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- Q4680537 subject Q7037494.
- Q4680537 subject Q7215285.
- Q4680537 subject Q7481094.
- Q4680537 abstract "The Adams–Williamson equation, named after L. H. Adams and E. D. Williamson, is a relation between the velocities of seismic waves and the density of the Earth's interior. Given the average density of rocks at the Earth's surface and profiles of the P-wave and S-wave speeds as function of depth, it can predict how density increases with depth. It assumes that the compression is adiabatic and that the Earth is spherically symmetric, homogeneous, and in hydrostatic equilibrium. It can also be applied to spherical shells with that property. It is an important part of models of the Earth's interior such as the Preliminary reference Earth model (PREM).".
- Q4680537 wikiPageWikiLink Q1208908.
- Q4680537 wikiPageWikiLink Q1318259.
- Q4680537 wikiPageWikiLink Q182453.
- Q4680537 wikiPageWikiLink Q186167.
- Q4680537 wikiPageWikiLink Q2053186.
- Q4680537 wikiPageWikiLink Q208641.
- Q4680537 wikiPageWikiLink Q29539.
- Q4680537 wikiPageWikiLink Q30006.
- Q4680537 wikiPageWikiLink Q39552.
- Q4680537 wikiPageWikiLink Q461466.
- Q4680537 wikiPageWikiLink Q62932.
- Q4680537 wikiPageWikiLink Q6583695.
- Q4680537 wikiPageWikiLink Q7037494.
- Q4680537 wikiPageWikiLink Q7215285.
- Q4680537 wikiPageWikiLink Q7481094.
- Q4680537 wikiPageWikiLink Q900371.
- Q4680537 comment "The Adams–Williamson equation, named after L. H. Adams and E. D. Williamson, is a relation between the velocities of seismic waves and the density of the Earth's interior. Given the average density of rocks at the Earth's surface and profiles of the P-wave and S-wave speeds as function of depth, it can predict how density increases with depth. It assumes that the compression is adiabatic and that the Earth is spherically symmetric, homogeneous, and in hydrostatic equilibrium.".
- Q4680537 label "Adams–Williamson equation".