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- W2090837808 abstract "Synopsis Mixed pyroclastic rock accumulations in the Eastern Red Hills district of the Tertiary igneous centre of Skye show a wide range in composition and mode of formation. Prior to this investigation these volcanic products were interpreted as vent infillings. It is shown that this model is unrealistic, as detailed mapping demonstrates that they are bedded, subaerial and subaqueous deposits. Chaotic, polylithic agglomerates, at least 300 m thick, are preserved in a ring-faulted mass in the Kilchrist area and are intercalated with thin acid tuffs, basic tuffs (grading towards coarser material) and ignimbrites. A hyaloclastite horizon is also present within the sequence. It is concluded that these accumulations of pyroclastic rocks do not show close genetic links with the later, spatially-associated granites of the Eastern Red Hills Centre, but may have originated by explosive volcanism triggered off by earlier events in the Skye Centre. Later subaerial and subaqueous processes greatly modified their primary appearance. Intercalated with the pyroclastic rocks are rhyolite lavas which are associated with the subvolcanic granites of the district. These lavas provide evidence of the close connection between surface volcanism and subvolcanic activity in the Skye Centre." @default.
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- W2090837808 date "1985-04-01" @default.
- W2090837808 modified "2023-09-27" @default.
- W2090837808 title "The pyroclastic rocks and rhyolitic lavas of the Eastern Red Hills district, Isle of Skye" @default.
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- W2090837808 doi "https://doi.org/10.1144/sjg21010057" @default.
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