MadSci Network: Earth Sciences |
Seismic waves have a great contribution on determining the temperature
of the lithosphere, and, consequently, the temperature of the upper
asthenosphere. The main point here is that the wave velocities depend upon
several parameters, and one of the most important is the temperature. So, by
modelling the wave velocities vertical distribution, one can model the
lithosphere thermal structure.
The process is not so simple, and it requires also a thermal conductivity
model to calculate the lithosphere distribution of temperature, and some
assumption on the distribution of heat producing elements in this region
in order to constrain some parameters.
A recent work on the determination of the thermal structure of the
lithosphere (and so, the top of the asthenosphere) was presented by Irina
Artemieva and Walter D. Mooney, and you can see the poster in the attached
images. The references below can help you in the understanding of this
process.
Best regards
Eder C. Molina (eder@iag.usp.br)
Dept. of Geophysics
Institute of Astronomy, Geophysics and Atmospheric Sciences
University of Sao Paulo - BRAZIL
REFERENCES
Artemieva, I.M. & Mooney, W.D., 2001. Thermal structure and evolution of Precambrian Lithosphere. Journal of Geophysical Research, 106, 16387-16414.
Pollack, H.N., Hurter, S.J. and Johnson, J.R., 1993. Heat flow from the Earth's interior: analysis of the geothermal data set. Reviews of Geophysics, 31, 267-280.
Related web links:
CRUST 2.0 - a new global crustal model at 2x2 degree
A new global heatflow compilation
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