Melting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray Diffraction

@article{Anzellini2013MeltingOI,
  title={Melting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray Diffraction},
  author={Simone Anzellini and Agn{\`e}s Dewaele and Mohamed Mezouar and Paul Loubeyre and Guillaume Morard},
  journal={Science},
  year={2013},
  volume={340},
  pages={464 - 466}
}
Hot Enough to Melt Iron Earth's core is divided into a fluid outer core and a solid inner core, both composed predominately of iron at extremely high pressures and temperatures. The boundary between these two regions is largely controlled by the melting point of iron at ∼330 GPa, which in turn influences heat transfer and geodynamo generation. Anzellini et al. (p. 464, see the Perspective by Fei) compressed iron in a laser-heated diamond anvil cell, tracking its structure and texture by using… 

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