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- W2547588655 abstract "Abstract Chlorite, ordered mixed-layer chlorite-smectites, laumontite, quartz and albite are the most widespread alteration assemblage in cone-building and near-vent successions of lavas, autoclastic, pyroclastic and resedimented volcaniclastic deposits of the Oligocene Smrekovec Volcanic Complex, Slovenia. Randomly interstratified corrensite-chlorite with ~ 70–80% of corrensite layers (R0 Cr-Ch) is less common in occurrence and associated either with clinoptilolite and heulandite in fine-grained vitric tuffs, or with prehnite, laumontite, actinolite, analcime and albite in extensively altered and/or fractured host-rocks. The assemblage with clinoptilolite and heulandite indicates the temperatures of formation of" @default.
- W2547588655 created "2016-11-11" @default.
- W2547588655 creator A5085204147 @default.
- W2547588655 date "2016-12-01" @default.
- W2547588655 modified "2023-10-17" @default.
- W2547588655 title "Hydrothermal alteration of chlorite to randomly interstratified corrensite-chlorite: Geological evidence from the Oligocene Smrekovec Volcanic Complex, Slovenia" @default.
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- W2547588655 doi "https://doi.org/10.1016/j.clay.2016.10.025" @default.
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