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  • 1
    Book
    Book
    Die Cambridge Platonists : Religion und Freiheit in England im 17. Jahrhundert (1993)
    Frankfurt am Main u.a. :Lang,
    Details
    UID:
    almahu_BV007229929
    Format: 181 S.
    ISBN: 3-631-45684-0
    Series Statement: [Europäische Hochschulschriften / 03] 540
    Note: Zugl.: Trier, Univ., Diss., 1991
    Language: German
    Subjects: Theology , Philosophy
    RVK:
    BF 1440
    RVK:
    CF 1250
    RVK:
    CF 1200
    Keywords: Philosophenschule ; Philosophenschule ; Platonismus ; Philosophenschule ; Freiheit ; Hochschulschrift ; Hochschulschrift ; Hochschulschrift
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  • 2
    Book
    Book
    Bewahren und Erneuern : Geschichte der katholischen Erwachsenenbildung im Saarland (1998)
    Weimar :Dadder,
    Details
    UID:
    almahu_BV025925291
    Format: 180 S.
    ISBN: 3-926406-98-4
    Language: German
    Subjects: Education
    RVK:
    DW 1021
    Keywords: Katholische Erwachsenenbildung ; Geschichte ; Geschichte
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  • 3
    Book
    Book
    Mandeville und Smith : ökonomisches Denken im Kontext der englischen Sozial- und Wirtschaftsgeschichte des 18. Jahrhunderts (1984)
    Details
    UID:
    almafu_BV042581059
    Format: 156 S.
    Note: Berlin, Freie Univ., Magisterarbeit, 1984
    Language: German
    Keywords: Hochschulschrift
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  • 4
    Online Resource
    Online Resource
    Iron isotope fractionation in carbonatite melt systems : = Fe-Isotopenfraktionierung in karbonatitischen Schmelzen (2021)
    Potsdam
    Details
    UID:
    gbv_1777953286
    Format: 1 Online-Ressource (xvi, 137 Seiten, 14025 KB) , Illustrationen, Diagramme
    Content: Carbonatite magmatism is a highly efficient transport mechanism from Earth’s mantle to the crust, thus providing insights into the chemistry and dynamics of the Earth’s mantle. One evolving and promising tool for tracing magma interaction are stable iron isotopes, particularly because iron isotope fractionation is controlled by oxidation state and bonding environment. Meanwhile, a large data set on iron isotope fractionation in igneous rocks exists comprising bulk rock compositions and fractionation between mineral groups. Iron isotope data from natural carbonatite rocks are extremely light and of remarkably high variability. This resembles iron isotope data from mantle xenoliths, which are characterized by a variability in δ56Fe spanning three times the range found in basalts, and by the extremely light values of some whole rock samples, reaching δ56Fe as low as -0.69 ‰ in a spinel lherzolite. Cause to this large range of variations may be metasomatic processes, involving metasomatic agents like volatile bearing high-alkaline ...
    Note: Volltext: PDF , Dissertation Universität Potsdam 2021
    Additional Edition: Erscheint auch als Druck-Ausgabe Stuff, Maria Iron isotope fractionation in carbonatite melt systems Potsdam, 2021
    Language: English
    Keywords: Hochschulschrift
    DOI: 10.25932/publishup-51992
    URN: urn:nbn:de:kobv:517-opus4-519928
    URL: Volltext  (kostenfrei)
    URL: Volltext  (kostenfrei)
    URL: https://d-nb.info/1243582138/34
    URL: kostenfrei
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    Fulltext
    UB Potsdam
  • 5
    Book
    Book
    Mikromechanisches Modell zur Ermittlung effektiver Materialeigenschaften von geschädigten Polykristallen (2001)
    Karlsruhe : IKM
    Details
    UID:
    b3kat_BV014025362
    Format: VI, 136 S. , Ill., graph. Darst. : 21 cm
    Edition: Als Ms. gedr.
    Series Statement: IKM-Schriftenreihe 35
    Note: Zugl.: Karlsruhe, Univ., Diss., 2001
    Language: German
    Keywords: Hochschulschrift
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  • 6
    Microfilm
    Microfilm
    High field strength elements and rare earth elements in the depleted mantle : a trace element and isotope study of the Balmuccia peridotite complex (Ivrea Zone, Italian Alps) (2001)
    Details
    UID:
    almafu_BV014023262
    Format: 125 S. : , Ill., graph. Darst.
    Edition: [Mikrofiche-Ausg.]
    Edition: Mikroform-Ausgabe Münster r@tiodata 2001 2 Mikrofiches : 24 X
    Note: Münster, Univ., Diss., 2001
    Additional Edition: Reproduktion von Weyer, Stefan High field strength elements and rare earth elements in the depleted mantle 2001
    Language: English
    Keywords: Peridotit ; Elementenhäufigkeit ; Mikroform ; Hochschulschrift
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  • 7
    Online Resource
    Online Resource
    Iron Geochemistry: An Isotopic Perspective (2020)
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Details
    UID:
    gbv_1689110724
    Format: 1 Online-Ressource(XII, 360 p. 129 illus., 123 illus. in color.)
    Edition: 1st ed. 2020.
    ISBN: 9783030338282
    Series Statement: Advances in Isotope Geochemistry
    Content: Introduction and Overview -- Analytical Methods -- Fe Isotope Fractionation Factors -- High-Temperature Fe Isotope Geochemistry -- The modern surficial world -- The Ancient Earth.
    Content: This book provides a comprehensive summary of research to date in the field of stable iron isotope geochemistry. Since research began in this field 20 years ago, the field has grown to become one of the major research fields in "non-traditional" stable isotope geochemistry. This book reviews all aspects of the field, from low-temperature to high-temperature processes, biological processes, and cosmochemical processes. It provides a detailed history and state-of-the art summary about analytical methods to determine Fe-isotope ratios and discusses analytical and sample prospects.
    Additional Edition: ISBN 9783030338275
    Additional Edition: ISBN 9783030338299
    Additional Edition: ISBN 9783030338305
    Additional Edition: Erscheint auch als Druck-Ausgabe Johnson, Clark Iron geochemistry Cham, Switzerland : Springer, 2020 ISBN 9783030338275
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 9783030338299
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 9783030338305
    Language: English
    Subjects: Earth Sciences
    RVK:
    TH 4100
    Keywords: Eisenisotop ; Stabiles Isotop ; Isotopengeochemie ; ICP-Massenspektrometrie ; Isotopengeologie ; Biogeochemie ; Isotopenhäufigkeit ; Isotopieeffekt ; Eisenisotop ; Kosmochemie ; Hochtemperatur ; Paläoozeanographie
    DOI: 10.1007/978-3-030-33828-2
    URL: lizenzpflichtig
    URL: Cover
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  • 8
    Book
    Book
    Iron isotope fractionation in carbonatite melt systems (2021)
    Potsdam
    Details
    UID:
    gbv_1777953502
    Format: xvi, 137 Seiten , Illustrationen, Diagramme
    Content: Carbonatite magmatism is a highly efficient transport mechanism from Earth’s mantle to the crust, thus providing insights into the chemistry and dynamics of the Earth’s mantle. One evolving and promising tool for tracing magma interaction are stable iron isotopes, particularly because iron isotope fractionation is controlled by oxidation state and bonding environment. Meanwhile, a large data set on iron isotope fractionation in igneous rocks exists comprising bulk rock compositions and fractionation between mineral groups. Iron isotope data from natural carbonatite rocks are extremely light and of remarkably high variability. This resembles iron isotope data from mantle xenoliths, which are characterized by a variability in δ56Fe spanning three times the range found in basalts, and by the extremely light values of some whole rock samples, reaching δ56Fe as low as -0.69 ‰ in a spinel lherzolite. Cause to this large range of variations may be metasomatic processes, involving metasomatic agents like volatile bearing high-alkaline ...
    Note: Dissertation Universität Potsdam 2021
    Additional Edition: Erscheint auch als Online-Ausgabe Stuff, Maria Iron isotope fractionation in carbonatite melt systems Potsdam, 2021
    Language: English
    Keywords: Hochschulschrift
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  • 9
    Online Resource
    Online Resource
    Iron geochemistry: an isotopic perspective / (2020)
    Cham :Springer,
    Details
    UID:
    edocfu_BV046403208
    Format: 1 Online-Ressource (xii, 360 Seiten) : , Illustrationen, Diagramme (teilweise farbig).
    ISBN: 978-3-030-33828-2
    Series Statement: Advances in Isotope Geochemistry
    Additional Edition: Erscheint auch als Druck-Ausgabe, Hardcover ISBN 978-3-030-33827-5
    Additional Edition: Erscheint auch als Druck-Ausgabe, Softcover ISBN 978-3-030-33830-5
    Language: English
    Subjects: Earth Sciences
    RVK:
    TH 4100
    DOI: 10.1007/978-3-030-33828-2
    URL: Volltext  (URL des Erstveröffentlichers)
    URL: http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=031815930&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
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  • 10
    Online Resource
    Online Resource
    Iron geochemistry : an isotopic perspective (2020)
    Cham : Springer
    Details
    UID:
    kobvindex_GFZEBC6011713
    Format: 1 Online-Ressource (xii, 360 Seiten) , Illustrationen
    ISBN: 9783030338282 , 978-3-030-33828-2
    ISSN: 2364-5113 , 2364-5105
    Series Statement: Advances in isotope geochemistry
    Content: This book provides a comprehensive summary of research to date in the field of stable iron isotope geochemistry. Since research began in this field 20 years ago, the field has grown to become one of the major research fields in "non-traditional" stable isotope geochemistry. This book reviews all aspects of the field, from low-temperature to high-temperature processes, biological processes, and cosmochemical processes. It provides a detailed history and state-of-the art summary about analytical methods to determine Fe-isotope ratios and discusses analytical and sample prospects.
    Note: Contents 1 Introduction and Overview 1.1 Geochemistry of Fe 1.1.1 Fe Redox 1.2 Stable Isotope Geochemistry 1.2.1 Nomenclature 1.2.2 Isotopic Fractionation 1.2.3 Processes that Produce Isotopic Variations 1.3 Overview of the Chapters References 2 Analytical Methods 2.1 Introduction 2.2 Iron Purification Methods 2.3 Mass Spectrometry 2.3.1 Beginnings of Fe Isotope Analysis 2.3.2 Multi Collector Inductively Coupled Plasma Mass Spectrometry (MC-ICP-MS) 2.3.3 Modern MC-ICP-MS Using Pseudo High Mass Resolution Methods 2.3.4 Matrix Effects and Instrumental Mass Fractionation Corrections 2.4 In Situ Techniques 2.5 Summary References 3 Fe Isotope Fractionation Factors 3.1 Introduction 3.2 Deriving Fe Isotope Fractionation Factors from First Principles 3.3 Experimental Methods for Measuring Fe Isotope Fractionation Factors 3.3.1 The Role of Sorption in Isotope Exchange 3.4 Equilibrium Fractionation of Fe Isotopes: Working Toward a Unified Set of Fractionation Factors 3.4.1 Aqueous Fe Species 3.4.2 Aqueous Fe Mineral Fractionation 3.5 Biological Experiments 3.5.1 Fe Oxidizing Experiments 3.5.2 Magnetotactic Bacteria 3.5.3 Fe Reducing Experiments 3.6 Preferred Set of b-Values 3.7 Summary References 4 High-Temperature Fe Isotope Geochemistry 4.1 Iron Isotope Variations in the Solar System 4.1.1 Chondrites and Chondritic Components 4.1.2 Differentiated Planetary Material 4.2 The Silicate Earth 4.2.1 The Mantle and Its Minerals 4.2.2 Basalts and Komatiites 4.2.3 Differentiated Crust 4.2.4 Magmatic Minerals 4.2.5 Hydrothermal Products and Ores 4.2.6 Metamorphic Rocks 4.3 Planetary Formation and Magmatic Processes 4.3.1 Planetary Accretion 4.3.2 Formation and Differentiation of Planetary Cores 4.3.3 Partial Melting on Earth and Other Planets 4.3.4 Mantle Metasomatism 4.3.5 Differentiation of Melts 4.3.6 The Mantle and Crust of the Earth as Compared to Other Planets 4.4 Summary References 5 The Modern Surficial World 5.1 Weathering 5.1.1 Mechanical Weathering 5.1.2 Chemical Weathering 5.1.3 Soils 5.2 Rivers and Groundwater 5.2.1 Rivers 5.2.2 Groundwater and Terrestrial Hydrothermal Systems 5.3 Redox-Stratified Water Bodies 5.3.1 Lake Water 5.3.2 Lake Sediments 5.3.3 The Black Sea 5.4 Marine Sediments 5.4.1 Reactive Fe Inventories 5.4.2 Pore Fluid-Sediment Interactions 5.4.3 Solid-Phase Fe Components 5.4.4 Benthic Fe Fluxes 5.5 The Fe Budget of the Modern Oceans 5.5.1 Seawater Fe 5.5.2 Riverine and Aeolian Sources 5.5.3 Benthic Sources 5.5.4 Hydrothermal Sources 5.6 Summary References 6 The Ancient Earth 6.1 The Cenozoic Marine System 6.1.1 Global Changes in the Cenozoic 6.1.2 Fe–Mn Crusts as Archives of Paleo-Seawater Compositions 6.1.3 Fe Isotope Variations in Cenozoic Seawater 6.2 Cretaceous Anoxic Events 6.2.1 Cenomanian-Turonian OAE-2 6.3 Precambrian Earth: An Introduction 6.3.1 Broad Changes in the Surface Earth in the Precambrian 6.3.2 Temporal Changes in Fe Abundance and Speciation 6.3.3 Differences in Marine Fe Pathways Between Modern and Ancient Earth 6.3.4 Authigenic Fe Isotope and Reactive Fe Trends 6.4 Precambrian Earth: The Neoproterozoic 6.4.1 Neoproterozoic Clastic Marine Sedimentary Rocks 6.4.2 Revisiting Reactive Fe Speciation and d56Fe 6.4.3 Neoproterozoic Iron Formations (IFs) 6.5 Precambrian Earth: The Paleoproterozoic and Neoarchean Transition Through the GOE 6.5.1 The Post-GOE Sedimentary Record 6.5.2 Changes in Weathering Across the GOE 6.5.3 Moving to a Low-Oxygen World: Key Issues of Fe Mass Balance, Fe Isotope Fractionation Factors, Fe 2+aq Oxidation, and the Age of Redox Proxies 6.5.4 Early Paleoproterozoic Iron Formations (IFs) 6.5.5 Early Paleoproterozoic Rise of Mn Redox 6.5.6 Paleoproterozoic and Neoarchean Continental Margins: Relations Between Shales, Carbonate Platforms, and IFs . 6.6 Precambrian Earth: The Early Archean Record 6.6.1 The Mesoarchean Witwatersrand and Pongola Basins 6.6.2 The Paleoarchean Barberton Greenstone Belt and Pilbara Craton 6.6.3 The High-Grade Metamorphic Terranes of the Eoarchean 6.7 Precambrian Earth: Synthesis of the Eoarchean Through Paleoproterozoic 6.8 Chapter Summary References
    Language: English
    Keywords: Electronic books ; Lehrbuch
    DOI: 10.1007/978-3-030-33828-2
    URL: Fulltext @ Ebook Central (AWI only)
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    Wissenschaftspark Albert Einstein
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