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- W2096397784 abstract "Garnets in continentally derived high-pressure (HP) rocks of the Sesia Zone (Western Alps) exhibit three different chemical zonation patterns, depending on sample locality. Comparison of observed garnet zonation patterns with thermodynamically modelled patterns shows that the different patterns are caused by differences in the water content of the subducted protoliths during prograde metamorphism. Zonation patterns of garnets in water-saturated host rocks show typical prograde chemical zonations with steadily increasing pyrope content and increasing XMg, together with bell-shaped spessartine patterns. In contrast, garnets in water-undersaturated rocks have more complex zonation patterns with a characteristic decrease in pyrope and XMg between core and inner rim. In some cases, garnets show an abrupt compositional change in core-to-rim profiles, possibly due to water-undersaturation prior to HP metamorphism. Garnets from both water-saturated and water-undersaturated rocks show signs of intervening growth interruptions and core resorption. This growth interruption results from bulk-rock depletion caused by fractional garnet crystallization." @default.
- W2096397784 created "2016-06-24" @default.
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- W2096397784 creator A5039063088 @default.
- W2096397784 creator A5080041527 @default.
- W2096397784 date "2006-08-24" @default.
- W2096397784 modified "2023-09-29" @default.
- W2096397784 title "The Physico-Chemical Properties of a Subducted Slab from Garnet Zonation Patterns (Sesia Zone, Western Alps)" @default.
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- W2096397784 doi "https://doi.org/10.1093/petrology/egl039" @default.
- W2096397784 hasPublicationYear "2006" @default.
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