By Gerald Schubert, Donald L. Turcotte, Peter Olson
ISBN-10: 0511017863
ISBN-13: 9780511017865
ISBN-10: 0511612877
ISBN-13: 9780511612879
ISBN-10: 052135367X
ISBN-13: 9780521353670
ISBN-10: 0521798361
ISBN-13: 9780521798365
Mantle Convection within the Earth and Planets is a accomplished synthesis of all features of mantle convection in the Earth, the terrestrial planets, the Moon, and the Galilean satellites of Jupiter. The authors comprise updated discussions of the newest study advancements that experience revolutionized our figuring out of the Earth and the planets. The ebook encompasses a entire index, an in depth reference record, a variety of illustrations (many in colour) and significant questions that spotlight the dialogue and recommend avenues of destiny learn. it truly is compatible as a textual content for graduate classes in geophysics and planetary physics, and as a supplementary reference to be used on the undergraduate point. it's also a useful evaluation for researchers within the huge fields of the Earth and planetary sciences.
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Additional resources for Mantle Convection in the Earth and Planets (Cambridge Monographs on Mechan)
Sample text
The result is an intracrustal asthenosphere layer within the continental lithosphere. Although the concept of a lithosphere is straightforward, there is in fact considerable confusion because the precise definition depends on the property being considered. We speak of the mechanical lithosphere, the thermal lithosphere, and the elastic lithosphere. Here each is considered in turn. (1) Mechanical lithosphere. The mechanical lithosphere is defined to be those rocks that remain a coherent part of the plates on geological time scales.
The essentials of the plate tectonics model will be discussed in the next chapter. Although plate tectonics is an enormously successful model, it is essentially kinematic in nature. As the accounts in this chapter indicate, the search for a fully dynamic theory for tectonics has proven to be a far more difficult task. It has involved many branches of Earth Science, and continues to this day. This book describes the achievements as well as the questions remaining in this search. 1 Introduction During the 1960s there were a wide variety of studies on continental drift and its relationship to mantle convection.
Studies of seismic focal mechanisms in the Wadati–Benioff zone give extensional stresses in the upper part of the zone and compressional stresses in the lower part of the zone (Isacks and Molnar, 1971). Another major mantle phase transition at a depth of about 410 km is associated with the phase change from olivine to β spinel. Theoretical studies indicate that this shallower exothermic phase change will enhance convection (Turcotte and Schubert, 1971). , 1975; Christensen and Yuen, 1984). The effects of major solid–solid phase transitions on convection in the mantle will be discussed in detail in Chapters 4, 9, and 10.
Mantle Convection in the Earth and Planets (Cambridge Monographs on Mechan) by Gerald Schubert, Donald L. Turcotte, Peter Olson
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