Geodynamic phenomena such as earthquakes and volcanic eruptions are frequently observed in the Japanese island arcs, and this lecture aims at providing understanding of the geodynamics as a part of the physical and chemical processes within the Earth. By comparing basic theory and observations of mantle convection, the geodynamical phenomena are discussed for its elemental processes and mechanism in a quantitative manner.
Concerning dynamical phenomena of solid Earth, in particular, crustal deformation and mantle convection, the basic equations and the principal behaviors of dynamics are explained. How key parameters such as Rayleight number and non-dimensional internal heat generation control the system, based on which the nature of boundary layers and heat-material transportation are understood, leading to overall grasp of the Eath's system and evolution.
solidEarth, mantle, crust, convection, heat transportation, material differentiation
✔ Specialist skills | Intercultural skills | ✔ Communication skills | Critical thinking skills | Practical and/or problem-solving skills |
While explaining the basic concepts and phenomena, we try to deepen understanding through questions-and-answers and discussion of interactive-type. In addition, several exercises for important subjects are provided to be answered as a paper.
Course schedule | Required learning | |
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Class 1 | Crustal deformation in Japanese island arcs | earthquake, crustal deformation |
Class 2 | Mantle convection: basic equations and conservation law | mantle, convection, basic equations |
Class 3 | Mantle convection: equation-of-state and constitutive equation | mantle, convection, basic equations |
Class 4 | Nature of mantle convectoin | thermal convection, nature |
Class 5 | Parameters and basic structures of thernmal convection | thermal convection, parameter, structure |
Class 6 | Heat and mechanical balance in boundary layer | boundary layer, heat balance, mechanical balance |
Class 7 | Features of Earth's mantle convection | Earth's mantle, convection |
Class 8 | Structure and motion of plate and lithosphere | plate, lithosphere, structure and motion |
Class 9 | Structure of asthenosphere and 660 km discontinuity | asthenosphere, 660 kmdiscontinuity |
Class 10 | Core-mantle boundary and core convection | Core-mantle boundary |
Class 11 | Whole structure and temporal evolution of mantle convection | symmetry of convection, thermal evolution |
Class 12 | Material differentiation and cycling in the Earth | magma, elemental fractionation |
Class 13 | Formation and evolution of continental crust | magma, water, radiogenic elements |
Class 14 | Material cycling in subduction zones | magma, water, subducting plate |
Class 15 | Geodynamics of subduction zones | earthquake, magmatism, subduction zones |
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none. Reference data and diagrams are distributed at any time.
Understanding of solid Earth dynamics, in particular mantle convection, are evaluated by papers on several subjects and/or examination.
none in particular