A sagging-spreading continuum of large volcano structure
2013; Geological Society of America; Volume: 41; Issue: 3 Linguagem: Inglês
10.1130/g33990.1
ISSN1943-2682
AutoresP. K. Byrne, Eoghan P. Holohan, Matthieu Kervyn, Benjamín van Wyk de Vries, Valentín R. Troll, John B. Murray,
Tópico(s)earthquake and tectonic studies
ResumoResearch Article| March 01, 2013 A sagging-spreading continuum of large volcano structure P.K. Byrne; P.K. Byrne 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road NW, Washington, D.C. 20015, USA4Laboratoire Magmas et Volcans, Université Blaise-Pascal, 5 Rue Kessler, 63038 Clermont-Ferrand Cedex, France Search for other works by this author on: GSW Google Scholar E.P. Holohan; E.P. Holohan 2School of Geological Sciences, University College Dublin, Belfield, Dublin 4, Ireland Search for other works by this author on: GSW Google Scholar M. Kervyn; M. Kervyn 3Department of Geography, Vrije Universiteit Brussels, Pleinlaan 2 050 Brussels, Belgium Search for other works by this author on: GSW Google Scholar B. van Wyk de Vries; B. van Wyk de Vries 4Laboratoire Magmas et Volcans, Université Blaise-Pascal, 5 Rue Kessler, 63038 Clermont-Ferrand Cedex, France Search for other works by this author on: GSW Google Scholar V.R. Troll; V.R. Troll 5Department of Earth Sciences, Uppsala University, Villavägen 16 B, 751 05 Uppsala, Sweden Search for other works by this author on: GSW Google Scholar J.B. Murray J.B. Murray 6Department of Earth and Environmental Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK Search for other works by this author on: GSW Google Scholar Author and Article Information P.K. Byrne 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road NW, Washington, D.C. 20015, USA4Laboratoire Magmas et Volcans, Université Blaise-Pascal, 5 Rue Kessler, 63038 Clermont-Ferrand Cedex, France E.P. Holohan 2School of Geological Sciences, University College Dublin, Belfield, Dublin 4, Ireland M. Kervyn 3Department of Geography, Vrije Universiteit Brussels, Pleinlaan 2 050 Brussels, Belgium B. van Wyk de Vries 4Laboratoire Magmas et Volcans, Université Blaise-Pascal, 5 Rue Kessler, 63038 Clermont-Ferrand Cedex, France V.R. Troll 5Department of Earth Sciences, Uppsala University, Villavägen 16 B, 751 05 Uppsala, Sweden J.B. Murray 6Department of Earth and Environmental Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK Publisher: Geological Society of America Received: 28 Aug 2012 Revision Received: 21 Sep 2012 Accepted: 25 Sep 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (3): 339–342. https://doi.org/10.1130/G33990.1 Article history Received: 28 Aug 2012 Revision Received: 21 Sep 2012 Accepted: 25 Sep 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation P.K. Byrne, E.P. Holohan, M. Kervyn, B. van Wyk de Vries, V.R. Troll, J.B. Murray; A sagging-spreading continuum of large volcano structure. Geology 2013;; 41 (3): 339–342. doi: https://doi.org/10.1130/G33990.1 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 Gravitational deformation strongly influences the structure and eruptive behavior of large volcanoes. Using scaled analog models, we characterize a range of structural architectures produced by volcano sagging and volcano spreading. These arise from the interplay of variable basement rigidity and volcano-basement (de-)coupling. From comparison to volcanoes on Earth (La Réunion and Hawaii) and Mars (Elysium and Olympus Montes), the models highlight a structural continuum in which large volcanoes throughout the Solar System lie. 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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