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• W2006439083 abstract "The authigenic marine zeolites, clinoptilolite and phillipsite, form from the low P–T alteration of volcanic glass shards, and the dominant factor controlling zeolite type is the SiAl ratio of the parent glass. The low-silica zeolite, phillipsite, is formed by the rapid breakdown of basic, alkaline glasses (low SiAl ratios) and is therefore abundant in young ocean sediments, whereas the high-silica zeolite, clinoptilolite, is formed by the slow breakdown of acidic glasses (high SiAl ratios) and is therefore more abundant in older sediments. Most volcanic debris originates from subaerial sources and there is a close correlation between the spatial and temporal distribution patterns of clinoptilolite and phillipsite and those of subaerial acidic and basic volcanicity. Although there are correlations between zeolite species and both sedimentation rates and sediment lithologies, these are considered to be largely coincidental. However, the dissolution of siliceous organisms in sediments may result in local silica enrichments in seawater which will increase SiAl ratios and so promote the formation of clinoptilolite." @default.
• W2006439083 created "2016-06-24" @default.
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• W2006439083 date "1979-01-01" @default.
• W2006439083 modified "2023-09-25" @default.
• W2006439083 title "Authigenic marine zeolites and their relationship to global volcanism" @default.
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• W2006439083 doi "https://doi.org/10.1016/0025-3227(79)90112-9" @default.
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