| scholarly article | Q13442814 |
| P819 | ADS bibcode | 1992Natur.355..791S |
| P6179 | Dimensions Publication ID | 1009191314 |
| P356 | DOI | 10.1038/355791A0 |
| P2888 | exact match | https://scigraph.springernature.com/pub.10.1038/355791a0 |
| P50 | author | Peter M. Shearer | Q57725827 |
| P2093 | author name string | T. Guy Masters | |
| P2860 | cites work | Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications | Q30040418 |
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| The post-spinel phase of forsterite | Q59079295 | ||
| Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuity | Q59083388 | ||
| Horizontal shear flow in the mantle beneath the Tonga arc | Q59085007 | ||
| Tomographic imaging of subducted lithosphere below northwest Pacific island arcs | Q59098742 | ||
| Investigation of deep slab structure using long-period S waves | Q59797290 | ||
| Deep Slabs, Geochemical Heterogeneity, and the Large-Scale Structure of Mantle Convection: Investigation of an Enduring Paradox | Q60568902 | ||
| Negative Pressure-Temperature Slopes for Reactions Formign MgSiO3 Perovskite from Calorimetry | Q81195667 | ||
| Mapping the upper mantle: Three-dimensional modeling of earth structure by inversion of seismic waveforms | Q97999071 | ||
| S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuity | Q107112369 | ||
| Long-wavelengthS-wave velocity structure throughout the mantle | Q107112388 | ||
| Some geophysical constraints on the chemical composition of the earth's lower mantle | Q107274970 | ||
| The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgOFeOSiO2 | Q107274973 | ||
| P433 | issue | 6363 | |
| P407 | language of work or name | English | Q1860 |
| P304 | page(s) | 791-796 | |
| P577 | publication date | 1992-02-01 | |
| P1433 | published in | Nature | Q180445 |
| P1476 | title | Global mapping of topography on the 660-km discontinuity | |
| P478 | volume | 355 |
| Q59875218 | A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China |
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