The Solid Earth: An Introduction to Global Geophysics
Cambridge University Press, 2005 - 685 pages
The Solid Earth is a general introduction to the study of the physics of the solid Earth, including the workings of both the Earth's surface and its deep interior. The emphasis throughout is on basic physical principles rather than instrumentation or data handling. The second edition of this acclaimed textbook has been revised to bring the content fully up-to-date and to reflect the most recent advances in geophysical research. It is designed for undergraduates on introductory geophysics courses who have a general background in the physical sciences, including introductory calculus. It can also be used as a reference book for graduate students and other researchers in geology and geophysics. Each chapter ends with exercises of various degrees of complexity, for which solutions are available to instructors from www.cambridge.org/9780521893077. The book contains an extensive glossary of geological and physical terms, as well as appendices that develop more advanced mathematical topics.
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Past plate motions
Seismology Measuring the interior
The deep interior of the Earth
ridges transforms trenches
The continental lithosphere
Autres éditions - Tout afficher
American Geophysical Union amplitude Archaean asthenosphere Astr basalt basin beneath calculated centre constant continental crust continental margin continents convection cooling crustal deep deformation density depth determined Distance km Earth Planet earthquakes East Pacific Rise equation equilibrium estimate Figure fracture zone geoid geological Geophys geotherm gradient gravity anomaly heat flow horizontal hotspot inner core interface isostatic isotope layer lithosphere lower mantle magma chamber magnetic field magnitude measured metamorphic Mid-Atlantic Ridge mid-ocean ridges minerals Moho North occur oceanic crust oceanic lithosphere olivine outer core P-wave P-wave velocity Pacific plate partial melting phase plane plate boundary plate motions plate tectonics radioactive ratio reflection refraction region result ridge axis rift rocks sample Section sedimentary sediments seismic velocity seismograms seismometer shallow shear shown in Fig shows slab structure subducting plate subduction zone temperature thermal thickness transform faults trench triple junction upper mantle vector viscosity volcanic