The outer shells of the earth

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ID: 300306
1928
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Abstract
A discussion of Adam and Gibson (1926) and Bridgman's (1925) results on the compressibility of basaltic glass. Daly revises their estimates of compressibility at high pressure and claims that computed seismic velocities fit his model of a basaltic layer and cast doubt upon the existence of an ultramafic or peridotite mantle.
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openalex_W2318933900 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors R. A. Daly
Journal american journal of science
Year 1928
DOI
10.2475/ajs.s5-15.86.108
URL
Keywords Keywords not found

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