Studium rovnováhy mezi klesajícími kapkami železa a roztavenými silikáty v magmatických oceánech
During the Earth's accretion process deep magma oceans were episodically formed. Differentiation of iron took place within the melted zone and small droplets of iron were sinking to the base of the magma ocean due to the density contrast. In the present work we study the process of equilibratio...
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| Format: | Dissertation |
| Language: | English |
| Published: |
2008
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| Online Access: | http://www.nusl.cz/ntk/nusl-292931 |