Is there a first-order discontinuity in the lowermost mantle?

Xian Feng Liu, Jeroen Tromp, Adam M. Dziewonski

Research output: Contribution to journalArticle

21 Scopus citations

Abstract

In 1983, Lay and Helmberger [Geophys. J. R. Astron. Soc. 75 (1983) 799-837] reported the detection of a precursor to the seismic phase ScS. They attributed this precursor to a sharp seismic discontinuity located several hundred kilometers above the core-mantle boundary. Such a lowermost mantle discontinuity implies the existence of a sharp phase change or a chemical boundary. Precursors to ScS and, less frequently, PcP have since been observed in numerous locations, but are not a global phenomenon. Frequently, PcP precursors are weak or absent when ScS precursors are observed in the same location, and vice versa. There can be significant variations in the amplitude and arrival time of the precursor relative to the main phase. The presence or absence of these precursors has led to speculations about the nature of the lowermost mantle. Here we demonstrate that ScS or PcP precursors may be produced by gradients in seismic wave speed associated with large-scale lowermost mantle heterogeneity. Rather than a phase or chemical boundary with substantial topography, such gradients require lateral variations in temperature and, close to the core-mantle boundary, composition.

Original languageEnglish (US)
Pages (from-to)343-351
Number of pages9
JournalEarth and Planetary Science Letters
Volume160
Issue number3-4
DOIs
StatePublished - Aug 1 1998

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Keywords

  • Core-mantle boundary
  • D″ layer
  • Global
  • Lower mantle
  • Mantle
  • Mantle discontinuity
  • Seismology

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