Research Article| September 01, 2009 Sequence stratigraphy hierarchy and the accommodation succession method Jack Neal; Jack Neal 1ExxonMobil Exploration Company, 233 Benmar Drive, Houston, Texas 77060, USA Search for other works by this author on: GSW Google Scholar Vitor Abreu Vitor Abreu 1ExxonMobil Exploration Company, 233 Benmar Drive, Houston, Texas 77060, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Jack Neal 1ExxonMobil Exploration Company, 233 Benmar Drive, Houston, Texas 77060, USA Vitor Abreu 1ExxonMobil Exploration Company, 233 Benmar Drive, Houston, Texas 77060, USA Publisher: Geological Society of America Received: 31 Dec 2008 Revision Received: 23 Mar 2009 Accepted: 09 Apr 2009 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2009 Geological Society of America Geology (2009) 37 (9): 779–782. https://doi.org/10.1130/G25722A.1 Article history Received: 31 Dec 2008 Revision Received: 23 Mar 2009 Accepted: 09 Apr 2009 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jack Neal, Vitor Abreu; Sequence stratigraphy hierarchy and the accommodation succession method. Geology 2009;; 37 (9): 779–782. doi: https://doi.org/10.1130/G25722A.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 We propose a framework for the hierarchy of sedimentary units observed in stratigraphic data that is based entirely on the geometric relationship of the strata. This framework of geometries is assumed to result from repeated successions of accommodation creation and sediment fill (here named accommodation succession). We have modified existing hierarchal frameworks to describe depositional units resulting from accommodation successions of varying magnitude and duration, across a depositional profile. Each full succession consists of component partial succession sets that are, sequentially, lowstand—progradation to aggradational; transgressive—retrogradation; and highstand—aggradation to progradation to degradation. The terms "highstand" and "lowstand" as originally defined to label systems tracts relative to a shelf edge, and with an implied relationship between sea level and systems tracts, have been the root of confusion. We propose that these terms be used in the strict sense of the original definition, because their meaning has been lost when applied to the many depositional settings and high-resolution data sets to which the concepts of sequence stratigraphy are now applied. We propose that the concept of accommodation succession stacking be used in the interpretation of stratigraphic data within a hierarchal framework of depositional sequences, sequence sets, and composite sequences. This will allow an interpreter to accurately categorize observations, provide a basis for predictions away from control points, and develop a framework that allows revisions as higher-resolution data become available. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
No takes yet. Share an insight, caveat, or question.
Neal et al. (2009) studied this question.
Synapse has enriched 2 closely related papers on similar clinical questions. Consider them for comparative context: