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Density and composition of mantle and core

Birch, Francis·1964·Journal of Geophysical Research

Abstract

Two new density distributions are obtained, closely related to the seismic velocities. In the upper mantle and transition layer, density is assumed to be proportional to the velocity of compressional waves, with ratios consistent with experimental studies of rocks. In the lower mantle and core, the density variation is found by the Adams-Williamson method. The resulting densities in the lower mantle are found to be in good agreement with shock-wave measurements on rocks having FeO contents in the range 10±2% by weight, and may be accounted for in terms of mixtures of close-packed oxides, silica transforming to stishovite in the transition layer. Except for iron oxide, the chemical composition of the mantle is indeterminate. The density of the outer core is lower than that of iron by about 10%. The estimated density of the inner core, based on shock-wave measurements of metals and considerations of abundance, is no higher than 13.5 g/cm3.

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Metadata

Authors
Birch, F.
Venue
Journal of Geophysical Research
Published
1964-10-15
Volume
69
Issue
20
Pages
4377-4388
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2040292903
Cited by
646
References
1
FWCI
14.25
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Density and composition of mantle and core. https://app.cochat.ai/papers/10.1029/jz069i020p04377
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Birch, F. (1964). Density and composition of mantle and core. Journal of Geophysical Research. https://doi.org/10.1029/jz069i020p04377

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