The Short-Range Order (SRO) and Structure

Abstract

Research Article| May 01, 2022 The Short-Range Order (SRO) and Structure Grant S. Henderson; Grant S. Henderson Department of Earth Sciences, University of Toronto, 22 Russell St, Toronto, Ontario, M5S 3B1, Canada henders@es.utoronto.ca Search for other works by this author on: GSW Google Scholar Jonathan F. Stebbins Jonathan F. Stebbins Department of Geological Sciences, Stanford University, Stanford, California 94305–2115, USA stebbins@stanford.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Grant S. Henderson Department of Earth Sciences, University of Toronto, 22 Russell St, Toronto, Ontario, M5S 3B1, Canada Jonathan F. Stebbins Department of Geological Sciences, Stanford University, Stanford, California 94305–2115, USA henders@es.utoronto.ca stebbins@stanford.edu 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): 1–53. https://doi.org/10.2138/rmg.2022.87.01 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 Grant S. Henderson, Jonathan F. Stebbins; The Short-Range Order (SRO) and Structure. Reviews in Mineralogy and Geochemistry 2022;; 87 (1): 1–53. doi: https://doi.org/10.2138/rmg.2022.87.01 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 Magmas are mixtures of melt, crystals and dissolved gasses with or without crystalline material (Mysen and Richet 2019). They play an important role in igneous processes particularly those influenced by their viscosity, density, and other physical properties. Much of the research to date has used quenched melts (or glasses) as proxies for studying the melt portion of magmas. Studies of glasses and melts at elevated temperatures or in-situ have been carried out since the late 1970s (cf., Waseda and Egami 1979; Exarhos et al. 1988) but remain difficult experiments to perform due to technical difficulties dealing... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.