Thermal regime of the Earth's interior

Stacey F.D. (1975) Thermal regime of the Earth's interior. Nature, 255 5503: 44-45. doi:10.1038/255044a0

Author Stacey F.D.
Title Thermal regime of the Earth's interior
Journal name Nature   Check publisher's open access policy
ISSN 0028-0836
Publication date 1975-01-01
Sub-type Article (original research)
DOI 10.1038/255044a0
Open Access Status Not yet assessed
Volume 255
Issue 5503
Start page 44
End page 45
Total pages 2
Language eng
Subject 2700 Medicine
1000 General
Abstract SEVERAL recent and apparently unrelated geophysical observations and deductions, when considered together, necessitate a fundamental re-examination of our ideas about the thermal state of the Earth's deep interior. In summary they are: (1) Precession must be discounted as a power source for the geomagnetic dynamo1, leaving core convection as the only plausible basic mechanism. Therefore the temperature gradient in the outer core cannot be less than adiabatic. (2) The thermodynamic Grüneisen parameter for the outer core is about 1.4 and is only slightly pressure dependent (R. D. Irvine and F.D.S., unpublished). (3) The resulting adiabatic gradient is much steeper than the Fe melting point gradient2 or the Fe-S eutectic gradient3. (4) Continents and ocean floors are both mobile, although the ocean floors are much more so4, so that equality of the continental and oceanic heat fluxes which is observed5 (in spite of gross differences between the radioactive constituents of the continental and oceanic crusts) cannot be explained in terms of an association of depleted regions of the mantle with continents. (5) Hot spots, across which the tectonic plates move, are not themselves moving perceptibly with respect to one another and are presumed to mark features of a rigid lower mantle4. (6) A weak layer (asthenosphere) in the upper mantle allows virtually perfect isostatic balance of continent-sized blocks6 but the lower mantle must have greater strength. Low degree harmonic features of the geoid are supported by stresses at depths of several hundred kilometres7. (7) Radiative transfer does not cause a dramatic increase in the thermal conductivity of mantle material at high temperatures8,9.
Q-Index Code C1
Institutional Status Unknown

Document type: Journal Article
Sub-type: Article (original research)
Collection: Scopus Import - Archived
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Citation counts: TR Web of Science Citation Count  Cited 19 times in Thomson Reuters Web of Science Article | Citations
Scopus Citation Count Cited 14 times in Scopus Article | Citations
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