Single-crystal elasticity of (Al,Fe)-bearing bridgmanite and seismic shear wave radial anisotropy at the topmost lower mantle

Suyu Fu, Jing Yang, Noriyoshi Tsujino, Takuo Okuchi, Narangoo Purevjav, Jung Fu Lin

Research output: Contribution to journalArticle

Abstract

In this study, we investigated the single-crystal elasticity of (Al,Fe)-bearing bridgmanite (Bgm)with chemical compositions of Mg 0.95 Fe 0.033 2+ Fe 0.027 3+ Al 0.04 Si 0.96 O 3 (Fe6-Al4-Bgm)and Mg 0.89 Fe 0.024 2+ Fe 0.096 3+ Al 0.11 Si 0.89 O 3 (Fe12-Al11-Bgm)using combined experimental results from Brillouin light scattering (BLS), impulsive stimulated light scattering (ISLS), and X-ray diffraction (XRD)measurements in diamond anvil cells at 25 and 35 GPa. Based on experimentally measured compressional and shear wave velocities (V P , V S )as a function of azimuthal angles within selected crystal platelets that are sensitive to derivation of nine elastic constants for each composition, we reliably derived the full elastic constants of Fe6-Al4-Bgm and Fe12-Al11-Bgm at the two experimental pressures. Our results show that the combined Fe and Al substitution results in a reduction of both V S and V P in Fe12-Al11-Bgm up to 2.6(±0.5)% and 1.5(±0.3)%, respectively, compared with those in Fe6-Al4-Bgm at the experimental pressures. In particular, we observed strong combined Fe and Al effects on V S splitting anisotropy of (Al,Fe)-bearing Bgm at the two experimental pressures: Fe6-Al4-Bgm exhibits the highest V S splitting anisotropy of ∼8.23-9.0% along the [001]direction, while the direction shifts to the midway between [100]and [001]directions for Fe12-Al11-Bgm with V S splitting anisotropy of ∼7.68-11.06%. Combining the single-crystal elasticity data of Fe6-Al4-Bgm and Fe12-Al11-Bgm with the crystallographic preferred orientation (CPO)results of deformed Bgm at relevant lower-mantle pressure-temperature (P-T)conditions from literature, we modeled the seismic V S radial anisotropy of deformed (Al,Fe)-bearing Bgm near a subducting slab at conditions relevant to the topmost lower mantle. Taking into account the Fe and Al contents in (Al,Fe)-bearing Bgm with depth in the Earth's topmost lower mantle, the results of our model show that the deformation of Fe6-Al4-Bgm and Fe12-Al11-Bgm crystals would produce ∼0.9% and ∼0.8% V S radial anisotropy at depths of ∼670 and ∼920 km, respectively. These findings provide mineral physics explanations to the distinct seismically-detected V S radial anisotropies at the topmost lower mantle near subducted slabs, especially in the Tonga-Kermadec subduction region.

Original languageEnglish
Pages (from-to)116-126
Number of pages11
JournalEarth and Planetary Science Letters
Volume518
DOIs
Publication statusPublished - Jul 15 2019

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Bearings (structural)
Seismic waves
Shear waves
lower mantle
seismic wave
elasticity
S waves
S-wave
Elasticity
Earth mantle
Anisotropy
anisotropy
elastic properties
Single crystals
crystal
single crystals
light scattering
Elastic constants
Light scattering
slab

Keywords

  • bridgmanite
  • seismic anisotropy
  • single-crystal elasticity
  • topmost lower mantle

ASJC Scopus subject areas

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

Cite this

Single-crystal elasticity of (Al,Fe)-bearing bridgmanite and seismic shear wave radial anisotropy at the topmost lower mantle. / Fu, Suyu; Yang, Jing; Tsujino, Noriyoshi; Okuchi, Takuo; Purevjav, Narangoo; Lin, Jung Fu.

In: Earth and Planetary Science Letters, Vol. 518, 15.07.2019, p. 116-126.

Research output: Contribution to journalArticle

Fu, Suyu ; Yang, Jing ; Tsujino, Noriyoshi ; Okuchi, Takuo ; Purevjav, Narangoo ; Lin, Jung Fu. / Single-crystal elasticity of (Al,Fe)-bearing bridgmanite and seismic shear wave radial anisotropy at the topmost lower mantle. In: Earth and Planetary Science Letters. 2019 ; Vol. 518. pp. 116-126.
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abstract = "In this study, we investigated the single-crystal elasticity of (Al,Fe)-bearing bridgmanite (Bgm)with chemical compositions of Mg 0.95 Fe 0.033 2+ Fe 0.027 3+ Al 0.04 Si 0.96 O 3 (Fe6-Al4-Bgm)and Mg 0.89 Fe 0.024 2+ Fe 0.096 3+ Al 0.11 Si 0.89 O 3 (Fe12-Al11-Bgm)using combined experimental results from Brillouin light scattering (BLS), impulsive stimulated light scattering (ISLS), and X-ray diffraction (XRD)measurements in diamond anvil cells at 25 and 35 GPa. Based on experimentally measured compressional and shear wave velocities (V P , V S )as a function of azimuthal angles within selected crystal platelets that are sensitive to derivation of nine elastic constants for each composition, we reliably derived the full elastic constants of Fe6-Al4-Bgm and Fe12-Al11-Bgm at the two experimental pressures. Our results show that the combined Fe and Al substitution results in a reduction of both V S and V P in Fe12-Al11-Bgm up to 2.6(±0.5){\%} and 1.5(±0.3){\%}, respectively, compared with those in Fe6-Al4-Bgm at the experimental pressures. In particular, we observed strong combined Fe and Al effects on V S splitting anisotropy of (Al,Fe)-bearing Bgm at the two experimental pressures: Fe6-Al4-Bgm exhibits the highest V S splitting anisotropy of ∼8.23-9.0{\%} along the [001]direction, while the direction shifts to the midway between [100]and [001]directions for Fe12-Al11-Bgm with V S splitting anisotropy of ∼7.68-11.06{\%}. Combining the single-crystal elasticity data of Fe6-Al4-Bgm and Fe12-Al11-Bgm with the crystallographic preferred orientation (CPO)results of deformed Bgm at relevant lower-mantle pressure-temperature (P-T)conditions from literature, we modeled the seismic V S radial anisotropy of deformed (Al,Fe)-bearing Bgm near a subducting slab at conditions relevant to the topmost lower mantle. Taking into account the Fe and Al contents in (Al,Fe)-bearing Bgm with depth in the Earth's topmost lower mantle, the results of our model show that the deformation of Fe6-Al4-Bgm and Fe12-Al11-Bgm crystals would produce ∼0.9{\%} and ∼0.8{\%} V S radial anisotropy at depths of ∼670 and ∼920 km, respectively. These findings provide mineral physics explanations to the distinct seismically-detected V S radial anisotropies at the topmost lower mantle near subducted slabs, especially in the Tonga-Kermadec subduction region.",
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AU - Fu, Suyu

AU - Yang, Jing

AU - Tsujino, Noriyoshi

AU - Okuchi, Takuo

AU - Purevjav, Narangoo

AU - Lin, Jung Fu

PY - 2019/7/15

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N2 - In this study, we investigated the single-crystal elasticity of (Al,Fe)-bearing bridgmanite (Bgm)with chemical compositions of Mg 0.95 Fe 0.033 2+ Fe 0.027 3+ Al 0.04 Si 0.96 O 3 (Fe6-Al4-Bgm)and Mg 0.89 Fe 0.024 2+ Fe 0.096 3+ Al 0.11 Si 0.89 O 3 (Fe12-Al11-Bgm)using combined experimental results from Brillouin light scattering (BLS), impulsive stimulated light scattering (ISLS), and X-ray diffraction (XRD)measurements in diamond anvil cells at 25 and 35 GPa. Based on experimentally measured compressional and shear wave velocities (V P , V S )as a function of azimuthal angles within selected crystal platelets that are sensitive to derivation of nine elastic constants for each composition, we reliably derived the full elastic constants of Fe6-Al4-Bgm and Fe12-Al11-Bgm at the two experimental pressures. Our results show that the combined Fe and Al substitution results in a reduction of both V S and V P in Fe12-Al11-Bgm up to 2.6(±0.5)% and 1.5(±0.3)%, respectively, compared with those in Fe6-Al4-Bgm at the experimental pressures. In particular, we observed strong combined Fe and Al effects on V S splitting anisotropy of (Al,Fe)-bearing Bgm at the two experimental pressures: Fe6-Al4-Bgm exhibits the highest V S splitting anisotropy of ∼8.23-9.0% along the [001]direction, while the direction shifts to the midway between [100]and [001]directions for Fe12-Al11-Bgm with V S splitting anisotropy of ∼7.68-11.06%. Combining the single-crystal elasticity data of Fe6-Al4-Bgm and Fe12-Al11-Bgm with the crystallographic preferred orientation (CPO)results of deformed Bgm at relevant lower-mantle pressure-temperature (P-T)conditions from literature, we modeled the seismic V S radial anisotropy of deformed (Al,Fe)-bearing Bgm near a subducting slab at conditions relevant to the topmost lower mantle. Taking into account the Fe and Al contents in (Al,Fe)-bearing Bgm with depth in the Earth's topmost lower mantle, the results of our model show that the deformation of Fe6-Al4-Bgm and Fe12-Al11-Bgm crystals would produce ∼0.9% and ∼0.8% V S radial anisotropy at depths of ∼670 and ∼920 km, respectively. These findings provide mineral physics explanations to the distinct seismically-detected V S radial anisotropies at the topmost lower mantle near subducted slabs, especially in the Tonga-Kermadec subduction region.

AB - In this study, we investigated the single-crystal elasticity of (Al,Fe)-bearing bridgmanite (Bgm)with chemical compositions of Mg 0.95 Fe 0.033 2+ Fe 0.027 3+ Al 0.04 Si 0.96 O 3 (Fe6-Al4-Bgm)and Mg 0.89 Fe 0.024 2+ Fe 0.096 3+ Al 0.11 Si 0.89 O 3 (Fe12-Al11-Bgm)using combined experimental results from Brillouin light scattering (BLS), impulsive stimulated light scattering (ISLS), and X-ray diffraction (XRD)measurements in diamond anvil cells at 25 and 35 GPa. Based on experimentally measured compressional and shear wave velocities (V P , V S )as a function of azimuthal angles within selected crystal platelets that are sensitive to derivation of nine elastic constants for each composition, we reliably derived the full elastic constants of Fe6-Al4-Bgm and Fe12-Al11-Bgm at the two experimental pressures. Our results show that the combined Fe and Al substitution results in a reduction of both V S and V P in Fe12-Al11-Bgm up to 2.6(±0.5)% and 1.5(±0.3)%, respectively, compared with those in Fe6-Al4-Bgm at the experimental pressures. In particular, we observed strong combined Fe and Al effects on V S splitting anisotropy of (Al,Fe)-bearing Bgm at the two experimental pressures: Fe6-Al4-Bgm exhibits the highest V S splitting anisotropy of ∼8.23-9.0% along the [001]direction, while the direction shifts to the midway between [100]and [001]directions for Fe12-Al11-Bgm with V S splitting anisotropy of ∼7.68-11.06%. Combining the single-crystal elasticity data of Fe6-Al4-Bgm and Fe12-Al11-Bgm with the crystallographic preferred orientation (CPO)results of deformed Bgm at relevant lower-mantle pressure-temperature (P-T)conditions from literature, we modeled the seismic V S radial anisotropy of deformed (Al,Fe)-bearing Bgm near a subducting slab at conditions relevant to the topmost lower mantle. Taking into account the Fe and Al contents in (Al,Fe)-bearing Bgm with depth in the Earth's topmost lower mantle, the results of our model show that the deformation of Fe6-Al4-Bgm and Fe12-Al11-Bgm crystals would produce ∼0.9% and ∼0.8% V S radial anisotropy at depths of ∼670 and ∼920 km, respectively. These findings provide mineral physics explanations to the distinct seismically-detected V S radial anisotropies at the topmost lower mantle near subducted slabs, especially in the Tonga-Kermadec subduction region.

KW - bridgmanite

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KW - single-crystal elasticity

KW - topmost lower mantle

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