oxides (and hydroxides) -- 4.4.4 Complex oxides -- 4.4.5 Band theory and the transition-metal monoxides. , 4.5 Calculation of Mössbauer parameters in iron oxides (and other iron compounds) -- 5. APPLICATIONS TO SILICATE, CARBONATE, AND BORATE MINERALS AND RELATED SPECIES -- 5.1 Introduction -- 5.2 Silicates -- 5.2.1 Olivines: Geometric structures -- 5.2.2 Olivines: Electronic structures -- 5.2.3 Element distributions and solid solutions in olivines -- 5.2.4 Structure and stability of silicates of intermediate polymerization -- 5.2.5 Electronic structures of silicates other than olivines and SiO[sub(2)] -- 5.3 Carbonates -- 5.3.1 Carbonates: Geometric structures -- 5.3.2 Carbonates: Electronic structures and properties -- 5.4 Borates -- 5.4.1 B[sub(2)]O[sub(3)] and the borates: Geometric structures -- 5.4.2 B[sub(2)]O[sub(3)] and the borates: Spectra and electronic structures -- 6. APPLICATION OF BONDING MODELS TO SULFIDE MINERALS -- 6.1 Introduction -- 6.2 Sphalerite, würtzite, and related phases [ZnS, CdS, HgS, (Zn,Fe)S] -- 6.3 Galena (PbS) and the isostructural selenide and telluride minerals (PbSe, PbTe) -- 6.4 Pyrite (FeS[sub(2)]), pyrrhotite (Fe[sub(1-x)]S), and related phases (CoS[sub(2)], NiS[sub(2)], CuS[sub(2)], ZnS[sub(2)] -- CoS, NiS) -- 6.5 Marcasite (FeS[sub(2)]), arsenopyrite (FeAsS), loellingite (FeAs[sub(2)]), and related minerals -- 6.6 Copper, copper-iron, and related sulfides (Cu[sub(2)]S, CuS, CuFeS[sub(2)], Cu[sub(5)]FeS[sub(4)], Ag[sub(2)]S) -- 6.7 The thiospinels [Co[sub(3)]S[sub(4)], CuCo[sub(2)]S[sub(4)], (Co,Ni)[sub(3)]S[sub(4)], Ni[sub(3)]S[sub(4)], FeNi[sub(2)]S[sub(4)], FeCr[sub(2)]S[sub(4)]] -- 6.8 Other (including complex) sulfides [MoS[sub(2)], Co[sub(9)]S[sub(8)], (Ni,Fe)[sub(9)]S[sub(8)], Cu[sub(12)]Sb[sub(4)]S[sub(13)], etc.] -- 6.9 Concluding remarks -- 7. APPLICATIONS IN MINERAL PHYSICS AND CHEMISTRY -- 7.1 Structure, bonding, and stereochemistry -- 7.1.1 Covalency and ionicity in solids from calculation and experiment. , 7.1.2 Calculation of geometric structures and their (phase) relations: The example of the SiO[sub(2)] polymorphs -- 7.1.3 Pauling's rules reinterpreted -- 7.1.4 Qualitative molecular-orbital theory and its applications -- 7.2 Minerals at elevated pressures and the interior of the Earth -- 7.2.1 Olivine and Mg[sub(2)]SiO[sub(4)] spinel -- 7.2.2 MgSiO[sub(3)]and CaSiO[sub(3)] perovskite -- 7.2.3 Simple oxides, structural and electronic phase transitions -- 7.2.4 Iron (and Fe-rich alloys) at core pressures -- 7.3 Industrial mineral materials -- 7.3.1 Zeolites -- 7.3.2 Transition-metal sulfide catalysts -- 7.4 Concluding remarks -- 8. APPLICATIONS TO GEOCHEMICAL PROBLEMS -- 8.1 The nature of melts, glasses, and crystal-melt equilibria -- 8.1.1 Silica glass and melt -- 8.1.2 Glasses and melts of more complex compositions -- 8.1.3 Crystal-melt equilibria -- 8.2 Solution species -- 8.2.1 Quantum-mechanical studies of water and aqueous (ionic) solutions -- 8.2.2 Aqueous metal complexes, hydrothermal solutions, and hydrothermal ore deposits -- 8.2.3 Theoretical studies on Zn chloride complexes in aqueous solution -- 8.3 Mineral surfaces -- 8.3.1 The surface of MgO (periclase) -- 8.3.2 The surface of TiO[sub(2)] (rutile) -- 8.3.3 Oxide surface defects and the reactivity of surfaces -- 8.3.4 The surface of ZnS (sphalerite) -- 8.3.5 The surface of Cu[sub(5)]FeS[sub(4)] (bornite) and atmospheric tarnishing -- 8.3.6 Concluding remarks on surface studies -- 8.4 Geochemical distribution of the elements -- 8.4.1 The Goldschmidt classification: Ionic and orbital interpretations -- 8.4.2 Lithophile versus chalcophile behavior: The M-O versus the M-S bond -- 8.4.3 Geochemical coherence and geochemical differentiation -- 9. THE FUTURE -- 9.1 Capabilities of quantum-mechanical methods -- 9.2 Future areas of application in structures and energetics. , 9.3 Future applications in mineral spectroscopy -- 9.4 New areas of application -- 9.5 Research directions -- 9.6 Epilog: Theoretical geochemistry and the Earth and environmental sciences -- APPENDIX A: Symbols, units, conversion factors, and constants -- APPENDIX B: Experimental methods for obtaining information on structure and bonding -- APPENDIX C: Quantum-mechanical (and related) calculational methods and terminology -- REFERENCES -- INDEX -- A -- B -- C -- D -- E -- F -- G -- H -- I -- L -- M -- N -- O -- P -- Q -- R -- S -- T -- W -- X -- Z.
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  • 2
    Book
    Book
    Cambridge [u.a.] : Cambridge Univ. Press
    Keywords: Metal sulfides ; Kristallchemie ; Mineral ; Sulfiderz ; Kristallchemie ; Mineral ; Sulfiderz
    Type of Medium: Book
    Pages: XV, 493 S , graph. Darst
    ISBN: 0521214890
    Series Statement: Cambridge earth science series
    DDC: 549.32
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    Language: English
    Note: Literaturverz. S. 441 - 476
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  • 3
    Keywords: Analytical geochemistry ; Quantum chemistry ; Mineralogical chemistry ; Chemical bonds ; analytic geochemistry ; quantum chemistry ; mineralogical chemistry ; chemical bonds ; Geology and Palaeontology ; Geochemie ; Quantenmechanik ; Angewandte Geowissenschaften ; Mineralogie
    Type of Medium: Book
    Pages: XIV, 514 S , graph. Darst
    ISBN: 0195044037
    DDC: 551.9
    RVK:
    Language: English
    Note: Literaturverz. S. 458 - 508
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  • 4
    Book
    Book
    New York, NY [u.a.] : Wiley
    Keywords: Ores ; Thin sections (Geology) ; Geology and ; Palaeontology ; ores ; thin sections (geology) ; Erzmineralien ; Mikroskopie ; Gesteinskunde ; Dünnschliff ; Erzmineralien ; Mikroskopie ; Gesteinskunde ; Dünnschliff ; Erzmikroskopie ; Erz ; Gesteinskunde
    Type of Medium: Book
    Pages: XIV, 434 S. , Ill., graph. Darst. , 24 cm
    Edition: 2. ed.
    ISBN: 0471115991 , 0471551759
    Series Statement: Wiley interscience publication
    DDC: 549/.12
    RVK:
    Language: English
    Note: Literaturangaben
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  • 5
    Book
    Book
    Chantilly, Va. : Mineralogical Society of America [u.a.]
    Keywords: Sulfides ; Geochemistry ; Aufsatzsammlung ; Konferenzschrift ; Mineralogie ; Sulfide ; Geochemie ; Sulfide ; Sulfide ; Mineralogie ; Mineralchemie
    Type of Medium: Book
    Pages: XIII, 714 S , Ill., graph. Darst., Tab
    ISBN: 0939950731
    Series Statement: Reviews in mineralogy and geochemistry 61
    DDC: 549.32
    RVK:
    RVK:
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    Language: English
    Note: Literaturangaben
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 240 (1972), S. 33-35 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Amphiboles, which are hydroxyl-bearing double-chain silicates, are important constituents of the crust4'5. They occur not only in a variety of igneous and metamorphic rocks that crystallized at moderate temperatures and pressures, but also in alkali amphiboles such as Na2(Mg,Fe2+)3(Al,Fe3+) ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 13 (1986), S. 347-350 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Auger electron spectra (AES) of sulfides are interpreted using published photoelectron spectra, sulfurK β X-ray emission spectra (XES) and Multiple ScatteringX α calculations on metal-sulfide molecular clusters and using newly measured spectra for ZnS, Cu2S and MoS2. For compounds without appreciable metald-sulfur 3p interactions, only one sulfur LVV peak or a closely spaced doublet is observed. For those with substantial metald-sulfur 3p interactions additional peaks occur, with peaks at lower electron kinetic energy arising from ejection of electrons from orbitals more tightly bound than theS3p, and those with higher kinetic energy arising from electrons in less tightly bound orbitals. Thus, for many sulfide minerals, the sulfur LVV Auger Spectrum is essentially a self-convolution of the valence band density of states weighted by the amount of S3p character, and can be predicted from a knowledge of the sulfurK β X-ray emission spectra and the X-ray photoelectron spectra.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Synchrotron radiation has been used to collect Cu K-edge and Ag K-edge EXAFS from several tetrahedrite, (Cu,Ag)10(Zn,Fe,Cu)2Sb4S13, minerals. The results have been used to investigate the coordination environment of the Ag and Cu, and to determine which sites in the structure are occupied by silver atoms when they replace copper. The Ag EXAFS spectrum of a sample with high silver content reveals an interaction between silver and antimony which may explain the anomalous decrease in unit cell size found in natural tetrahedrites when the silver content increases beyond four atoms per unit formula.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 9 (1983), S. 253-262 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The sulfide minerals exhibit a rich diversity in sturctural chemistry and in electrical, magnetic and other physical properties. Models based on molecular orbital theory and incorporating some elements of band theory can be developed to describe the diverse valence electron behavior in these minerals. Qualitative models can be proposed on the basis of observed properties, and the models can be tested and refined using experimental data from X-ray emission and X-ray photoelectron spectroscopy and quantum mechanical calculations performed on cluster units which form the basic building blocks of the crystals. This approach to chemical bonding in sulfide minerals is illustrated for binary non-transition metal sulfides (ZnS, CdS, HgS, PbS), binary transition metal sulfides (FeS2, CoS2, NiS2, CuS2 ZnS2) and more complex sulfides (CuFeS2, Cu2S, Ag2S, CuS, Co3S4, CuCo2S4, Fe3S4). The relationship between qualitative and quantitative theories is reviewed with reference to the pyrite-marcasite-arsenopyrite-loellingite series of minerals. Application of the models to understanding structure-determining principles, relative stabilities, solid solution limits and properties such as color, reflectance and hardness are discussed.
    Type of Medium: Electronic Resource
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