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Cited by 311

The DOI matches its Crossref record; 197 of the 197 references it cites were found in a registry or an index.

Composition of the upper mantle: Geophysical tests of two petrological models

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Bass, Jay D., Anderson, Don L.·1984·Geophysical Research Letters

Abstract

The elastic properties of candidate mantle phases are used to test the viability of olivine‐rich (pyrolitic) and CaO + Al 2 O 3‐rich (eclogitic) assemblages for the mantle. High temperature adiabats for each phase of interest are constructed and compared to mantle seismic properties. Both pyrolitic and eclogitic assemblages satisfy the seismic properties between ∼ 200 and 400 km. Between 400 and 670 km depth an eclogitic assemblage yields a superior match to velocities and velocity gradients. The 400 km seismic discontinuity may represent a chemical boundary between pyrolite and picritic eclogite (“piclogite”) or phase transformations in the olivine + orthopyroxene components of a piclogitic assemblage containing about 16% olivine. High velocity gradients in the transition zone may be explained by the transformation of Ca‐rich cpx to majorite garnet. Seismic properties at the top of the lower mantle are consistent with pyrolite, piclogite or perovskite, implying that the 670 km discontinuity may be a chemical boundary.

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Metadata

Authors
Bass, J. D., & Anderson, D. L.
Venue
Geophysical Research Letters
Published
1984-03
Volume
11
Issue
3
Pages
229-232
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2094922011
Cited by
311
References
197
FWCI
10.00
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Composition of the upper mantle: Geophysical tests of two petrological models. https://app.cochat.ai/papers/10.1029/gl011i003p00229
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Bass, J. D., & Anderson, D. L. (1984). Composition of the upper mantle: Geophysical tests of two petrological models. Geophysical Research Letters. https://doi.org/10.1029/gl011i003p00229

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