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Title: Strongly Anisotropic Magnesiowüstite in Earth's Lower Mantle

Journal Article · · Journal of Geophysical Research. Solid Earth
DOI:https://doi.org/10.1029/2017JB015349· OSTI ID:1472128

Abstract The juxtaposition of a liquid iron‐dominant alloy against a mixture of silicate and oxide minerals at Earth's core‐mantle boundary is associated with a wide range of complex seismological features. One category of observed structures is ultralow‐velocity zones, which are thought to correspond to either aggregates of partially molten material or solid, iron‐enriched assemblages. We measured the phonon dispersion relations of (Mg,Fe) O magnesiowüstite containing 76 mol % FeO, a candidate ultralow‐velocity zone phase, at high pressures using high‐energy resolution inelastic X‐ray scattering. From these measurements, we find that magnesiowüstite becomes strongly elastically anisotropic with increasing pressure, potentially contributing to a significant proportion of seismic anisotropy detected near the base of the mantle.

Research Organization:
Argonne National Laboratory (ANL), Argonne, IL (United States)
Sponsoring Organization:
National Science Foundation (NSF); Consortium for Materials Properties Research in Earth Sciences (COMPRES); USDOE
Grant/Contract Number:
AC02-06CH11357; DE‐AC02‐06CH11357; DE‐FG02‐94ER14466
OSTI ID:
1472128
Alternate ID(s):
OSTI ID: 1454624
Journal Information:
Journal of Geophysical Research. Solid Earth, Vol. 123, Issue 6; ISSN 2169-9313
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 18 works
Citation information provided by
Web of Science

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Cited By (1)

Lowermost Mantle Anisotropy Beneath Africa From Differential SKSSKKS Shear‐Wave Splitting journal August 2019

Figures / Tables (8)