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Research Article| May 01, 2022 Magma / Suspension Rheology Stephan Kolzenburg; Stephan Kolzenburg Department of Geology University at Buffalo 126 Cooke Hall Buffalo, NY 14260-4130, USADepartment of Earth and Environmental Sciences Ludwig-Maximilians-University Munich Theresienstr. 41 / III 80333, Munich, GermanyDepartment of Earth and Planetary Sciences McGill University 3450 University Street Montreal, H3A 0E8, Quebec, Canada stephank@buffalo.edu Search for other works by this author on: GSW Google Scholar Magdalena O. Chevrel; Magdalena O. Chevrel Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS, IRD, OPGC, 6 Avenue Blaise Pascal f-63000, Clermont-Ferrand, France oryaelle.chevrel@ird.fr 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-University Munich Theresienstr. 41 / III 80333, Munich, Germany dingwell@lmu.de Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2022) 87 (1): 639–720. https://doi.org/10.2138/rmg.2022.87.14 Article history first online: 01 May 2022 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Stephan Kolzenburg, Magdalena O. Chevrel, Donald B. Dingwell; Magma / Suspension Rheology. Reviews in Mineralogy and Geochemistry 2022;; 87 (1): 639–720. doi: https://doi.org/10.2138/rmg.2022.87.14 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 When considering the rheology of a suspension the fundamental physical aspect to be quantified is the redistribution of strain between the deformable matrix fraction of the physical mixture and the suspended phase or phases. For the case of solid particle suspensions in magma and lava the suspended crystalline phases will generally be devoid of significant internal strain during flow. With some exceptions (Cordonnier et al. 2009; Kendrick et al. 2017), the stresses driving the magmatic deformation and flow, are generally not high enough to induce significant crystal deformation (see however below). Thus, the primary task becomes one... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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