Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt
We performed experiments at 3.0 GPa and 1530-1565 °C to investigate the effects of crystal composition on trace element partitioning between garnet and anhydrous silicate melt. Bulk compositions along the pyrope (Py: Mg3Al2Si3O12)-grossular (Gr: Ca3Al2Si3O12) join, doped with a suite of trace elemen...
| Egile Nagusiak: | , , |
|---|---|
| Formatua: | Journal article |
| Hizkuntza: | English |
| Argitaratua: |
1999
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