Probing planetary core structure and dynamics using density and sound velocity

Articles in the same Issue

1. Highlights and Breakthroughs
2. Probing planetary core structure and dynamics using density and sound velocity
3. Mapping the distribution of melt during anatexis at the source area of crustal granites by synchrotron μ-XRF
4. Geochemical constraints on residual metal and sulfide in the sources of lunar mare basalts
5. High-temperature behavior of natural ferrierite: In-situ synchrotron X-ray powder diffraction study
6. The crystal chemistry of the sakhaite–harkerite solid solution
7. Quantitative analysis of H-species in anisotropic minerals by unpolarized infrared spectroscopy: An experimental evaluation
8. Liquid properties in the Fe-FeS system under moderate pressure: Tool box to model small planetary cores
9. Solution mechanisms of COHN fluids in melts to upper mantle temperature, pressure, and redox conditions
10. Dating phosphates of the strongly shocked Suizhou chondrite
11. Quantitative measurement of olivine composition in three dimensions using helical-scan X-ray micro-tomography
12. Chemical fingerprints and residence times of olivine in the 1959 Kilauea Iki eruption, Hawaii: Insights into picrite formation
13. Predicting olivine composition using Raman spectroscopy through band shift and multivariate analyses
14. Dehydrogenation and dehydroxylation as drivers of the thermal decomposition of Fe-chlorites
15. High-pressure granulite facies metamorphism (~1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A.
16. Letter
17. Raman elastic geobarometry for anisotropic mineral inclusions
18. Synthesis and crystal structure of Mg-bearing Fe₉O₁₁: New insight in the complexity of Fe-Mg oxides at conditions of the deep upper mantle