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• W2054116178 abstract "Research Article| March 01, 2009 Deconvolving tectono-climatic signals in deep-marine siliciclastics, Eocene Ainsa basin, Spanish Pyrenees: Seesaw tectonics versus eustasy Kevin T. Pickering; Kevin T. Pickering 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK Search for other works by this author on: GSW Google Scholar Nicole J. Bayliss Nicole J. Bayliss 1Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK Search for other works by this author on: GSW Google Scholar Geology (2009) 37 (3): 203–206. https://doi.org/10.1130/G25261A.1 Article history received: 08 Jul 2008 rev-recd: 20 Oct 2008 accepted: 21 Oct 2008 first online: 02 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 Kevin T. Pickering, Nicole J. Bayliss; Deconvolving tectono-climatic signals in deep-marine siliciclastics, Eocene Ainsa basin, Spanish Pyrenees: Seesaw tectonics versus eustasy. Geology 2009;; 37 (3): 203–206. doi: https://doi.org/10.1130/G25261A.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 The Eocene deep-marine siliciclastic fill of the Ainsa basin, Spanish Pyrenees, gives unprecedented temporal resolution of the causes and timing of coarse clastic sediment supply to a deep-marine basin. Early Eocene tectonic subsidence linked to Pyrenean orogenesis created the Ainsa basin, with water depths of ~400–800 m above a foundered shallow-marine mixed carbonate and clastic shelf. The ~25 sandbodies or channelized submarine fans in the basin were controlled by the ~400 k.y. Milankovitch frequency, with modes at ~100 k.y. and ~41 k.y. (possibly stacked ~23 k.y.) influencing bottom-water conditions in the basin, causing periodic stratification in the water column across a submarine sill at the western basin margin (early Boltaña anticline). Intrabasinal tectonics defined and controlled the position of eight sandy systems and their constituent fans, in a process of seesaw tectonics, by (1) westward lateral offset stacking of sandy fans due to growth of the eastern side of the basin, represented today by the Mediano anticline, and (2) eastward (orogenward) back stepping of the depositional axis of each sandy system, due to phases of relative uplift of the Boltaña anticline. During basin infill, uplift of the Boltaña anticline led to increasing basin narrowing and depositional confinement. Unlike the earlier depositional systems, the youngest deep-marine system was fed from a more southern sediment source between the growth anticlines, as was the overlying deltaic system. All the older deep-marine sandy systems were fed from southeast point sources, from canyons and erosional lower-slope channels eroding the growing Mediano anticline. The depositional style outlined in this paper might be common to other active margins where siliciclastic basins evolve between active thrusts. 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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• W2054116178 title "Deconvolving tectono-climatic signals in deep-marine siliciclastics, Eocene Ainsa basin, Spanish Pyrenees: Seesaw tectonics versus eustasy" @default.
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