Matches in SemOpenAlex for { <https://semopenalex.org/work/W2054703344> ?p ?o ?g. }
- W2054703344 abstract "Nemrut volcano, adjacent to Lake Van (Turkey), is one of the most important peralkaline silicic centres in the world, where magmatism for ~570,000 years has been dominated by peralkaline trachytes and rhyolites. Using onshore and Lake Van drill site tephra samples, we document the phenocryst and glass matrix compositions, confirming a complete spectrum from very rare mafic to dominantly silicic magmas. Magma mixing has been common and, along with the multi-lineage nature of the magmas, indicates that Nemrut has been a very open system where, nevertheless, compositionally zoned caps developed during periods of relative eruptive quiescence. Geothermometry suggests that the intermediate-silicic magmas evolved in an upper crustal magma reservoir at temperatures between 1100 and 750 °C, at fO2 close to the FMQ buffer. The silicic magmas either were halogen poor or exsolved a halogen-rich phase prior to or during eruption. An unusual Pb-rich phase, with up to 98.78 wt% PbO, is interpreted as having exsolved from the intermediate-rhyolitic magmas." @default.
- W2054703344 created "2016-06-24" @default.
- W2054703344 creator A5012647261 @default.
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- W2054703344 date "2015-03-24" @default.
- W2054703344 modified "2023-10-14" @default.
- W2054703344 title "Peralkaline felsic magmatism at the Nemrut volcano, Turkey: impact of volcanism on the evolution of Lake Van (Anatolia) IV" @default.
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- W2054703344 doi "https://doi.org/10.1007/s00410-015-1127-6" @default.
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