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• W2074821141 abstract "Research Article| April 01, 2005 Active faulting within the offshore western Gulf of Corinth, Greece: Implications for models of continental rift deformation L.C. McNeill; L.C. McNeill 1Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar C.J. Cotterill; C.J. Cotterill 1Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar T.J. Henstock; T.J. Henstock 1Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar J.M. Bull; J.M. Bull 1Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar A. Stefatos; A. Stefatos 2Laboratory of Marine Geology and Physical Oceanography, University of Patras, Patras 26500, Greece Search for other works by this author on: GSW Google Scholar R.E.Ll. Collier; R.E.Ll. Collier 3School of Earth Sciences, University of Leeds, Leeds LS2 9JT, UK Search for other works by this author on: GSW Google Scholar G. Papatheoderou; G. Papatheoderou 4Laboratory of Marine Geology and Physical Oceanography, University of Patras, Patras 26500, Greece Search for other works by this author on: GSW Google Scholar G. Ferentinos; G. Ferentinos 4Laboratory of Marine Geology and Physical Oceanography, University of Patras, Patras 26500, Greece Search for other works by this author on: GSW Google Scholar S.E. Hicks S.E. Hicks 5Southampton Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Search for other works by this author on: GSW Google Scholar Geology (2005) 33 (4): 241–244. https://doi.org/10.1130/G21127.1 Article history received: 14 Sep 2004 rev-recd: 06 Dec 2004 accepted: 07 Dec 2004 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation L.C. McNeill, C.J. Cotterill, T.J. Henstock, J.M. Bull, A. Stefatos, R.E.Ll. Collier, G. Papatheoderou, G. Ferentinos, S.E. Hicks; Active faulting within the offshore western Gulf of Corinth, Greece: Implications for models of continental rift deformation. Geology 2005;; 33 (4): 241–244. doi: https://doi.org/10.1130/G21127.1 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 Discrimination between different lithospheric extension models focusing on the roles of low-angle vs. high-angle faulting, and how strain is distributed, requires high-fidelity imaging of brittle deformation. High-resolution seismic reflection and multibeam bathymetric data in the western Gulf of Corinth continental rift were collected to establish the contribution of offshore faults to extension. Onshore fault slip here is significantly less than expected from geodetic strain rates. The rift at this location is a half-graben tilted to the north by S-dipping faults within the uppermost crust. A basement horst on the northern margin is uplifted by the North and South Eratini faults, and the axial channel is fault controlled. Subsided lowstand shorelines in the hanging wall of the North Eratini and the well-studied Aigion fault suggest that the faults have similar displacements. Summed extension from the four major faults across this part of the rift (Eliki, Subchannel, South Eratini, North Eratini) is ∼8–16 mm/yr, thereby reconciling geologic and geodetic data sets. Distributed deformation across isolated multiple faults can model this part of the rift without recourse to, and potentially incompatible with, an underlying low-angle detachment. 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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• W2074821141 title "Active faulting within the offshore western Gulf of Corinth, Greece: Implications for models of continental rift deformation" @default.
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