Relating Geophysical Structures and Processes: The Jeffreys

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The inner core, however, is solid because of the enormous pressure. [7] Reconstruction of seismic reflections in the deep interior indicate some major discontinuities in seismic velocities that demarcate the major zones of the Earth: inner core, outer core, mantle, lithosphere and crust. Editor-in-Chief, Frontiers in Mineral Physics: Report of Mineral Physics Committee of the AGU, 1988. Students will spend at least one academic year of residency at each campus.

Pages: 133

Publisher: American Geophysical Union; 1 edition (January 11, 1993)

ISBN: 087590467X

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