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In planetary science, planetary differentiation is the process by which the chemical elements of a planetary body accumulate in different areas of that body, due to their physical or chemical behavior (e.g. density and chemical affinities). The process of planetary differentiation is mediated by partial melting with heat from radioactive isotope decay…
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differentiation materials elements process core earth material planetary chemical density iron mantle magma body crust lighter accretion large heating formation
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Planetary differentiation | is a | process by which the chemical elements of a planetary body accumulate in different areas of that body | 0.90 | text |
| plagioclase tends to rise | instance of | a light mineral | 0.80 | text |
| granite are abundant in the Earth's upper crust | instance of | Diapirs of molten low-density silicate rocks | 0.80 | text |
| methane | instance of | they may be hydrocarbons | 0.80 | text |
| water as liquid or ice | instance of | they may be hydrocarbons | 0.80 | text |
| or frozen carbon dioxide.Fractional melting | instance of | they may be hydrocarbons | 0.80 | text |
| crystallizationMagma in the Earth is produced by partial melting of a source rock | instance of | they may be hydrocarbons | 0.80 | text |
| ultimately in the mantle | instance of | they may be hydrocarbons | 0.80 | text |
| nickel | instance of | Siderophile elements | 0.80 | text |
| cobalt can dissolve in molten iron | instance of | Siderophile elements | 0.80 | text |
| Planetary differentiation | related to Core formation mechanisms | Core | 0.60 | section |
| Planetary differentiation | related to Core formation mechanisms | Examples | 0.60 | section |
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