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- W1996116293 abstract "Research Article| October 01, 1998 Contemporaneity of component units of the lowstand systems tract: An example from the Pleistocene Kazusa forearc basin, Boso Peninsula, Japan Makoto Ito Makoto Ito 1Department of Earth Sciences, Chiba University, Chiba 263, Japan Search for other works by this author on: GSW Google Scholar Author and Article Information Makoto Ito 1Department of Earth Sciences, Chiba University, Chiba 263, Japan Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1998) 26 (10): 939–942. https://doi.org/10.1130/0091-7613(1998)026<0939:COCUOT>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Makoto Ito; Contemporaneity of component units of the lowstand systems tract: An example from the Pleistocene Kazusa forearc basin, Boso Peninsula, Japan. Geology 1998;; 26 (10): 939–942. doi: https://doi.org/10.1130/0091-7613(1998)026<0939:COCUOT>2.3.CO;2 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 The lowstand systems tract of the standard sequence-stratigraphic model consists of three major component units—in ascending order, the basin-floor fan, slope fan, and lowstand wedge. However, there are no modern or ancient examples of a lowstand systems tract that contain each of the three component units from the base to top. Three-dimensional outcrop analysis and detailed chronostratigraphic correlation of the lowstand deposits that infilled the Pleistocene Kazusa forearc basin exposed on the Boso Peninsula of Japan reveal that the three component units of the lowstand systems tract are largely age equivalent. Their development was controlled much more by geographic setting, in conjunction with spatial variation in sediment supply and basin subsidence, than by the position of relative sea level. It is concluded that the lowstand systems tract of the sequence-stratigraphic model is a theoretical concept that is not accurately reflected in the stratigraphic relationships shown in the present field case. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W1996116293 title "Contemporaneity of component units of the lowstand systems tract: An example from the Pleistocene Kazusa forearc basin, Boso Peninsula, Japan" @default.
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