Structure and dynamics of the Earth's interior. 2, Composition and structure of the Earth's mantle için kapak resmi
Başlık:
Structure and dynamics of the Earth's interior. 2, Composition and structure of the Earth's mantle
Yazar:
Demouchy, Sylvie, editor.
ISBN:
9781394361779
Fiziksel Tanımlama:
1 online resource (304 pages)
Seri:
Science. Geoscience. Earth's interior
İçerik:
Foreword xi Michel GRÉGOIRE -- Chapter 1 The Earth's Mantle: Phase Diagrams and Mineralogical Composition 1 Jean-Philippe PERRILLAT -- 1.1 Introduction -- 1.2 Phase relationships: experiments and models -- 1.3 Minerals in the Earth's mantle -- 1.4 Phase diagrams of ultra basic rocks, seismic discontinuities and mantle dynamics -- 1.5 Phase diagram of subducted basalts and fate of plates in the deep mantle -- 1.6 D" zone and bridgmanite-post-perovskite transition -- 1.7 Conclusion -- 1.8 References -- Chapter 2 Seismology of the Earth's Mantle 33 Stéphanie DURAND, Benoît TAUZIN and Éric DEBAYLE -- 2.1 Introduction -- 2.2 The architecture of the mantle: seismic discontinuities -- 2.3 The drapery: three-dimensional variations of seismic velocities -- 2.4 Mantle flow and partial melting: seismic anisotropy and attenuation -- 2.5 References -- Chapter 3 The Deep Hydrogen Cycle 83 Nathalie BOLFAN-CASANOVA and Bertrand MOINE -- 3.1 Introduction -- 3.2 The origin of terrestrial water -- 3.4 Hydrothermal weathering on the ocean floor -- 3.5 References -- Chapter 4 The Role of Volatile CO2 -H2O Species in the Melting of the Earth's Mantle 115 Malcolm MASSUYEAU and Tahar HAMMOUDA -- 4.1 Presence and storage of carbon and hydrogen in the upper mantle -- 4.2 Effects of CO2 and H2O on melting temperatures in the Earth's peridotitic mantle -- 4.3 Composition of mantle magmas in the presence of CO2 and H2O -- 4.4 Impact of CO2 and H2O on the mantle's geophysical signatures -- 4.5 References -- Chapter 5 Oxygen Fugacity in the Mantle 147 Alan B. WOODLAND -- 5.1 Introduction -- 5.2 Equilibria with iron oxides -- 5.3 The significance of oxygen fugacity -- 5.4 The ƒO2 importance for processes in the Earth's interior -- 5.5 Determining the ƒO2 content of a rock -- 5.6 The ƒO2 of the upper mantle (lithospheric) -- 5.7 Redox conditions in the deep mantle -- 5.8 A final word -- 5.9 References -- Chapter 6 Elasticity and Composition of the Earth's Mantle 193 Tiziana BOFFA-BALLARAN -- 6.1 Elasticity -- 6.2 Elastic waves -- 6.3 Polycrystalline materials -- 6.4 Experimental techniques -- 6.5 Models of the Earth's interior -- 6.6 References -- Chapter 7 Earth's Mantle Rheology 221 Sylvie DEMOUCHY and Patrick CORDIER -- 7.1 Introduction -- 7.2 Ductile deformation: mechanisms -- 7.3 Observables -- 7.4 Methodological approaches -- 7.5 Deformation in the upper mantle -- 7.6 Deformation in the mantle transition zone -- 7.7 Deformation in the lower mantle -- 7.8 Conclusion -- 7.9 References -- Chapter 8 Laboratory Measurements of Electrical Conductivity and their Applications to Planetary Interiors 249 Geeth MANTHILAKE -- 8.1 Theoretical background -- 8.2 Laboratory measurements of electrical conductivity -- 8.3 Laboratory measurements of electrical conductivity -- 8.4 Electrical conductivity of a composite medium -- 8.5 Factors affecting the electrical conductivity of planetary materials -- 8.6 The modeling of electrical conductivity data for planetary applications -- 8.7 References -- List of Authors -- Index.
Özet:
The interior of our planet is one of the last 'terra incognita'. Its chemical composition and onion-like structure of solid rocks and rare minerals make it a fascinating object. It is primarily its dynamic that makes Earth such a singular object in the solar system, with perennial, active plate tectonics for several billion years. While its dynamic is obvious on the surface (earthquakes, volcanic eruptions, mid-oceanic rifts), the very nature of the Earth's mantle - beneath the crust and in contact with the core - has not revealed all of its secrets. Structure and Dynamics of the Earth's Interior 2 recalls the fundamental principles of several key physicochemical properties of the materials which make up the Earth's mantle. This book then describes the latest technological advances used at high pressures and temperatures to reproduce the extreme conditions of the Earth's mantle in the laboratory. It also presents the latest and most significant scientific results.
Notlar:
John Wiley and Sons
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