Ar and K partitioning between clinopyroxene and silicate melt to 8 GPa
The relative incompatibility of Ar and K are fundamental parameters in understanding the degassing history of the mantle. Clinopyroxene is the main host for K in most of the upper mantle, playing an important role in controlling the K/Ar ratio of residual mantle and the subsequent time-integrated ev...
Main Authors: | , , , , , |
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Format: | Journal article |
Language: | English |
Published: |
2002
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