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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Mars (Planet) - Volcanoes. ; Electronic books.
    Description / Table of Contents: This comprehensive volume outlines the distinctive processes and characteristics of glaciovolcanic eruptions, with reference to terrestrial and Martian occurrences, and how they can be used to unravel planetary palaeoclimatic histories. Supported by abundant photos, this is an ideal reference for academic researchers and postgraduate students.
    Type of Medium: Online Resource
    Pages: 1 online resource (514 pages)
    Edition: 1st ed.
    ISBN: 9781316667415
    DDC: 551.21
    Language: English
    Note: Cover -- Half-title page -- Title page -- Copyright page -- Contents -- Preface: Nature and scope of the volume -- Acknowledgments -- 1 Introduction -- 1.1 What is glaciovolcanism? -- 1.2 The importance of glaciovolcanism -- 1.3 History of glaciovolcanic research -- 1.4 Styles of glaciovolcanism and classification of the products -- 1.5 The 'standard tuya model' -- 1.6 Compositional classification used in this book -- 2 Distribution of glaciovolcanism on Earth -- 2.1 Introduction -- 2.2 Antarctica -- 2.3 Iceland -- 2.4 North America -- 2.5 Other locations -- 2.6 Summary -- 3 Observations of historical and recent glaciovolcanic eruptions -- 3.1 Introduction -- 3.2 Classification of glaciovolcanic eruptions -- 3.3 Descriptions of observed glaciovolcanic eruptions -- 3.4 Important lessons learned and observations needed for future eruptions -- 4 Physical properties of ice important for glaciovolcanic eruptions -- 4.1 Introduction -- 4.2 Physical structure of an ice mass -- 4.3 Thermal regime -- 4.4 Rheology -- 4.5 Hydraulics -- 5 Chemical and physical properties important to glaciovolcanic lavas -- 5.1 Introduction -- 5.2 Compositional range -- 5.3 Lava temperatures -- 5.4 Viscosity (η) -- 5.5 Other thermodynamic properties -- 5.6 Summary -- 6 Physics of glaciovolcanism -- 6.1 Introduction -- 6.2 Magma generation -- 6.3 Magma migration -- 6.4 Heat transfer -- 6.5 Fragmentation processes -- 6.6 Volatile saturation and vesiculation -- 6.7 Constraints on modes of emplacement -- 6.8 Formation of cooling fractures -- 6.9 Summary -- 7 Analytical studies of glaciovolcanic materials -- 7.1 Introduction -- 7.2 Morphometry -- 7.3 Major, minor and trace element geochemistry -- 7.4 Volatile elements -- 7.5 Mineral, glass and palagonite compositions -- 7.6 Stable isotope studies -- 7.7 Geochronometric studies -- 7.8 Quantitative analysis of grain sizes. , 7.9 Summary -- 8 Landform classification and morphometry of glaciovolcanic centres -- 8.1 Introduction -- 8.2 Classification of glaciovolcanic landforms -- 8.3 Glaciovolcanic landforms constructed under cold-based ice -- 9 Lithofacies in glaciovolcanic sequences -- 9.1 Introduction -- 9.2 Terminology -- 9.3 Primary coherent lithofacies -- 9.4 Primary fragmental lithofacies -- Plates -- 9.5 Coeval deformation features -- 10 Mafic glaciovolcanic sequences -- 10.1 Introduction -- 10.2 Ice-impounded lavas -- 10.3 Pillow mounds and ridges -- 10.4 Tindars and tuyas -- 10.5 Pillow sheets: fact or fiction? -- 10.6 Sheet-like sequences -- 10.7 Large polygenetic glaciovolcanic centres -- 11 Intermediate-composition glaciovolcanic sequences -- 11.1 Introduction -- 11.2 Ice-impounded lavas -- 11.3 Domes -- 11.4 Tuyas -- 11.5 Other intermediate-composition glaciovolcanic sequences -- 11.6 Large polygenetic glaciovolcanic centres -- 12 Felsic glaciovolcanic sequences -- 12.1 Introduction -- 12.2 Ice-impounded lavas -- 12.3 Domes -- 12.4 Tuyas -- 12.5 Tindars -- 12.6 Sheet-like sequences -- 12.7 Other felsic glaciovolcanic sequences -- 12.8 Large polygenetic glaciovolcanic centres -- 13 Glaciovolcanic sequences as palaeoenvironmental proxies -- 13.1 Introduction -- 13.2 Ancient ice -- 13.3 Sedimentary evidence for glacial conditions and basal thermal regime -- 13.4 Glaciovolcanic evidence for ancient ice -- 13.5 Calculating ice thicknesses and surface elevation from glaciovolcanic sequences -- 13.6 Effect of volcanic heat on basal thermal regime of ice -- 13.7 Strengths and disadvantages of glaciovolcanic palaeoenvironmental investigations -- 13.8 Examples of palaeoenvironmental investigations using glaciovolcanic sequences -- 14 Climate triggers for glaciovolcanism -- 14.1 Introduction -- 14.2 Historical studies. , 14.3 How can waxing and waning of glaciers and ice sheets affect volcanism? -- 14.4 Likelihood of present-day climate change increasing volcanic activity -- 14.5 Potential glacial-volcanic climate feedback mechanisms -- 15 Hazards associated with glaciovolcanic eruptions -- 15.1 Introduction -- 15.2 Lava flows -- 15.3 Ash falls -- 15.4 Pyroclastic density currents -- 15.5 Meltwater floods and associated mass flows -- 15.6 Avalanches -- 15.7 Lightning -- 15.8 Short-term versus long-term climate impacts -- 15.9 Summary -- 16 Glaciovolcanism on Mars -- 16.1 Introduction -- 16.2 Geological background -- 16.3 A water inventory for Mars -- 16.4 The hydrological cycle on Mars and glacial-interglacial cyclicity -- 16.5 Theoretical aspects of Mars' glaciovolcanism -- 16.6 Observations of Mars' glaciovolcanism -- 17 Outstanding challenges and possibilities -- 17.1 Introduction -- 17.2 Towards a better understanding of the physics and chemistry of glaciovolcanism -- 17.3 Understanding boundary conditions: how does the ice-bedrock interface influence eruptions? -- 17.4 Differentiating between marine and freshwater glaciovolcanic eruptions -- 17.5 Ice melting rates and the 'space problem' -- 17.6 Towards better assessment, monitoring and mitigation of glaciovolcanic hazards -- 17.7 Geochronology -- 17.8 Improving our understanding of planetary glaciovolcanism: Earth-Mars comparisons -- 17.9 Towards improved integration of information from ancient glaciovolcanic deposits into planetary climate models: the past as a guide to modelling future Earth climate -- Glossary: terminology of glaciovolcanism -- References -- Index.
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  • 2
    Type of Medium: Book
    Pages: S. 247 - 391 , Ill., graph. Darst., Kt.
    Series Statement: Journal of volcanology and geothermal research 185.2009,4
    Language: English
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  • 3
    Type of Medium: Book
    Pages: 131 S. , Ill., graph. Darst., Kt.
    Series Statement: Journal of volcanology and geothermal research 186.2009,1/2
    Language: English
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  • 4
    Keywords: Volcanism ; Volcanoes ; Magmas ; Ice ; Frozen ground ; Mars (Planet) Geology ; Mars (Planet) Volcanoes ; Gletscher ; Eruption ; Vulkangebiet ; Glazialgeologie ; Glazialmorphologie ; Vulkanologie ; Vulkan ; Eisdecke ; Eiskappe ; Vulkanismus ; Dynamische Geomorphologie ; Vulkanismus ; Gletscher
    Type of Medium: Book
    Pages: xii, 483 Seiten, 16 ungezählte Seiten , Illustrationen, Karten
    ISBN: 9781107037397
    DDC: 551.21
    RVK:
    RVK:
    Language: English
    Note: Literaturverzeichnis: Seite 410-460. Index
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  • 5
    Publication Date: 2020-11-30
    Description: Magma-carbonate interactions and the subsequent CO2 release can occur before and during an eruption, critically affecting magma storage and ascent processes. However, the mechanisms and timescales of those interactions are unclear, particularly during the fast magma withdrawal that feeds high-intensity eruptions. In order to better understand magma‑carbonate interactions, we selected the caldera-forming Pomici di Base plinian eruption, the oldest (22 ka) and largest (〉 4.4 km3) explosive event in the history of the Somma-Vesuvius volcanic system, as case study. During this event the emission of trachytic and latitic-shoshonitic (~25% and ~75% of the erupted magma volume respectively) magmas generated a long-lasting plinian column, hypothetically driven by CO2 liberation during magma‑carbonate interaction. In this study, we reconstruct in detail the evolution of the plumbing system during the Pomici di Base eruption combining geochemical (major/minor elements and radiogenic/stable isotopes) analyses of juvenile products with thermodynamic and kinetic calculations. Our results demonstrate that magmatic stoping (i.e., the formation and transport of host-rock pieces into a magma body) during caldera collapse evolution can promote rapid magma assimilation of carbonate blocks and CO2-rich fluids resulting from destabilization of the carbonate bedrock, thus triggering CO2 release and acting as a fuel for the eruption explosivity, especially when residual hot mafic magmas are involved. Our findings suggest that the accurate knowledge of these processes and their influence on eruptive dynamics are critical for improving the hazard assessments of volcanoes with plumbing systems located in carbonate bedrocks.
    Description: Published
    Description: 105628
    Description: 1V. Storia eruttiva
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: 4V. Processi pre-eruttivi
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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