| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2006GMS...168..131J |
| P356 | DOI | 10.1029/168GM10 |
| P50 | author | Steven D. Jacobsen | Q50635880 |
| P2093 | author name string | Joseph R. Smyth | |
| P2860 | cites work | Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 | Q29029100 |
| Whole-mantle convection and the transition-zone water filter | Q34227876 | ||
| Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite | Q43530263 | ||
| Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States | Q43587644 | ||
| Preliminary reference Earth model | Q55868389 | ||
| Calibration of the ruby pressure gauge to 800 kbar under quasi-hydrostatic conditions | Q56431094 | ||
| The Elastic Behaviour of a Crystalline Aggregate | Q56656592 | ||
| A computer simulation study of OH defects in Mg2SiO4 and Mg2GeO4 spinels | Q57619028 | ||
| Oxidation state of iron in hydrous mantle phases: implications for subduction and mantle oxygen fugacity | Q57854409 | ||
| Experimental evidence for a hydrous transition zone in the early Earth's mantle | Q57854463 | ||
| Storage capacity of H2O in nominally anhydrous minerals in the upper mantle | Q57857324 | ||
| Hydrous modified spinel, Mg1.75SiH0.5O4: A new water reservoir in the mantle transition region | Q57866652 | ||
| Thermal expansion of Mg2SiO4ringwoodite at high pressures | Q57873003 | ||
| Hydroxide in olivine: A quantitative determination of the absolute amount and calibration of the IR spectrum | Q59829722 | ||
| Water transport into the deep mantle and formation of a hydrous transition zone | Q60722490 | ||
| Structural systematics of hydrous ringwoodite and water in Earth’s interior | Q61773552 | ||
| Elasticity and strength of hydrous ringwoodite at high pressure | Q61773553 | ||
| Optical and near infrared spectra of ringwoodite to 21.5 GPa: Implications for radiative heat transport in the mantle | Q61773554 | ||
| Temperature dependence of the elastic moduli of ringwoodite | Q63930509 | ||
| Single-crystal elasticity of ringwoodite to high pressures and high temperatures: implications for 520 km seismic discontinuity | Q63930525 | ||
| Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite | Q63930557 | ||
| First-principles determination of elastic anisotropy and wave velocities of MgO at lower mantle conditions | Q73216160 | ||
| Seismic evidence for water deep in Earth's upper mantle | Q73491022 | ||
| The Effect of H2O on the 410-Kilometer Seismic Discontinuity | Q80949865 | ||
| Comparative Compressibilities of Silicate Spinels: Anomalous Behavior of (Mg,Fe)2SiO4 | Q81056050 | ||
| Traveltimes for global earthquake location and phase identification | Q98140037 | ||
| Equation of state of hydrous Fo90 ringwoodite to 45 GPa by synchrotron powder diffraction | Q105594512 | ||
| Structure and elasticity of single-crystal (Mg,Fe)O and a new method of generating shear waves for gigahertz ultrasonic interferometry | Q105603073 | ||
| Sound velocities and elastic constants of ZnAl2O4 spinel and implications for spinel-elasticity systematics | Q105605152 | ||
| A gigahertz ultrasonic interferometer for the diamond anvil cell and high-pressure elasticity of some iron-oxide minerals | Q105605157 | ||
| High pressure crystal chemistry of hydrous ringwoodite and water in the Earth’s interior | Q105605166 | ||
| Sound velocities and elastic constants of iron-bearing hydrous ringwoodite | Q105605204 | ||
| Is the transition zone an empty water reservoir? Inferences from numerical model of mantle dynamics | Q107269608 | ||
| Thermal equation of state of (Mg0.91Fe0.09)2SiO4 ringwoodite | Q107269626 | ||
| Enhancement of radiative transfer in the upper mantle by OH− in minerals | Q107269657 | ||
| Water partitioning at 660 km depth and evidence for very low water solubility in magnesium silicate perovskite | Q107271094 | ||
| Seismic Anisotropy in the Deep Mantle, Boundary Layers and the Geometry of Mantle Convection | Q107274947 | ||
| Single-crystal elasticity of pyrope and MgO to 20 GPa by Brillouin scattering in the diamond cell | Q107275324 | ||
| Pressure and strain dependence of the strength of sintered polycrystalline Mg2SiO4ringwoodite | Q107288508 | ||
| P304 | page(s) | 131-145 | |
| P577 | publication date | 2013-03-19 | |
| P1476 | title | Effect of Water on the Sound Velocities of Ringwoodite in the Transition Zone |
| Q105594485 | Effects of hydration on the elastic properties of olivine |
| Q62701901 | Mantle Transition Zone Structure Beneath Northeast Asia From 2‐D Triplicated Waveform Modeling: Implication for a Segmented Stagnant Slab |
| Q107271035 | Upper mantle seismic shear discontinuities of the Pacific |
| Q58795977 | Water makes glass elastically stiffer under high-pressure |
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