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Earth’s Deep Mantle – Structure, Composition, and Evolution

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Earth’s Deep Mantle – Structure, Composition, and Evolution

Earth's Deep Mantle - Structure, Composition, and Evolution
Robert D. Van Der Hilst , Jay D. Bass , JAN Matas , Jeannot Trampert
American Geophysical Union
Earth's Deep Mantle - Structure, Composition, and Evolution
  • Release Date
    2022-09-04
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3.0 $

  • Category
    Earth Science
  • File Type
    Book
  • Language
    English
  • File Format
    PDF
  • Year
    2005
  • ISBN-13
    9780875904252
  • Pages
    337 pages
  • File Size
    54.827 MB
  • Release Date
    2022-09-04

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Book Summary

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 160.

Understanding the inner workings of our planet and its relationship to processes closer to the surface remains a frontier in the geosciences. Manmade probes barely reach ˜10 km depth and volcanism rarely brings up samples from deeper than ˜150 km. These distances are dwarfed by Earth’s dimensions, and our knowledge of the deeper realms is pieced together from a range of surface observables, meteorite and solar atmosphere analyses, experimental and theoretical mineral physics and rock mechanics, and computer simulations. A major unresolved issue concerns the nature of mantle convection, the slow (1-5 cm/year) solid-state stirring that helps cool the planet by transporting radiogenic and primordial heat from Earth’s interior to its surface.

Expanding our knowledge here requires input from a range of geoscience disciplines, including seismology, geodynamics, mineral physics, and mantle petrology and chemistry. At the same time, with better data sets and faster computers, seismologists are producing more detailed models of 3-D variations in the propagation speed of different types of seismic waves; new instrumentation and access to state-of-the-art community facilities such as synchrotrons have enabled mineral physicists to measure rock and mineral properties at ever larger pressures and temperatures; new generations of mass spectrometers are allowing geo-chemists to quantify minute concentrations of diagnostic isotopes; and with supercomputers geodynamicists are making increasingly realistic simulations of dynamic processes at conditions not attainable in analogue experiments. But many questions persist. What causes the lateral variations in seismic wavespeed that we can image with mounting accuracy? How reliable are extrapolations of laboratory measurements on simple materials over many orders of magnitude of pressure and temperature? What are the effects of volatiles and minor elements on rock and mineral properties under extreme physical conditions? Can ab initio calculations help us understand material behavior in conditions that are still out of reach of laboratory measurement? What was the early evolution of our planet and to what extent does it still influence present-day dynamics? And how well do we know such first-order issues as the average bulk composition of Earth?

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