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- W2150484429 abstract "Anatectic crustal xenoliths in the Miocene volcanic rocks of Mazarron (southeast Spain) contain andalusite with melt inclu- sions, an unprecedented finding. Microstructures indicate that the melt inclusions were trapped during andalusite growth. The vola- tile content of the peraluminous inclusions is too low (Cl , 0.4 wt%, F , 0.3 wt%, P 1500 ppm, B , 850 ppm) to have caused a significant reduction of the wet solidus temperature. Moreover, the presence of graphite, as observed, during partial melting is expected to have raised the temperature of the wet solidus. Melting temperatures for the inclusions—obtained from quartz-albite-or- thoclase haplogranite system (680-790 8C), Zr (620-705 8C), and light rare earth element (615-725 8C) thermometry—indicate that the stability of andalusite 1 melt is incompatible with the position of the most commonly used andalusite 5 sillimanite equilibrium, and that the Al2SiO5 triple point must be placed at higher tem- peratures and pressures." @default.
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- W2150484429 date "2003-01-01" @default.
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- W2150484429 title "Primary melt inclusions in andalusite from anatectic graphitic metapelites: Implications for the position of the Al2SiO5 triple point" @default.
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- W2150484429 doi "https://doi.org/10.1130/0091-7613(2003)031<0573:pmiiaf>2.0.co;2" @default.
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