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• W2019870909 abstract "Research Article| July 01, 2007 Development of en echelon magmatic segments along oblique spreading ridges J.W. van Wijk; J.W. van Wijk 1Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA Search for other works by this author on: GSW Google Scholar D.K. Blackman D.K. Blackman 1Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA Search for other works by this author on: GSW Google Scholar Author and Article Information J.W. van Wijk 1Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA D.K. Blackman 1Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA Publisher: Geological Society of America Received: 23 Aug 2006 Revision Received: 16 Feb 2007 Accepted: 25 Feb 2007 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2007) 35 (7): 599–602. https://doi.org/10.1130/G23294A.1 Article history Received: 23 Aug 2006 Revision Received: 16 Feb 2007 Accepted: 25 Feb 2007 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation J.W. van Wijk, D.K. Blackman; Development of en echelon magmatic segments along oblique spreading ridges. Geology 2007;; 35 (7): 599–602. doi: https://doi.org/10.1130/G23294A.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 En echelon magmatic segments commonly develop along obliquely spreading oceanic ridges. To clarify some of the dynamic aspects of this plate boundary, we performed a series of thermo-mechanical numerical tests. When extension of oceanic lithosphere becomes oblique, deformation within the axial region localizes into distinct upwelling centers. Temperatures are elevated in the upwelling cells, which are shallow mantle features that form the new plate boundary. The predicted features are similar to the axial volcanic ridges documented at Mohns and Reykjanes Ridges, and we conclude that they become the new loci of extensional deforma tion, upwelling, and magmatic activity. These ridges, suborthogonal to the plate spreading direction, only develop when the axis rift zone is weak. The subsegment length and spacing depend primarily on obliquity and axial width. Predicted crustal thickness along the subsegmented axis varies discernibly; this might explain the morphology and satellite gravity of the flanks of oblique spreading ridges. 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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• W2019870909 title "Development of en echelon magmatic segments along oblique spreading ridges" @default.
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