Erratum

Abstract

SedimentologyVolume 51, Issue 5 p. 1155-1155 Free Access Erratum First published: 17 August 2004 https://doi.org/10.1111/j.1365-3091.2004.00667.xCitations: 1AboutSectionsPDF 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 Lunt et al. (2004), the following error was published in Fig. 24b on page 405. In part B of Fig. 24b, a section of descriptive fill patterns has not been reproduced. The publisher apologizes for this error. Please find the corrected figure below. Figure 24bOpen in figure viewerPowerPoint Cross-sections showing large-scale inclined strata (associated with compound and unit bars) from deposits in the active part of the channel belt. Vertical exaggeration is 2:1. Thin lines represent large-scale strata, medium weight lines represent bases of large-scale sets, and thick lines represent bases of compound sets. Large-scale strata generally dip at < 12°, but may be up to the angle of repose. References Lunt, I.A., Bridge, J.S., Tye, R.S. (2004) A quantitative three-dimensional depositional model of gravelly braided rivers. Sedimentology, 51, 377– 414.DOI: 10.1111/j.1365-3091.2004.00627.x Wiley Online LibraryWeb of Science®Google Scholar Citing Literature Volume51, Issue5October 2004Pages 1155-1155 FiguresReferencesRelatedInformation