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The fractionation progress of a crystallizing basaltic magma is recorded in the changing mineral compositions of binary solutions that form a part of plagioclase, olivine, and augite. When such compositional data are plotted against an independent measure of progress such as volume, they can often be described by a Rayleigh equation that reveals details of the crystallization history. A binary sol...

The Internal Magma Reservoir of Large Intrusions Revealed by Multiphase Rayleigh Fractionation