Abstract
A melting experiment has been made on a natural lherzolite (spinel lherzolite, KLB‐1) at 20 GPa and 2160°C under hydrous conditions. The stable phase assemblage is liquid, garnet, and modified spinel, which is replaced by phase B above the melting temperature of modified spinel, and garnet is the liquidus phase at this pressure.
| Original language | English |
|---|---|
| Pages (from-to) | 181-184 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 13 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - Mar 1986 |
| Externally published | Yes |
All Science Journal Classification (ASJC) codes
- Geophysics
- General Earth and Planetary Sciences
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