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• W2013907048 abstract "Research Article| May 01, 1992 The genesis, ascent, and emplacement of the Northern Arran Granite, Scotland: Implications for granitic diapirism RICHARD W. ENGLAND RICHARD W. ENGLAND 1Department of Geological Sciences, University of Durham, Durham, DH1 3LE, United Kingdom Search for other works by this author on: GSW Google Scholar GSA Bulletin (1992) 104 (5): 606–614. https://doi.org/10.1130/0016-7606(1992)104<0606:TGAAEO>2.3.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation RICHARD W. ENGLAND; The genesis, ascent, and emplacement of the Northern Arran Granite, Scotland: Implications for granitic diapirism. GSA Bulletin 1992;; 104 (5): 606–614. doi: https://doi.org/10.1130/0016-7606(1992)104<0606:TGAAEO>2.3.CO;2 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 SocietyGSA Bulletin Search Advanced Search Abstract Integrated structural and petrological data are used to trace the evolution of the Northern Arran Coarse Granite during the latter stages of its ascent and its emplacement. Structural analysis of the aureole of the granite suggests that it rose as a single body of magma, which is confirmed by petrological data. During its ascent, the pluton intersected the downward-dipping limb of an existing synform, refolding and displacing it upward to form a concentric or rim synform. This direct evidence of vertical displacement of the country rocks confirms that the pluton is a diapir. Diapiric ascent was permitted by a reduction in wall-rock viscosity and hence viscous drag forces on the pluton, aided by heat loss due to crystallization during ascent. Most of the deformation within the aureole can be attributed to ascent of the pluton. The early rim synform is overprinted by flattening strains and faulting caused by in situ radial expansion, which represents the ultimate evolution of a diapiric body. The final shape of the pluton is determined by inhomogeneous deformation of the aureole, which is partly controlled by pre-existing faults. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2013907048 title "The genesis, ascent, and emplacement of the Northern Arran Granite, Scotland: Implications for granitic diapirism" @default.
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