Basin-scale dolomite cementation of shoreface sandstones in response to sea-level fall

Abstract

Research Article| October 01, 2003 Basin-scale dolomite cementation of shoreface sandstones in response to sea-level fall Kevin G. Taylor; Kevin G. Taylor 1Department of Environmental and Geographical Sciences, Manchester Metropolitan University, Chester Street, Manchester M1 5GD, UK Search for other works by this author on: GSW Google Scholar Rob. L. Gawthorpe Rob. L. Gawthorpe 2Department of Earth Sciences, University of Manchester, Oxford Road, Manchester M13 9PL, UK Search for other works by this author on: GSW Google Scholar GSA Bulletin (2003) 115 (10): 1218–1229. https://doi.org/10.1130/B25227.1 Article history received: 01 Aug 2002 rev-recd: 15 Jan 2003 accepted: 12 Mar 2003 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Kevin G. Taylor, Rob. L. Gawthorpe; Basin-scale dolomite cementation of shoreface sandstones in response to sea-level fall. GSA Bulletin 2003;; 115 (10): 1218–1229. doi: https://doi.org/10.1130/B25227.1 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 This study documents a link between sea-level fall and basin-scale dolomite cementation of shoreface sandstones in the Upper Cretaceous Desert Member, Book Cliffs, Utah, by integrating sedimentology, sequence stratigraphy, and sedimentary geochemistry. Within the Desert Member shoreface sandstones, a number of high- frequency sequence boundaries formed as a result of relative sea-level falls that led to localized incised valley formation, subaerial exposure, and meteoric leaching of upper shoreface sandstones. Shoreface sandstones up to 10 km downdip from these subaerial exposure surfaces contain ferroan dolomite concretion bodies as much as 8 m thick. Basinward of this smaller (as much as 1 m in size), less abundant dolomite, concretions can be traced at the same horizons. Some δ18O data suggest that cement precipitated from porewater with a significant meteoric component, although reequilibration and recyrstallization cannot be eliminated. Some δ13C data suggest carbonate derivation from detrital dolomite leached from beneath organic-rich coastal plain strata deposited during high-frequency sequence boundary development. We propose that during high-frequency sequence boundary formation, meteoric fluids migrated basinward into shoreface sandstones as a result of the relative fall in sea level. The precipitation of dolomite cement in the shoreface sandstones was promoted by the updip dissolution and remobilization of detrital dolomite by the meteroic fluids, mixing with marine pore fluids, and the presence of detrital dolomite in the shoreface sandstones, which acted as nucleation sites for dolomite precipitation. This study illustrates the impact of stratigraphic development upon basin-scale early diagenetic cementation of siliciclastic succcesions. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.