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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Earth sciences. ; Geology. ; Geochemistry. ; Earth Sciences. ; Geology. ; Geochemistry.
    Description / Table of Contents: The World Hidden Beneath Us - Structure and Composition of the Earth -- Air, Water, Earth - The Exogenic Geological Processes -- Fire - How Magmatism Shaped the Earth -- Geomagnetism - The Space Shield of the Planet Earth -- Seismicity - The Breath of a Restless Earth -- Plate Tectonics - The Great Unifying Theory -- Geochemical Cycles - The Circulatory System of Planet Earth -- The Geochemical Cycles and the Environment - How Man is Changing the Earth -- From Hadean to Anthropocene - The Endless Story of a Lucky Planet -- Epilogue.
    Abstract: The book describes the structure, composition and evolution of the Earth, the main geological processes occurring on it, and how some crucial environmental matters that are amply debated in the media (e.g. pollution, greenhouse effect) can be fully understood by placing them in the holistic context of the system Earth as a whole. It provides basic information on a series of key geological issues, from the structure and composition of the Earth to the large-scale processes that characterize our planet, such as rock alteration and sedimentation, magmatism, geomagnetism, seismicity, plate tectonics, cyclical migration of chemical elements through various Earth reservoirs (Geochemical Cycles), and evolution of the planet from Hadean to present. It intends to reach a wide readership, which is interested in our planet and wish to have a general and comprehensive view of its origin, evolution and activity. Potential readership includes undergraduate and advanced undergraduate students in Geology and other scientific disciplines, and any moderately- to well-educated people interested in the surrounding world and eager to gain a basic knowledge of the Earth and to reach an integrated view of how our planet is working. Includes debated issues of the environmental changes by framing them within the evolution and history of the Earth.
    Type of Medium: Online Resource
    Pages: XV, 223 p. 59 illus., 58 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9783030780135
    DDC: 550
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 06.0282
    Description / Table of Contents: Contents: Plio-Quaternary Magmatism in Italy. - The Tuscany Magmatic Province. - The Umbria-ultra-alkaline Province. - The Roman Province. - Roccamonafina Province. - The Campania Province and Mt. Vulture. - The Aeolian Arc. - Sicily Na-alkaline Province. - Tyrrhenian Sea and Sardinia. - Geodynamic Setting.
    Type of Medium: Monograph available for loan
    Pages: XIV, 365 S. + 1 CD-ROM , Ill., graph. Darst. , 24 cm
    ISBN: 354025885X
    Classification:
    Petrology, Petrography
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    facet.materialart.12
    Cham : Springer
    Call number: 9783030780135 (e-book)
    Description / Table of Contents: The book describes the structure, composition and evolution of the Earth, the main geological processes occurring on it, and how some crucial environmental matters that are amply debated in the media (e.g. pollution, greenhouse effect) can be fully understood by placing them in the holistic context of the system Earth as a whole. It provides basic information on a series of key geological issues, from the structure and composition of the Earth to the large-scale processes that characterize our planet, such as rock alteration and sedimentation, magmatism, geomagnetism, seismicity, plate tectonics, cyclical migration of chemical elements through various Earth reservoirs (Geochemical Cycles), and evolution of the planet from Hadean to present. It intends to reach a wide readership, which is interested in our planet and wish to have a general and comprehensive view of its origin, evolution and activity. Potential readership includes undergraduate and advanced undergraduate students in Geology and other scientific disciplines, and any moderately- to well-educated people interested in the surrounding world and eager to gain a basic knowledge of the Earth and to reach an integrated view of how our planet is working. Includes debated issues of the environmental changes by framing them within the evolution and history of the Earth.
    Type of Medium: 12
    Pages: 1 Online-Ressource (xv, 223 Seiten) , Illustrationen
    Edition: 2021, corrected publication 2022
    ISBN: 9783030780135 , 978-3-030-78013-5
    Uniform Title: Aria, Acqua, Terra, Fuoco Come funziona il sistema Terra
    Language: English
    Note: Contents 1 The World Hidden Beneath Us - Structure and Composition of the Earth 1.1 Introduction 1.2 Xenoliths, Meteorites, Earthquakes: Witnesses of the Underground World 1.3 The Structure and Composition of the Earth 1.3.1 The Compositional Layering: Core, Mantle, and Crust 1.3.2 The Mechanical Layering: Inner Core, Outer Core, Convective Mantle, and Lithosphere 1.4 Summary 1.5 Box 1.1 - Minerals and Rocks References 2 Air, Water, Earth - The Exogenic Geological Processes 2.1 Introduction 2.2 Rocks and Soils 2.3 The Atmosphere 2.4 The Hydrosphere 2.5 The Sedimentary Cycle: Air, Water and Earth at Work 2.5.1 Rocks Breakdown 2.5.2 Removal and Transportation of Weathering Products 2.5.3 Sediment Deposition 2.5.4 Diagenesis: Back to Rocks 2.6 The Remains of Mountains 2.7 The Fate of the Organic Matter 2.8 Summary 2.9 Box 2.1 - Water-Air-Earth Interaction: Some Basic Geochemistry 2.10 Box 2.2 - Limestone, a Most Meritorious Rock References 3 Fire - How Magmatism Shaped the Earth 3.1 Introduction 3.2 Magmas: What They Are, How They Form 3.3 Magmatism and the Structure of the Earth 3.3.1 From Chaos to Order 3.4 Volcanism 3.4.1 Types of Volcanic Eruptions 3.4.2 Volcanism and the Terrestrial Environment 3.4.3 Large Igneous Provinces and Mass Extinctions 3.5 Global Distribution of Magmatism 3.6 Summary 3.7 Box 3.1 - Magmatism: How and Why 3.7.1 Main Types of Magma 3.7.2 Ascent, Diversification and Solidification of Magmas 3.8 Box 3.2 - Heat Flow and Geothermal Energy 3.9 Box 3.3 - Magmatism and Ore Deposits References 4 Geomagnetism - The Space Shield of the Planet Earth 4.1 Introduction 4.2 The Earth’s Magnetic Field 4.3 Palaeomagnetism: The Magnetic Memory of Rocks 4.3.1 Magnetic Reversal 4.4 Palaeomagnetism, Continental Drift, and Ocean Floor Spreading 4.5 Summary 4.6 Box 4.1 - Geomagnetism: A Historical Perspective 4.7 Box 4.2 - Geomagnetism and the Biosphere References 5 Seismicity—The Breath of a Restless Earth 5.1 Introduction 5.2 Rock Failure, Earthquakes, and Faults 5.2.1 Stress and Rock Deformation 5.2.2 Earthquakes and Faults 5.3 Seismic Waves 5.4 Seismographs and Seismograms 5.5 Earthquake Magnitude, Intensity and Frequency 5.6 Global Distribution of Earthquakes 5.7 Summary 5.8 Box 5.1- Earthquake Effects, Prediction, Forecasting, and Mitigation References 6 Plate Tectonics - The Great Unifying Theory 6.1 Introduction 6.2 Fixism Versus Mobilism 6.2.1 The Theory of Continental Drift 6.2.2 From Continental Drift to Plate Tectonics 6.3 Plate Tectonics: The Framework 6.4 The Plate Boundaries 6.4.1 Divergent Boundaries 6.4.2 Convergent Boundaries 6.4.3 Transform Boundaries 6.5 Why Do Plates Move? 6.6 Where, When and Why Does Subduction Start 6.7 Summary 6.8 Box 6.1 - Linear Volcanism and Hotspots 6.9 Box 6.2 - The Continents References 7 Geochemical Cycles - The Circulatory System of Planet Earth 7.1 Introduction 7.2 Geochemical Cycles: Some Definitions 7.3 The Water Cycle 7.4 The Sodium Cycle 7.5 The Carbon Biogeochemical Cycle 7.6 The Phosphorus Biogeochemical Cycle 7.7 The Nitrogen Biogeochemical Cycle 7.8 The Oxygen Cycle 7.9 The Iron Cycle 7.10 The Geochemical Cycles of Lead and Arsenic 7.11 Summary 7.12 Box 7.1 The Rock Cycle 7.13 Box 7.2 The Geochemical Cycles and the Age of the Earth References 8 The Geochemical Cycles and the Environment - How Man is Changing the Earth 8.1 Introduction 8.2 Geochemical Cycles and Environmental Pollution 8.2.1 Toxic Elements 8.2.2 Phosphorus and Nitrogen Compounds 8.3 Environmental Aspects of the Carbon Cycle 8.3.1 CO2 and the Ocean Acidification 8.3.2 CO2 and the Greenhouse Effect 8.3.3 CO2 and Climatic Change: A Geological Perspective 8.3.4 A Lesson for the Future 8.4 Plastic Waste Pollution 8.5 Summary 8.6 Box 8.1 - Stable Isotopes: Measuring the Temperature of the Past 8.6.1 Some Basics of Isotope Geochemistry 8.6.2 The Delta Notation 8.6.3 Oxygen-Hydrogen Isotope Geothermometry 8.7 Box 8.2 - CO2 Sequestration: The message from Decameron References 9 From Hadean to Anthropocene - The Endless Story of a Lucky Planet 9.1 Introduction 9.2 From the Solar Nebula to the Formation of Planets 9.3 Hadean: The Hellish Aeon (~4600–4000 Ma) 9.4 Archaean (4000–2500 Ma): The Dawn of Life and the Start of Modern Plate Tectonics 9.5 Proterozoic (2500–541 Ma): Oxygen, Eukaryotes, Supercontinents 9.6 Phanerozoic: The explosion of Complex Organisms (541–0 Ma) 9.6.1 The Spread of Animals and Plants 9.7 Finally, The Anthropocene 9.8 The Gaia Hypothesis 9.9 Summary 9.10 Box 9.1 - Geochronology: How Ages of Rocks, Fossils and Geologic Events Are Determined 9.10.1 Relative Age of Rocks and Fossils 9.10.2 Absolute Age References 10 Epilogue 10.1 The Earth Anomaly 10.2 The Best of All Possible Worlds 10.3 Historical Times, Geological Times 10.4 Technology, Natural Resources and Environmental Impact 10.5 Natura, Non Nisi Parendo Vincitur Correction to: Air, Water, Earth, Fire Further Reading Index
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  • 4
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The problem of mantle metasomatism vs. crustal contamination in the genesis of arc magmas with different potassium contents has been investigated using new trace element and Sr–Nd–Pb isotopic data on the island of Vulcano, Aeolian arc. The analysed rocks range in age from 120 ka to the present day, and cover a compositional range from basalt to rhyolite of the high-K calc-alkaline (HKCA) to shoshonitic (SHO) and potassic (KS) series. Older Vulcano products (〉30 ka) consist of HKCA–SHO rocks with SiO2=48–56%. They show lower contents of K2O, Rb and of several other incompatible trace element abundances and ratios than younger rocks with comparable degree of evolution. 87Sr/86Sr ranges from 0.70417 to 0.70504 and increases with decreasing MgO and compatible element contents. 206Pb/204Pb ratios display significant variations (19.31 to 19.76) and are positively correlated with MgO, 143Nd/144Nd (0.512532–0.512768), 207Pb/204Pb (15.66–15.71) and 208Pb/204Pb (39.21–39.49). Overall, geochemical and isotopic data suggest that the evolution of the older series was dominated by assimilation–fractional crystallisation (AFC) with an important role for continuous mixing with mafic liquids. Magmas erupted within the last 30 ka consist mostly of SHO and KS intermediate and acid rocks, with minor mafic products. Except for a few acid rocks, they display moderate isotopic variations (e.g. 87Sr/86Sr=0.70457–0.70484; 206Pb/204Pb=19.28–19.55, but 207Pb/204Pb=15.66–15.82), which suggest an evolution by fractional crystallisation, or in some cases by mixing, with little interaction with crustal material. The higher Sr isotopic ratios (87Sr/86Sr=0.70494–0.70587) of a few, low-volume, intermediate to acid rocks support differentiation by AFC at shallow depths for some magma batches. New radiogenic isotope data on the Aeolian islands of Alicudi and Stromboli, as well as new data for lamproites from central Italy, are also reported in order to discuss along-arc compositional variations and to evaluate the role of mantle metasomatism. Geochemical and petrological data demonstrate that the younger K-rich mafic magmas from Vulcano cannot be related to the older HKCA and SHO ones by intra-crustal evolutionary processes and point to a derivation from different mantle sources. The data from Alicudi and Stromboli suggest that, even though interaction between magma and wall rocks of the Calabrian basement during shallow level magma evolution was an important process locally, a similar interpretation can be extended to the entire Aeolian arc.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 58 (1976), S. 63-81 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Analytical data for Sr, Rb, Cs, Ba, Pb, rare earth elements, Y, Th, U, Zr, Hf, Sn, Nb, Mo, Ni, Co, V, Cr, Sc, Cu and major elements are reported for eocene volcanic rocks cropping out in the Kastamonu area, Pontic chain of Northern Turkey. SiO2% versus K2O% relationship shows that the analyzed samples belong to two major groups: the basaltic andesitic and the andesitic ones. High-K basaltic andesites and low-K andesites occur too. Although emplaced on continental type basement (the North Anatolian Crystalline Swell), the Pontic eocene volcanics show elemental abundances closely comparable with typical island arc calc-alkaline suites, e.g. low SiO2% range, low to moderate K2O% and large cations (Cs, Rb, Sr, Ba, Pb) contents and REE patterns with fractionated light and almost flat heavy REE patterns. ΣREE and highly charged cations (Th, U, Hf, Sn, Zr) are slightly higher than typical calc-alkaline values. Ferromagnesian elements show variable values. Within the basaltic andesite group the increase of K%, large cations, ΣREE, La/Yb ratio and high valency cations and the decrease of ferromagnesian element abundances with increasing SiO2% content indicate that the rock types making up this group developed by crystalliquid fractionation of olivine and clinopyroxene from a basic parent magma. Trace element concentration suggest that the andesite group was not derived by crystal-liquid fractionation processes from the basaltic andesites, but could represent a distinct group of rocks derived from a different parent magma.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The present paper reports the results of a detailed stratigraphical, petrological and geochemical investigation on the island of Stromboli, Aeolian arc, Southern Tyrrhenian sea. Major and trace element data determined on a large quantity of samples from well-established stratigraphic positions indicate that the magmatological evolution of the island through time was more complex than previously known. The activity of the exposed part of Stromboli, which occurred over a time span of about 100 000 years, started with the emission of high-K calc-alkaline (HKCA) volcanics, which were covered by calc-alkaline (CA), shoshonitic (SHO), high-K calc-alkaline (HKCA) and potassic (KS) products. The most recent activity consists of HKCA lavas and the present-day SHO-basaltic volcanics emitted by mildly explosive “strombolian” activity. Most of the products are lavas, with minor amounts of pyroclastic rocks emplaced mainly during the early stages of activity. The transition from the SHO to the KS cycle was associated with the collapse of the upper part of the volcanic apparatus; the transition from KS to the present-day SHO activity has been found to have occurred at the time of the sliding of the western portion of the volcano that generated the “Sciara del Fuoco” depression. The rock series cropping out at Stromboli show variable enrichment in potassium, incompatible trace elements and radiogenic Sr which increase from CA through HKCA, and SHO up to KS rocks. Major, trace element and Sr-isotopic data agree in indicating that the HKCA and SHO series evolved by crystal/liquid fractionation starting from different parental liquids, whereas crustal assimilation appears to have been the leading process during the evolution of KS volcanics. Mixing processes also played a role although they can be well documented only when they occurred between magmas with different isotopic and geochemical characteristics. Geochemical modelling based on trace element and isotopic data indicates that the mafic magmas of the different volcanic series may be generated by melting of an upper mantle heterogeneously enriched in incompatible elements and radiogenic Sr by addition, via subduction, of different amounts of crustal material. Geochemical data, however, are also in agreement with the alternative hypothesis that the most mafic magmas of the different series have been generated by combined processes of fractional crystallization, assimilation and mixing of a CA magma in a deep-sited magma chamber; the mafic magmas formed by these complex processes were successively emplaced in a shallow reservoir where they evolved by simple fractional crystallization (HKCA and SHO series) and by assimilation of crustal material (KS). The occurrence of changes in the geochemical signatures of the magmas at the time of the structural modification of the volcano is believed to favour the hypothesis that the variable composition observed in the volcanic rocks of Stromboli is the result of processes occurring within the volcanic system.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2011-07-23
    Print ISSN: 1866-6280
    Electronic ISSN: 1866-6299
    Topics: Geosciences
    Published by Springer
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  • 8
    Publication Date: 2007-02-23
    Print ISSN: 0026-3672
    Electronic ISSN: 1436-5073
    Topics: Chemistry and Pharmacology
    Published by Springer
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  • 9
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