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• W2037299081 abstract "Research Article| September 01, 2007 Late Holocene strike-slip offset of a subsurface channel interpreted from three-dimensional seismic data, eastern offshore Trinidad David M. Soto; David M. Soto 1Jackson School of Geosciences, University of Texas at Austin, J.J. Pickle Research Campus, Building 196 (R2200OC), 10100 Burnet Road, Austin, Texas 78758-4445, USA Search for other works by this author on: GSW Google Scholar Paul Mann; Paul Mann 1Jackson School of Geosciences, University of Texas at Austin, J.J. Pickle Research Campus, Building 196 (R2200OC), 10100 Burnet Road, Austin, Texas 78758-4445, USA Search for other works by this author on: GSW Google Scholar Alejandro Escalona; Alejandro Escalona 1Jackson School of Geosciences, University of Texas at Austin, J.J. Pickle Research Campus, Building 196 (R2200OC), 10100 Burnet Road, Austin, Texas 78758-4445, USA Search for other works by this author on: GSW Google Scholar Lesli J. Wood Lesli J. Wood 1Jackson School of Geosciences, University of Texas at Austin, J.J. Pickle Research Campus, Building 196 (R2200OC), 10100 Burnet Road, Austin, Texas 78758-4445, USA Search for other works by this author on: GSW Google Scholar Geology (2007) 35 (9): 859–862. https://doi.org/10.1130/G23738A.1 Article history received: 28 Feb 2007 rev-recd: 23 Apr 2007 accepted: 28 Apr 2007 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 David M. Soto, Paul Mann, Alejandro Escalona, Lesli J. Wood; Late Holocene strike-slip offset of a subsurface channel interpreted from three-dimensional seismic data, eastern offshore Trinidad. Geology 2007;; 35 (9): 859–862. doi: https://doi.org/10.1130/G23738A.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 A right-lateral strike-slip fault offset of a shallowly buried fluvial paleochannel is interpreted from three-dimensional (3-D) seismic data in the eastern offshore area of Trinidad. The fault represents the eastern offshore continuation of the main South America–Caribbean plate boundary zone in Trinidad, the Central Range fault zone. Previous global positioning system–based geodetic studies and trenching have shown that the 50-km-long on-land segment of the Central Range fault zone accommodates a significant part of the present-day interplate motion. The 3-D seismic data shown here reveal that the 60-km-long offshore continuation of the Central Range fault zone forms a prominent seafloor lineament and dextrally offsets a shallowly buried (83 m below sea level), late Quaternary fluvial channel by 322–506 m. Based on the eustatic sea-level curve, we infer that the channel began to be incised during the beginning of the Last Glacial Maximum ca. 30 ka and was subsequently offset by the Central Range fault zone. Using the offset amounts and our inferred age for the filled channel, we can estimate a long-term slip along the fault of 17–19 mm/yr for the Central Range fault zone. Because no documented earthquake has occurred on the Central Range since A.D. 1800, as much as 3.7 m of elastic strain may have accumulated on the Central Range fault zone that could be released by a future magnitude >M7.5 earthquake. 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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• W2037299081 date "2007-01-01" @default.
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• W2037299081 title "Late Holocene strike-slip offset of a subsurface channel interpreted from three-dimensional seismic data, eastern offshore Trinidad" @default.
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