| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2007PNAS..104.9139C |
| P356 | DOI | 10.1073/PNAS.0608075104 |
| P8608 | Fatcat ID | release_7i3xyxa3jrhuxblq4k4dgcnlvm |
| P932 | PMC publication ID | 1890460 |
| P698 | PubMed publication ID | 17483461 |
| P5875 | ResearchGate publication ID | 6348856 |
| P50 | author | Barbara Romanowicz | Q2884020 |
| Fabio Cammarano | Q59763600 | ||
| P2860 | cites work | Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 | Q29029100 |
| Deep-mantle high-viscosity flow and thermochemical structure inferred from seismic and geodynamic data | Q30650754 | ||
| Whole-mantle convection and the transition-zone water filter | Q34227876 | ||
| Probabilistic tomography maps chemical heterogeneities throughout the lower mantle | Q34363126 | ||
| Mantle shear-wave tomography and the fate of subducted slabs | Q42038195 | ||
| Preliminary reference Earth model | Q55868389 | ||
| Generalized nonlinear inverse problems solved using the least squares criterion | Q56532217 | ||
| Qtomography of the upper mantle using three-component long-period waveforms | Q57574991 | ||
| A possible role for garnet pyroxenite in the origin of the "garnet signature" in MORB | Q57857421 | ||
| Seismic constraints on temperature of the Australian uppermost mantle | Q57884472 | ||
| A three-dimensional radially anisotropic model of shear velocity in the whole mantle | Q57890304 | ||
| Elasticity of forsterite to 16 GPa and the composition of the upper mantle | Q59038773 | ||
| Transition region of the Earth's upper mantle | Q59056516 | ||
| Normal-Mode and Free-Air Gravity Constraints on Lateral Variations in Velocity and Density of Earth's Mantle | Q60704643 | ||
| Geodynamic evidence for a chemically depleted continental tectosphere | Q73281079 | ||
| Elastic moduli of wadsleyite (beta-Mg2SiO4) to 7 gigapascals and 873 kelvin | Q95435481 | ||
| P433 | issue | 22 | |
| P407 | language of work or name | English | Q1860 |
| P304 | page(s) | 9139-9144 | |
| P577 | publication date | 2007-05-02 | |
| P1433 | published in | Proceedings of the National Academy of Sciences of the United States of America | Q1146531 |
| P1476 | title | Insights into the nature of the transition zone from physically constrained inversion of long-period seismic data | |
| P478 | volume | 104 |
| Q27336157 | Compositional mantle layering revealed by slab stagnation at ~1000-km depth |
| Q57852538 | Conductivity structure of the lithosphere-asthenosphere boundary beneath the eastern North American margin |
| Q105605097 | Elasticity of hydrous wadsleyite to 12 GPa: Implications for Earth's transition zone |
| Q46477052 | Geophysics. The thickness of tectonic plates |
| Q60719155 | High-resolution image of the geometry and thickness of the subducting Nazca lithosphere beneath northern Chile |
| Q57890004 | Inferring upper-mantle structure by full waveform tomography with the spectral element method |
| Q60153925 | Lithospheric Structure of the Northern Ordos From Ambient Noise and Teleseismic Surface Wave Tomography |
| Q57852895 | Mapping spherical seismic into physical structure: biases from 3-D phase-transition and thermal boundary-layer heterogeneity |
| Q57890085 | North American lithospheric discontinuity structure imaged byPsandSpreceiver functions |
| Q107269089 | On mantle chemical and thermal heterogeneities and anisotropy as mapped by inversion of global surface wave data |
| Q37282963 | Some recent advances in understanding the mineralogy of Earth's deep mantle |
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