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

Abstract

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 a

    Similar works

    Full text

    thumbnail-image