| scholarly article | Q13442814 |
| P6179 | Dimensions Publication ID | 1011640436 |
| P356 | DOI | 10.1038/365147A0 |
| P2888 | exact match | https://scigraph.springernature.com/pub.10.1038/365147a0 |
| P50 | author | John Vidale | Q6261987 |
| P2093 | author name string | H. M. Benz | |
| P2860 | cites work | Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications | Q30040418 |
| Preliminary reference Earth model | Q55868389 | ||
| Transition region of the Earth's upper mantle | Q59056516 | ||
| Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity | Q59083388 | ||
| Global mapping of topography on the 660-km discontinuity | Q59092563 | ||
| Upper-mantle seismic discontinuities and the thermal structure of subduction zones | Q59092566 | ||
| The system Mg2SiO4-Fe2SiO4at high pressures and temperatures: Precise determination of stabilities of olivine, modified spinel, and spinel | Q63930580 | ||
| Seismic Waves Reflected from Discontinuities within Earth's Upper Mantle | Q80895632 | ||
| S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity | Q107112369 | ||
| Precursors to P‘P’ re-examined using broad-band data | Q107112442 | ||
| Reflections of P'P' from upper mantle discontinuities beneath the Mid-Atlantic Ridge | Q107113927 | ||
| P433 | issue | 6442 | |
| P407 | language of work or name | English | Q1860 |
| P304 | page(s) | 147-150 | |
| P577 | publication date | 1993-09-01 | |
| P1433 | published in | Nature | Q180445 |
| P1476 | title | Sharpness of upper-mantle discontinuities determined from high-frequency reflections | |
| P478 | volume | 365 |
| Q60716045 | A discussion on “The 410-km-depth discontinuity: A sharpness estimate from near-critical reflections” by Vidale et al |
| Q59797235 | A mystery in the mantle |
| Q59032172 | A question of reduction |
| Q107269113 | Application of Ps Scattering Kernels to Imaging the Mantle Transition Zone With Receiver Functions |
| Q52624881 | Compositional heterogeneity near the base of the mantle transition zone beneath Hawaii. |
| Q59857935 | Constraining seismic velocity and density for the mantle transition zone with reflected and transmitted waveforms |
| Q59817522 | Detailed nature of the 660 km region of the mantle from global receiver function data |
| Q107271109 | Detailed structure and sharpness of upper mantle discontinuities in the Tonga subduction zone from regional broadband arrays |
| Q107269086 | Discontinuity structure of the mantle transition zone beneath the North China Craton from receiver function migration |
| Q107275091 | Dynamic phase boundary topography by latent heat effects |
| Q59038887 | Earth dons a different mantle |
| Q105594427 | Ferrous iron partitioning between magnesium silicate perovskite and ferropericlase and the composition of perovskite in the Earth's lower mantle |
| Q107275306 | Global de-correlation of the topography of transition zone discontinuities |
| Q107271075 | Global variability of transition zone thickness |
| Q60722528 | In situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg2SiO4 |
| Q60722222 | Influence of Water on Major Phase Transitions in the Earth's Mantle |
| Q59054557 | Iron partitioning in a pyrolite mantle and the nature of the 410-km seismic discontinuity |
| Q60719230 | Lithospheric and upper mantle structure of southern Tibet from a seismological passive source experiment |
| Q59797162 | Mantle discontinuities under southern Africa from precursors to P′ P′df |
| Q107275326 | Molecular dynamics simulation of MgSiO3 perovskite and the 660-km seismic discontinuity |
| Q56680244 | Olivine-wadsleyite transition in the system (Mg,Fe)2SiO4 |
| Q107275311 | Phase transformations and partitioning relations in peridotite under lower mantle conditions |
| Q56680247 | Phase transition Clapeyron slopes and transition zone seismic discontinuity topography |
| Q107275476 | Postspinel transformations in the system Mg2SiO4Fe2SiO4 element partitioning, calorimetry, and thermodynamic calculation |
| Q60709328 | Seismic discontinuity at the top of D″: A world-wide feature? |
| Q59056462 | Seismic evidence for a 920-km discontinuity in the mantle |
| Q28198144 | Seismic observations of splitting of the mid-transition zone discontinuity in Earth's mantle |
| Q59715026 | Seismic scattering at the top of the mantle Transition Zone |
| Q59858000 | Seismic studies of the upper mantle and transition zone |
| Q35680532 | Single-crystal Brillouin spectroscopy with CO2 laser heating and variable q. |
| Q63930525 | Single-crystal elasticity of ringwoodite to high pressures and high temperatures: implications for 520 km seismic discontinuity |
| Q63930557 | Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite |
| Q59797095 | Survey of precursors to P′P′: Fine structure of mantle discontinuities |
| Q59797215 | The 410-km-depth discontinuity: A sharpness estimate from near-critical reflections |
| Q107269150 | The Transition Zone Beneath West Argentina‐Central Chile Using P ‐to‐ S Converted Waves |
| Q105594532 | The effect of water on the 410-km discontinuity: An experimental study |
| Q60065753 | The mantle in sharper focus |
| Q105594526 | The structure and sharpness of (Mg,Fe)2SiO4 phase transformations in the transition zone |
| Q59807033 | Topography of the transition zone seismic discontinuities |
| Q59857997 | Topography on the 410-km seismic velocity discontinuity near subduction zones from stacking ofsS,sP, andpPprecursors |
| Q60700897 | Upper mantle compressional velocity structure beneath the West Mediterranean Basin |
| Q107275344 | Upper-mantle seismic discontinuities in a subduction zone (Japan) investigated from P to S converted waves |
| Q107275350 | Velocity anomalies and spatial distributions of physical properties in horizontally lying slabs beneath the Northwestern Pacific region |
| Q59857913 | observations of high-frequency scattered energy associated with the core PhasePKKP |
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