Peridotite melting at 1.0 and 1.5 GPa: and experimental evaluation of techniques using diamond aggregates and mineral mixes for determination of near-solidus melts
The experimental determination of liquid compositions in lherzolite as functions of pressure and temperature provides constraints on mantle dynamics and magma genesis. In this paper, we present a detailed evaluation of the use of natural mineral mixes as
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|Source:||Journal of Petrology|
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