High-pressure and High-temperature Experiments in the Multi-anvil Apparatus
3:04
Sample Analysis
4:08
Results: 3D Reconstruction of Fe-FeS Melt in an Olivine Matrix
5:33
Conclusion
The high-pressure and high-temperature experiments described here mimic planet interior differentiation processes. The processes are visualized and better understood by high-resolution 3D imaging and quantitative chemical analysis.