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- W2479365655 abstract "New experiments on the assemblages liquid-forsterite-anorthite-spinel (liq-fo-an-sp) and liq-fo-an have been performed at one atmosphere in the system CaO-MgO-Al 2 O 3 -SiO 2 (CMAS), in order to shed more light on the evolution of high-Mg to high-Al magmas, which often undergo olivine and/or plagioclase and/or spinel crystallisation during early stages of low-pressure differentiation. In CMAS, the prior crystallisation of fo, an, sp, fo + sp or an + sp forces high-Mg to high-Al compositions to converge toward intermediate Mg- and Al-rich magmas with constant MgO/(MgO + Al 2 O 3 ) ratio (≃ 2/3 in mole). This first step also increases the CaO/Al 2 O 3 ratio of liquids to produce Al-rich basalts in equilibrium with fo-an-sp" @default.
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- W2479365655 date "1994-09-28" @default.
- W2479365655 modified "2023-10-16" @default.
- W2479365655 title "Liquid-forsterite-anorthite-spinel assemblage at 1 bar in the CMAS system: implications for low-pressure evolution of high-Al and high-Mg magmas" @default.
- W2479365655 doi "https://doi.org/10.1127/ejm/6/5/0633" @default.
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