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• W2015308941 abstract "Research Article| May 01, 1980 Fines-depleted ignimbrite in New Zealand — The product of a turbulent pyroclastic flow G.P.L. Walker; G.P.L. Walker 1Imperial College, London SW7, England Search for other works by this author on: GSW Google Scholar C.J.N. Wilson; C.J.N. Wilson 1Imperial College, London SW7, England Search for other works by this author on: GSW Google Scholar P. C. Froggatt P. C. Froggatt 2Geology Department, Victoria University of Wellington, Wellington, New Zealand Search for other works by this author on: GSW Google Scholar Geology (1980) 8 (5): 245–249. https://doi.org/10.1130/0091-7613(1980)8<245:FIINZT>2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation G.P.L. Walker, C.J.N. Wilson, P. C. Froggatt; Fines-depleted ignimbrite in New Zealand — The product of a turbulent pyroclastic flow. Geology 1980;; 8 (5): 245–249. doi: https://doi.org/10.1130/0091-7613(1980)8<245:FIINZT>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A new type of ignimbrite, a “fines-depleted ignimbrite,” is largely depleted in the finer constituents and is clast-supported for all clasts exceeding about 2 mm in size. Its formation is attributed to the loss of fine (mostly submillimetre-sized) vitric material from the pyroclastic flow, by an amount equal to about half of the original mass of the flow. This loss, the large size and high content of lithic clasts, and the thorough intermixing of carbonized vegetation are believed to indicate that the pyroclastic flow, at least in part, traveled turbulently. Turbulent flow was partly a consequence of a high flow velocity, for which there is independent evidence (the same flow climbed 1,500 m up a mountain 46 km from source), and was partly caused by the ingestion of forest and the resulting high throughput of gas in the flow head. The implication is that normal ignimbrite is generated by laminar flow, whereas turbulent flows generate the significantly different, fines-depleted variant. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2015308941 title "Fines-depleted ignimbrite in New Zealand — The product of a turbulent pyroclastic flow" @default.
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