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• W2085596829 abstract "Research Article| July 01, 2005 Erosion-controlled geometry of buckle fold interference José L. Simón José L. Simón 1Departamento de Geología, Universidad de Zaragoza, 50009 Zaragoza, Spain Search for other works by this author on: GSW Google Scholar Author and Article Information José L. Simón 1Departamento de Geología, Universidad de Zaragoza, 50009 Zaragoza, Spain Publisher: Geological Society of America Received: 19 Jan 2005 Revision Received: 30 Mar 2005 Accepted: 31 Mar 2005 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2005) 33 (7): 561–564. https://doi.org/10.1130/G21468.1 Article history Received: 19 Jan 2005 Revision Received: 30 Mar 2005 Accepted: 31 Mar 2005 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation José L. Simón; Erosion-controlled geometry of buckle fold interference. Geology 2005;; 33 (7): 561–564. doi: https://doi.org/10.1130/G21468.1 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 Refolding structures in the Aliaga area (Iberian Chain, Spain) show how erosion can exert a control on the geometry of buckle fold interference. Early Miocene ENE-trending buckle folds are superposed on a large NNW-SSE anticline (Eocene–Oligocene). North of Aliaga, the earlier hinge zone in the competent limestone unit controlling buckling (Urgon facies, Lower Cretaceous) constitutes a mechanical obstacle to refolding, which induces development of essentially conical type 2 interference. To the south, erosional removal of the hinge zone at that competent unit allowed the near-vertical eastern limb to behave as independent layers, being refolded into cylindrical, near-vertical-axis folds showing a snake-like map pattern. Lower Miocene conglomerates containing pebbles of Jurassic origin, whose source area was the core of the earlier NNW-SSE–trending anticline, indicate that this Jurassic core had been effectively exhumed before refolding occurred. In this way, snake-like folds constitute a new case of erosion-controlled tectonic structure. 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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• W2085596829 title "Erosion-controlled geometry of buckle fold interference" @default.
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