Metal-silicate partitioning and the incompatibility of S and Si during core formation
We have determined the partitioning of a number of siderophile and lithophile elements between liquid metal and liquid silicate phases under the high temperature, low pressure conditions at which core segregation is considered to have originated [2]. Oxygen fugacity was varied from 2 to 6 log units...
| Prif Awduron: | , |
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| Fformat: | Journal article |
| Iaith: | English |
| Cyhoeddwyd: |
1997
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