The rate of sedimentation from turbulent suspension: An experimental model with application to pyroclastic density currents and discussion on the grain-size dependence of flow runout-Reference-Cited by-同舟云学术

The rate of sedimentation from turbulent suspension: An experimental model with application to pyroclastic density currents and discussion on the grain-size dependence of flow runout

Published:2018-07-02 Issue:1 Volume:66 Page:129-145
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Dellino Pierfrancesco¹^ORCID,Dioguardi Fabio²,Doronzo Domenico M.³,Mele Daniela⁴

Affiliation:

1. Dipartimento di Scienze della Terra e Geoambientali; Università di Bari; via Orabona 4 70125 Bari Italy

2. British Geological Survey; The Lyell Centre, Research Avenue South; Edinburgh EH14 4AP UK

3. Institute of Earth Sciences “Jaume Almera”; ICTJA, CSIC, Group of Volcanology; SIMGEO UB-CSIC; Lluis Sole i Sabaris s/n Barcelona 08028 Spain

4. Sezione di Napoli Osservatorio Vesuviano - Istituto Nazionale di Geofisica e Vulcanologia; via Diocleziano 328 Naples 80124 Italy

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12485/fullpdf

Reference41 articles.

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2. Experimental study of turbulence, sedimentation, and coignimbrite mass partitioning in dilute pyroclastic density currents;Andrews;J. Volcanol. Geotherm. Res.,2012

3. The impact of pyroclastic surges on buildings at the eruption of the Soufrière Hills volcano, Montserrat;Baxter;Bull. Volcanol.,2005

4. Internal flow variations and diachronous sedimentation within extensive, sustained, density stratified pyroclastic density currents down gentle slopes, as revealed by the internal architectures of ignimbrites in Tewnerife;Brown;Bull. Volcanol.,2013

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