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Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans.: 1 The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System, and has made important contributions to the understanding of a number of processes…
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elements rocks earth planets chemical iron metals silica isotopes ocean fractionation minerals form may composition trace one example two concentrations
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Geochemistry | is a | science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans | 0.90 | text |
| Geochemistry | is a | Goldschmidt classification | 0.90 | text |
| the Earth's crust | instance of | Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems | 0.80 | text |
| its oceans | instance of | Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems | 0.80 | text |
| reaction rate | instance of | Kinetic fractionation generally is enhanced compared to equilibrium fractionation and depends on factors | 0.80 | text |
| reaction pathway | instance of | Kinetic fractionation generally is enhanced compared to equilibrium fractionation and depends on factors | 0.80 | text |
| bond energy | instance of | Kinetic fractionation generally is enhanced compared to equilibrium fractionation and depends on factors | 0.80 | text |
| Ca | instance of | First to condense are materials rich in refractory elements | 0.80 | text |
| Al | instance of | First to condense are materials rich in refractory elements | 0.80 | text |
| carbonates | instance of | of the Earth is composed of non-silicate minerals | 0.80 | text |
| oxides | instance of | of the Earth is composed of non-silicate minerals | 0.80 | text |
| and sulfides.The other determining factor | instance of | of the Earth is composed of non-silicate minerals | 0.80 | text |
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