Earth's deep mantle

Structure, composition, and evolution

Robert D. Van Der Hilst, Jay D Bass, Jan Matas, Jeannot Trampert

Research output: Book/ReportBook

Abstract

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?

Original languageEnglish (US)
PublisherWiley
Number of pages334
ISBN (Electronic)9781118666258
ISBN (Print)0875904254, 9780875904252
DOIs
StatePublished - Mar 29 2013

Fingerprint

Earth mantle
minerals
planets
rock mechanics
rocks
atmospheres
supercomputers
petrology
seismology
solar atmosphere
geodynamics
seismic waves
meteorites
stirring
mounting
mass spectrometers
extrapolation
synchrotrons
convection
isotopes

ASJC Scopus subject areas

  • Physics and Astronomy(all)

Cite this

Earth's deep mantle : Structure, composition, and evolution. / Van Der Hilst, Robert D.; Bass, Jay D; Matas, Jan; Trampert, Jeannot.

Wiley, 2013. 334 p.

Research output: Book/ReportBook

Van Der Hilst, Robert D. ; Bass, Jay D ; Matas, Jan ; Trampert, Jeannot. / Earth's deep mantle : Structure, composition, and evolution. Wiley, 2013. 334 p.
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