Hot Sintering of Melts, Glasses and Magmas
Fabian B. Wadsworth, Jérémie Vasseur, Edward W. Llewellin, Donald B. Dingwell
Abstract
Research Article| May 01, 2022 Hot Sintering of Melts, Glasses and Magmas Fabian B. Wadsworth; Fabian B. Wadsworth Department of Earth Sciences, Durham University, Durham, United Kingdom [email protected] Search for other works by this author on: GSW Google Scholar Jérémie Vasseur; Jérémie Vasseur Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, Germany [email protected] Search for other works by this author on: GSW Google Scholar Edward W. Llewellin; Edward W. Llewellin Department of Earth Sciences, Durham University, Durham, United Kingdom [email protected] Search for other works by this author on: GSW Google Scholar Donald B. Dingwell Donald B. Dingwell Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, Germany [email protected] Search for other works by this author on: GSW Google Scholar Author and Article Information Fabian B. Wadsworth Department of Earth Sciences, Durham University, Durham, United Kingdom Jérémie Vasseur Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, Germany Edward W. Llewellin Department of Earth Sciences, Durham University, Durham, United Kingdom Donald B. Dingwell Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, Germany [email protected] [email protected] [email protected] [email protected] Publisher: Mineralogical Society of America First Online: 01 May 2022 Copyright © 2022 by the Mineralogical Society of AmericaMineralogical Society of America Reviews in Mineralogy and Geochemistry (2022) 87 (1): 801–840. https://doi.org/10.2138/rmg.2022.87.17 Article history First Online: 01 May 2022 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Fabian B. Wadsworth, Jérémie Vasseur, Edward W. Llewellin, Donald B. Dingwell; Hot Sintering of Melts, Glasses and Magmas. Reviews in Mineralogy and Geochemistry 2022;; 87 (1): 801–840. doi: https://doi.org/10.2138/rmg.2022.87.17 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 SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Magma may fragment as it ascends through the volcanic plumbing system to the Earth surface, forming volcanic ash and pyroclasts (Scheu and Dingwell 2022, this issue). If the pyroclastic products of fragmentation are deposited hot, they can stick, coalesce, and weld together, re-amalgamating into coherent magma. Subaerial deposits include welded, lava-like, and rheomorphic ignimbrites (Branney et al. 1992; Andrews and Branney 2011), and welded fall deposits proximal to an eruptive vent (Houghton and Carey 2015). Welding occurs in the sub-surface at conduit margins (Gardner et al. 2017; Wadsworth et al. 2020... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.