Mixing, volatile loss and compositional change during impact-driven accretion of the Earth.
The degree to which efficient mixing of new material or losses of earlier accreted material to space characterize the growth of Earth-like planets is poorly constrained and probably changed with time. These processes can be studied by parallel modelling of data from different radiogenic isotope syst...
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| Formaat: | Journal article |
| Taal: | English |
| Gepubliceerd in: |
2004
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