The Formation of Planetary Layers: Tracing the Origins of Core, Mantle, and Crust
The planets in our solar system show clear evidence of differentiation. For example, the Earth has a distinct iron core, a rocky mantle, and a thin crust of silicates. Similarly, Mars has a small iron core and a thin silicate crust. The largest planet Jupiter, does not have a solid surface, but it’s believed that […]
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