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- W2012116458 abstract "Research Article| October 01, 2012 Upper plate tectonic stress state may influence interseismic coupling on subduction megathrusts Laura M. Wallace; Laura M. Wallace 1GNS Science, 1 Fairway Drive, Lower Hutt, New Zealand *Current address: University of Texas Institute for Geophysics, 10100 Burnet Road (R2200), Austin, Texas 78758, USA. Search for other works by this author on: GSW Google Scholar Åke Fagereng; Åke Fagereng 2Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa Search for other works by this author on: GSW Google Scholar Susan Ellis Susan Ellis 1GNS Science, 1 Fairway Drive, Lower Hutt, New Zealand Search for other works by this author on: GSW Google Scholar Author and Article Information Laura M. Wallace *Current address: University of Texas Institute for Geophysics, 10100 Burnet Road (R2200), Austin, Texas 78758, USA. 1GNS Science, 1 Fairway Drive, Lower Hutt, New Zealand Åke Fagereng 2Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa Susan Ellis 1GNS Science, 1 Fairway Drive, Lower Hutt, New Zealand Publisher: Geological Society of America Received: 04 Mar 2012 Accepted: 12 Apr 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2012) 40 (10): 895–898. https://doi.org/10.1130/G33373.1 Article history Received: 04 Mar 2012 Accepted: 12 Apr 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Laura M. Wallace, Åke Fagereng, Susan Ellis; Upper plate tectonic stress state may influence interseismic coupling on subduction megathrusts. Geology 2012;; 40 (10): 895–898. doi: https://doi.org/10.1130/G33373.1 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 We document a correlation between along-strike variation in interseismic coupling depth on subduction interfaces, and the upper plate tectonic stress state in New Zealand, Vanuatu, and southwest Japan. Deep interseismic coupling occurs where the upper plate stress regime is contractional to transpressional, whereas a shallowing of interseismic coupling occurs where there is an along-strike shift to back-arc or intra-arc extension. To explain this relationship, we draw on theoretical studies suggesting that the fluid pressure state within the upper plate and on the subduction interface has a strong control on the depth of the transition from frictional to viscous behavior. Lower fluid pressures (e.g., close to hydrostatic) are expected where the over-riding plate is undergoing tectonic extension, whereas higher fluid pressures (e.g., close to lithostatic) are expected where the over-riding plate experiences long-term (e.g., >105 yr) tectonic shortening. Low fluid pressures within the upper plate may lead to a shallow frictional to viscous transition compared to an upper plate that is highly overpressured. We hypothesize that the state of tectonic stress and structural permeability in the upper plate are yet other variables to consider when evaluating which physical mechanisms control interseismic coupling of subduction megathrusts. 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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- W2012116458 title "Upper plate tectonic stress state may influence interseismic coupling on subduction megathrusts" @default.
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