| scholarly article | Q13442814 |
| P356 | DOI | 10.1029/GM117P0237 |
| P50 | author | Guilhem Barruol | Q57906667 |
| P2093 | author name string | D. Mainprice | |
| W. Ben Ismaïl | |||
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| The cubic-tetragonal phase transition in the system majorite (Mg4Si4O12) – pyrope (Mg3Al2Si3O12), and garnet symmetry in the Earth's transition zone | Q56851807 | ||
| Seismic Evidence for Partial Melt at the Base of Earth's Mantle | Q57380070 | ||
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| Absence of an aluminous phase in the upper part of the Earth's lower mantle | Q59081249 | ||
| Transformation of stishovite to a denser phase at lower-mantle pressures | Q59092340 | ||
| Global mapping of topography on transition zone velocity discontinuities by stackingSSprecursors | Q59857989 | ||
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| Microstructures in β-Mg1.8Fe0.2SiO4 experimentally deformed at transition-zone conditions | Q63930568 | ||
| A temperature profile of the mantle transition zone | Q63930577 | ||
| 3-D seismic velocities calculated from lattice-preferred orientation and reflectivity of a lower crustal section: examples of the Val Sesia section (Ivrea zone, northern Italy) | Q64029112 | ||
| Anisotropy of the inner core inferred fromPKIKPtravel times | Q64388230 | ||
| Structure and elasticity of MgO at high pressure | Q67003906 | ||
| Ultradeep (>300 kilometers) ultramafic xenoliths: petrological evidence from the transition zone | Q80913081 | ||
| Ultradeep (greater than 300 kilometers), ultramafic upper mantle xenoliths | Q80916654 | ||
| Single-crystal elastic properties of the modified spinel (Beta) phase of magnesium orthosilicate | Q81023583 | ||
| Elasticity of MgSiO3 in the Perovskite Structure | Q81145234 | ||
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| Orientation imaging: The emergence of a new microscopy | Q101074990 | ||
| Seismic anisotropy and shear-wave splitting in lower-crustal and upper-mantle rocks from the Ivrea Zone—experimental and calculated data | Q104212548 | ||
| Azimuthal anisotropy in the lithosphere from observations of long-period S-waves | Q107112623 | ||
| Seismic Anisotropy in the Deep Mantle, Boundary Layers and the Geometry of Mantle Convection | Q107274947 | ||
| Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle | Q107275011 | ||
| Synthesis and re-investigation of the elastic properties of single-crystal magnesium silicate perovskite | Q107275044 | ||
| Phase transformations and their bearing on the constitution and dynamics of the mantle | Q107275057 | ||
| P304 | page(s) | 237-264 | |
| P577 | publication date | 2000-01-01 | |
| P1433 | published in | Geophysical Monograph | Q29043683 |
| P1476 | title | The Seismic anisotropy of the Earth's mantle: From single crystal to polycrystal |
| Q64029096 | A Tertiary asthenospheric flow beneath the southern French Massif Central indicated by upper mantle seismic anisotropy and related to the west Mediterranean extension |
| Q64029087 | An integrated study of microstructural, geochemical, and seismic properties of the lithospheric mantle above the Kerguelen plume (Indian Ocean) |
| Q91427055 | Anhydrous Phase B: Transmission Electron Microscope Characterization and Elastic Properties |
| Q61717015 | Azimuthal seismic anisotropy of 70 Ma Pacific-plate upper mantle |
| Q107271033 | Crystallographic preferred orientation produced by diffusional creep of harzburgite: Effects of chemical interactions among phases during plastic flow |
| Q105242985 | Deformation of olivine-spinel aggregates in the system (Mg,Ni)2GeO4 deformed to high strain in torsion: Implications for upper mantle anisotropy |
| Q57835456 | Deformation of polycrystalline MgO at pressures of the lower mantle |
| Q43530675 | Development of anisotropic structure in the Earth's lower mantle by solid-state convection |
| Q57885493 | Differences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivity |
| Q61773553 | Elasticity and strength of hydrous ringwoodite at high pressure |
| Q60719550 | Evidence of midmantle anisotropy from shear wave splitting and the influence of shear-coupledPwaves |
| Q60710075 | Inversion for anisotropy from non-double-couple components of moment tensors |
| Q104212539 | Large-scale flow of Indian Ocean asthenosphere driven by Réunion plume |
| Q60700241 | Mapping upper mantle flow beneath French Polynesia from broadband ocean bottom seismic observations |
| Q52861995 | Mid-mantle deformation inferred from seismic anisotropy. |
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| Q57102617 | Olivine crystals align during diffusion creep of Earth's upper mantle |
| Q60700246 | PLUME investigates South Pacific Superswell |
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| Q63946411 | Radial anisotropy in seismic reference models of the mantle |
| Q58051389 | Rock seismic anisotropy of the low-velocity zone beneath the volcanic front in the mantle wedge |
| Q59806776 | SKSsplitting measurements in the Apenninic-Tyrrhenian domain (Italy) and their relation with lithospheric subduction and mantle convection |
| Q59806750 | Seismic anisotropy reveals focused mantle flow around the Calabrian slab (Southern Italy) |
| Q63432675 | Seismicity of the Bora‐Tullu Moye Volcanic Field, 2016–2017 |
| Q58779801 | Significant seismic anisotropy beneath the southern Lhasa Terrane, Tibetan Plateau |
| Q48267026 | Stability and anisotropy of (FexNi1-x)2O under high pressure and implications in Earth's and super-Earths' core |
| Q60700011 | Statistical properties of seismic anisotropy predicted by upper mantle geodynamic models |
| Q107271107 | Strain-induced seismic anisotropy of wadsleyite polycrystals and flow patterns in the mantle transition zone |
| Q64029099 | The Kaapvaal craton seismic anisotropy: Petrophysical analyses of upper mantle kimberlite nodules |
| Q59806773 | Toroidal mantle flow around the Calabrian slab (Italy) from SKS splitting |
| Q60700242 | Upper mantle anisotropy beneath Australia and Tahiti fromPwave polarization: Implications for real-time earthquake location |
| Q58209063 | Upper mantle anisotropy beneath the Seychelles microcontinent |
| Q58051386 | Uppermost mantle anisotropy beneath the southern Laurentian margin: Evidence from Knippa peridotite xenoliths, Texas |
| Q73312601 | Weak B‐Type Olivine Fabric Induced by Fast Compaction of Crystal Mush in a Crustal Magma Reservoir |
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