FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2051324656> ?p ?o ?g. }

• W2051324656 endingPage "751" @default.
• W2051324656 startingPage "729" @default.
• W2051324656 abstract "Research Article| May 01, 2009 Emplacement of the Cuera and Picos de Europa imbricate system at the core of the Iberian-Armorican arc (Cantabrian zone, north Spain): New precisions concerning the timing of arc closure Oscar A. Merino-Tomé; Oscar A. Merino-Tomé † 1Instituto Geológico y Minero de España, Parque Científico de León, Avda. Real 1, Edificio 1, 24006 León, Spain †E-mail: o.merino@igme.es. Search for other works by this author on: GSW Google Scholar Juan R. Bahamonde; Juan R. Bahamonde 2Departamento de Geología, Universidad de Oviedo, 33005 Oviedo, Spain Search for other works by this author on: GSW Google Scholar Juan R. Colmenero; Juan R. Colmenero 3Departamento de Geología, Universidad de Salamanca, 37008 Salamanca, Spain Search for other works by this author on: GSW Google Scholar Nemesio Heredia; Nemesio Heredia 4Instituto Geológico y Minero de España, 33005 Oviedo, Spain Search for other works by this author on: GSW Google Scholar Elisa Villa; Elisa Villa 2Departamento de Geología, Universidad de Oviedo, 33005 Oviedo, Spain Search for other works by this author on: GSW Google Scholar Pedro Farias Pedro Farias 2Departamento de Geología, Universidad de Oviedo, 33005 Oviedo, Spain Search for other works by this author on: GSW Google Scholar GSA Bulletin (2009) 121 (5-6): 729–751. https://doi.org/10.1130/B26366.1 Article history received: 13 Nov 2007 rev-recd: 04 Jun 2008 accepted: 04 Jun 2008 first online: 03 Oct 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Oscar A. Merino-Tomé, Juan R. Bahamonde, Juan R. Colmenero, Nemesio Heredia, Elisa Villa, Pedro Farias; Emplacement of the Cuera and Picos de Europa imbricate system at the core of the Iberian-Armorican arc (Cantabrian zone, north Spain): New precisions concerning the timing of arc closure. GSA Bulletin 2009;; 121 (5-6): 729–751. doi: https://doi.org/10.1130/B26366.1 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 SocietyGSA Bulletin Search Advanced Search Abstract The final stages of the Variscan orogeny (mostly Carboniferous) in the Western European Variscan belt involved the development of the Iberian-Armorican arc, which is cored by the Cantabrian zone (NW Iberia). The Cantabrian zone is the foreland of the Western European Variscan belt, and it is interpreted to record the waning stages of the closure of the Rheic Ocean. The distalmost tectonic units within the Cantabrian zone (the Cuera Unit and the Picos de Europa Province) were the last tectonic units emplaced at the core of the Western European Variscan belt orocline. Together, they form an imbricate system and associated wedge-top basins that are key to understanding the development of the orocline. The emplacement of the Cuera Unit and the Picos de Europa Province occurred in the latest Pennsylvanian, between Moscovian and Gzhelian times. New detailed mapping together with stratigraphic, sedimentologic, and biostratigraphic data analysis of syntectonic successions and structural information constrain the timing and evolution of this imbricate system. Our analysis indicates that the thrust sheets were emplaced roughly perpendicular to previous tectonic units of the Cantabrian Variscan foreland fold-and-thrust belt, most probably during the oroclinal bending of the SW European Variscan belt that formed the Iberian-Armorican arc. The N-S–directed imbricate system was characterized by a shallow dip of the topographic surface (α < 1°), allowing for the development of wedge-top basins. The large amount of shortening (>150 ± 15 km) and complex structure of the orogenic wedge are thought to result from the progressive increase in the dip of the basal décollement during bending of the underlying Gondwana lithosphere and may reflect the closure of the Iberian-Armorican arc. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2051324656 created "2016-06-24" @default.
• W2051324656 creator A5009199303 @default.
• W2051324656 creator A5025915493 @default.
• W2051324656 creator A5052422637 @default.
• W2051324656 creator A5064276805 @default.
• W2051324656 creator A5081538695 @default.
• W2051324656 creator A5083809124 @default.
• W2051324656 date "2009-04-27" @default.
• W2051324656 modified "2023-10-02" @default.
• W2051324656 title "Emplacement of the Cuera and Picos de Europa imbricate system at the core of the Iberian-Armorican arc (Cantabrian zone, north Spain): New precisions concerning the timing of arc closure" @default.
• W2051324656 cites W1603704122 @default.
• W2051324656 cites W1954474335 @default.
• W2051324656 cites W1966233754 @default.
• W2051324656 cites W1966824613 @default.
• W2051324656 cites W1975443961 @default.
• W2051324656 cites W1975615998 @default.
• W2051324656 cites W1976568427 @default.
• W2051324656 cites W1978503266 @default.
• W2051324656 cites W1980930235 @default.
• W2051324656 cites W1984405886 @default.
• W2051324656 cites W1985330850 @default.
• W2051324656 cites W1985819302 @default.
• W2051324656 cites W1986509574 @default.
• W2051324656 cites W1990340825 @default.
• W2051324656 cites W1993859923 @default.
• W2051324656 cites W1996151629 @default.
• W2051324656 cites W1996720026 @default.
• W2051324656 cites W2012887763 @default.
• W2051324656 cites W2013243648 @default.
• W2051324656 cites W2013853084 @default.
• W2051324656 cites W2019003007 @default.
• W2051324656 cites W2029177782 @default.
• W2051324656 cites W2031464896 @default.
• W2051324656 cites W2033298366 @default.
• W2051324656 cites W2039180525 @default.
• W2051324656 cites W2047326598 @default.
• W2051324656 cites W2052749433 @default.
• W2051324656 cites W2053518653 @default.
• W2051324656 cites W2059953658 @default.
• W2051324656 cites W2062320457 @default.
• W2051324656 cites W2063510845 @default.
• W2051324656 cites W2063963068 @default.
• W2051324656 cites W2065057512 @default.
• W2051324656 cites W2066638055 @default.
• W2051324656 cites W2066755719 @default.
• W2051324656 cites W2068200136 @default.
• W2051324656 cites W2074039741 @default.
• W2051324656 cites W2076960689 @default.
• W2051324656 cites W2077700883 @default.
• W2051324656 cites W2082726831 @default.
• W2051324656 cites W2083302925 @default.
• W2051324656 cites W2086159385 @default.
• W2051324656 cites W2095460972 @default.
• W2051324656 cites W2110949060 @default.
• W2051324656 cites W2111676506 @default.
• W2051324656 cites W2117434951 @default.
• W2051324656 cites W2121440949 @default.
• W2051324656 cites W2123167423 @default.
• W2051324656 cites W2134946466 @default.
• W2051324656 cites W2139868483 @default.
• W2051324656 cites W2140087217 @default.
• W2051324656 cites W2143627284 @default.
• W2051324656 cites W2155895997 @default.
• W2051324656 cites W2156764907 @default.
• W2051324656 cites W2172236306 @default.
• W2051324656 cites W2285820197 @default.
• W2051324656 cites W2323103518 @default.
• W2051324656 doi "https://doi.org/10.1130/b26366.1" @default.
• W2051324656 hasPublicationYear "2009" @default.
• W2051324656 type Work @default.
• W2051324656 sameAs 2051324656 @default.
• W2051324656 citedByCount "71" @default.
• W2051324656 countsByYear W20513246562012 @default.
• W2051324656 countsByYear W20513246562013 @default.
• W2051324656 countsByYear W20513246562014 @default.
• W2051324656 countsByYear W20513246562015 @default.
• W2051324656 countsByYear W20513246562016 @default.
• W2051324656 countsByYear W20513246562017 @default.
• W2051324656 countsByYear W20513246562018 @default.
• W2051324656 countsByYear W20513246562019 @default.
• W2051324656 countsByYear W20513246562020 @default.
• W2051324656 countsByYear W20513246562021 @default.
• W2051324656 countsByYear W20513246562022 @default.
• W2051324656 countsByYear W20513246562023 @default.
• W2051324656 crossrefType "journal-article" @default.
• W2051324656 hasAuthorship W2051324656A5009199303 @default.
• W2051324656 hasAuthorship W2051324656A5025915493 @default.
• W2051324656 hasAuthorship W2051324656A5052422637 @default.
• W2051324656 hasAuthorship W2051324656A5064276805 @default.
• W2051324656 hasAuthorship W2051324656A5081538695 @default.
• W2051324656 hasAuthorship W2051324656A5083809124 @default.
• W2051324656 hasConcept C127313418 @default.
• W2051324656 hasConcept C142362112 @default.
• W2051324656 hasConcept C151730666 @default.
• W2051324656 hasConcept C15708023 @default.
• W2051324656 hasConcept C161191863 @default.
• W2051324656 hasConcept C166957645 @default.

• next