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Chemical alteration of tephra in the depositional environment: theoretical stability modelling
74
Citations
15
References
2003
Year
Icelandic TephrasChemical KineticsEngineeringChemical DurabilityChemical AlterationChemistryEarth ScienceOrganic GeochemistryEnvironmental ChemistryChemical EngineeringEnvironmental GeochemistryMineral-fluid InteractionChemical StabilityTheoretical Stability ModellingDepositional EnvironmentBiogeochemistryComputational GeochemistryGeologyDepositional ProcessGeochemistryIgneous PetrologyPetrologyMineral Geochemistry
Abstract The study of the chemical stability of vitreous material in aqueous media is well‐established. There has to date been little consideration of the implications of variations in the chemical durability of tephra in Quaternary tephrochronology. Chemical alteration can take the form of cationic leaching from the matrix, or complete destruction of the silica network, either of which could constrain the ability to chemically identify distal tephra. Here we apply established models of vitreous durability to the published chemical analyses of a large number of Icelandic tephras in order to predict their relative durabilities under equivalent conditions. This suggests that some important tephras have relatively poor chemical stability, and that rhyolitic tephras are, in general, more stable than basaltic. We conclude that tephras should be expected to show predictable differential chemical stability in the post‐depositional environment. Copyright © 2003 John Wiley & Sons, Ltd.
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