Abstract

SedimentologyVolume 54, Issue 2 p. 481-481 Free Access Erratum First published: 13 March 2007 https://doi.org/10.1111/j.1365-3091.2007.00867.xAboutSectionsPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinked InRedditWechat In Sáez et al. (2006), the frames of three units in the key of Fig. 1B were incorrect. The corrected figure is reproduced below. Figure 1Open in figure viewerPowerPoint (B) Schematic map of the Upper Eocene–Lower Oligocene units in the central area of the eastern Ebro Basin. The Llobregat upper river valley and a lateral ramp associated with the Pedraforca Nappe coincide with the approximate location of the palaeovalley that fed the Cardona-Súria fluvial fan. The upper Cardener river valley and a lateral ramp associated with the Montsec Nappe coincide with the approximate location of the palaeovalley that fed the Solsona-Sanaüja fluvial fan. Reference Sáez A., Anadón P., Herrero M.J., Moscariello, A. (2006) Variable style of transition between Palaeogene fluvial fan and lacustrine systems, southern Pyrenean foreland, NE Spain. Sedimentology, 54, 367– 390. Web of Science®Google Scholar Volume54, Issue2April 2007Pages 481-481 FiguresReferencesRelatedInformation

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