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The Gold Flat Tuff, Nevada: Insights into the evolution of peralkaline silicic magmas

cris.lastimport.scopus2024-02-12T20:12:12Z
dc.abstract.enThe Gold Flat Tuff is the youngest (9.15 Ma) ash-flow sheet erupted from the Black Mountain Volcanic Centre, southwest Nevada, USA. This paper explores some aspects of the very complex nature of the tuff's magmatic plumbing system. The main body of the deposit is a mixed magma product, comprising pantelleritic and comenditic melts derived from independently evolving reservoirs, and antecrysts and enclaves derived from a range of basic to intermediate sources. Metre-scale cognate xenoliths point to the presence of alkali feldspar accumulation zones. The pantellerite contains phenocrysts of fluorite and chevkinite-(Ce). The inferred intermediate magma component contains perrierite-(Ce) phenocrysts. The pantellerite has unusually high contents of F (≤2.2 wt%), F + Cl (≤2.9 wt%) and ZrO2 (≤1.04 wt%). The high halogen contents may have influenced the evolution of the strongly peralkaline magma. The crystallization conditions are poorly constrained but those for the pantelleritic magma may have been close to water-saturation (N4 wt% melt water) at temperatures ~740 °C and fO2 around FMQ.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorMacdonald, R.
dc.contributor.authorBagiński, Bogusław
dc.contributor.authorBelkin, H.E.
dc.contributor.authorWhite, J.C.
dc.contributor.authorNoble, D.C.
dc.date.accessioned2024-01-26T10:15:33Z
dc.date.available2024-01-26T10:15:33Z
dc.date.issued2019
dc.description.financeNie dotyczy
dc.description.volume328-329
dc.identifier.doi10.1016/J.LITHOS.2019.01.017
dc.identifier.issn0024-4937
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/122377
dc.identifier.weblinkhttps://doi.org/10.1016/j.lithos.2019.01.017
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofLithos
dc.relation.pages1-13
dc.rightsClosedAccess
dc.sciencecloudnosend
dc.subject.enGold Flat Tuff
dc.subject.enNevada
dc.subject.enPeralkaline rhyolites
dc.subject.enMagma mixing
dc.subject.enFluorite and Chevkinite-(Ce) phenocrysts
dc.titleThe Gold Flat Tuff, Nevada: Insights into the evolution of peralkaline silicic magmas
dc.typeJournalArticle
dspace.entity.typePublication