An experimental study of water in nominally anhydrous minerals in the upper mantle near the water-saturated solidus
The incorporation of water in olivine and pyroxenes interlayered within fertile lherzolite compositions was explored experimentally near the wet solidus of lherzolite at 2·5 and 4 GPa. The concentrations and activities of water were varied to establish t
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|Source:||Journal of Petrology|
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