
Başlık:
Structure and dynamics of the Earth's interior. 1, Dynamics of the Earth's mantle
Yazar:
Monteux, Julien, editor.
ISBN:
9781394361748
9781394361731
Fiziksel Tanımlama:
1 online resource (272 pages)
Seri:
Sciences. Geoscience. Earth's interior
İçerik:
Foreword -- Yanick RICARD -- Chapter 1. Models of Mantle Dynamics 1 Gaël CHOBLET -- 1.1. Toward the first models of the Earth's mantle -- 1.1.1. Prior to the models -- 1.1.2. Continental drift, thermal convection and plate tectonics -- 1.2. The physical model: thermal convection -- 1.2.1. Conservation laws: mass, momentum, energy -- 1.2.2. Constitutive relationships: Fourier, rheology and equation of state -- 1.2.3. Boundary and initial conditions -- 1.2.4. Dimensioning, dimensional analysis and dimensionless numbers -- 1.2.5. From linear stability analysis to turbulent convection -- 1.3. "Solving" partial differential equations -- 1.3.1. Spectral methods -- 1.3.2. Finite-difference or finite-volume methods -- 1.3.3. Finite element methods -- 1.3.4. Various aspects of contemporary methods -- 1.4. From a reductionist to a holistic approach -- 1.4.1. Mixed heating -- 1.4.2. Sphericity -- 1.4.3. Rheology -- 1.4.4. Composition -- 1.4.5. Several phases -- 1.5. Conclusion -- 1.6. References -- Chapter 2. How the Earth's Core and Mantle are Separated: Geochemical and Dynamic Constraints 41 Julien MONTEUX and Maud BOYET -- 2.1. Introduction -- 2.2. How the Earth's core and mantle are separated: geochemical clues -- 2.2.1. Internal composition model of the Earth and telluric planets -- 2.2.2. Chemical elements and their properties -- 2.2.3. Meteorites: Building blocks of the Earth -- 2.2.4. Constraints using moderately siderophile elements -- 2.2.5. Excessive concentration of HSE -- 2.3. Iron/silicate separation in a magma ocean -- 2.3.1. Fragmentation on impact -- 2.3.2. Fragmentation in the magma ocean -- 2.3.3. Thermochemical evolution of iron droplets -- 2.4. Iron/silicate separation by giant diapirism -- 2.5. Giant impact core assemblies -- 2.6. Conclusion and outlook for magnetic fields -- 2.7. References -- Chapter 3. Dynamics and Thermal Evolution of the Earth's Early Mantle 75 Julien MONTEUX and Denis ANDRAULT -- 3.1. Introduction -- 3.2. Primitive energy sources -- 3.2.1. Short-lived radioactive elements -- 3.2.2. Impact heating -- 3.2.3. Viscous dissipation related to core formation -- 3.2.4. Giant impacts and the Moon's formation -- 3.3. Melting curves in the deep mantle -- 3.3.1. Mantle solidus profile: the temperature at which the first magmas formed -- 3.3.2. Melting curves for other silicates in the Earth's mantle -- 3.3.3. Eutectic mantle melting diagram: example of the core/mantle boundary -- 3.3.4. Temperature constraints at the core/mantle boundary -- 3.4. The mantle during the magma ocean stage -- 3.4.1. A vigorous convection system -- 3.4.2. Magma ocean modeling -- 3.4.3. Adiabatic profiles -- 3.4.4. Cooling dynamics -- 3.5. From magma oceans to present-day mantle dynamics -- 3.5.1. Melt fraction rates and viscosity models -- 3.5.2. Cooling dynamics -- 3.5.3. Magma ocean-solid mantle coupling -- 3.5.4. Geochemical consequences -- 3.6. External influences -- 3.6.1. Relationship between the primitive mantle and the core -- 3.6.2. Influence of the primitive atmosphere -- 3.6.3. The Moon's influence -- 3.7. Conclusion -- 3.8. References -- Chapter 4. Hotspots, Large Igneous Provinces and Global Mantle Dynamics 115 Cinzia G. FARNETANI -- 4.1. Introduction -- 4.2. Active hotspots today -- 4.3. Geochemistry of hotspot lavas: long-lived and short-lived isotope systems, what do they tell us? -- 4.4. Seismic imaging below hotspots: To which extent do LLSVPs and ULVZs "feed" mantle plumes? -- 4.5. Plumes in the convecting mantle -- 4.6. Large igneous provinces -- 4.6.1. Phanerozoic continental flood basalts -- 4.6.2. Phanerozoic oceanic plateaus -- 4.6.3. Older LIPs and radiating dyke swarms -- 4.7. Environmental effects of Phanerozoic large igneous provinces -- 4.7.1. Factors triggering global warming and global cooling -- 4.7.2. Oceanic anoxia events: ocean acidification -- 4.7.3. Ozone depletion from halogen emissions: release of toxic metals -- 4.8. Concluding remarks -- 4.9. References -- Chapter 5. Heat Flow and Secular Cooling of the Mantle 155 Stéphane LABROSSE -- 5.1. Introduction -- 5.2. Geophysics of the seafloor and the oceanic heat flow -- 5.2.1. Infinite half-space model -- 5.2.2. Observations: seafloor age and heat flow -- 5.2.3. Seafloor depth -- 5.2.4. Total oceanic heat loss -- 5.2.5. Link to mantle dynamics -- 5.3. Continental heat flow -- 5.4. Heat sources and secular evolution -- 5.5. Conclusion -- 5.6. References -- Chapter 6. Noble Gases: Geochemical Tracers of Mantle Dynamics 187 Manuel Alexis MOREIRA -- 6.1. Introduction -- 6.2. Noble gases in the mantle -- 6.2.1. General information on noble gases -- 6.2.2. Noble gas analysis -- 6.3. The evolution of the mantle-atmosphere system -- 6.3.1. Outflows: mantle degassing -- 6.4. Past and present dynamics of the Earth's mantle -- 6.4.1. A homogeneous asthenosphere through convection and/or efficient melting? -- 6.4.2. Noble gas constraints on magma ocean dynamics -- 6.5. Open questions on the origin and evolution of terrestrial noble gases -- 6.5.1. Helium concentration in island basalts -- 6.5.2. The origin of terrestrial neon (and of helium and hydrogen) -- 6.5.3. Missing xenon -- 6.6. References -- List of Authors -- Index.
Özet:
The silicate mantle and its dynamics have controlled the Earth's internal cooling for over four billion years. Today, these dynamics are rather slow, but this was not always the case: shortly after the core/mantle separation, this reservoir was significantly melted, with dynamics like those of a magma ocean. Despite advances in analytical and numerical tools and a better understanding of the Earth's internal structure, the Earth's mantle currently remains a mystery. Structure and Dynamics of the Earth's Interior 1 presents the evolution of mantle dynamics throughout Earth's history, from its formation to the present day. It examines the contributions of numerical modeling, as well as the seismological, petrological and geochemical data used to constrain dynamic models. Finally, the book analyzes the manifestations of mantle dynamics in terms of surface cooling, volcanism and coupling with the atmosphere.
Notlar:
John Wiley and Sons
Tür:
Yazar Ek Girişi:
Elektronik Erişim:
https://onlinelibrary.wiley.com/doi/book/10.1002/9781394361748Kopya:
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Kütüphane | Materyal Türü | Demirbaş Numarası | Yer Numarası | Durumu/İade Tarihi | Materyal Ayırtma |
|---|---|---|---|---|---|
Arıyor... | E-Kitap | 599805-1001 | QE509.4 | Arıyor... | Arıyor... |
