{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,9,3]],"date-time":"2026-09-03T04:08:26Z","timestamp":1788408506943,"version":"build-2803163510"},"reference-count":0,"publisher":"Society for Sedimentary Geology","issue":"4","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[1991,7,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>The Exxon sequence models of Posamentier and coworkers incorporate two concepts which I question. They suggest that rivers grade to a \"bayline\", but evidence from modern major rivers indicates that they do not. They also proposed that fluvial sedimentary accomodation space is generated by the seaward shift in equilibrium profiles during sea-level fall, but this is too simplistic a model, based on the use of schematic continental margin configurations which do not incorporate real slope and relief data. In most cases, a fall in base level leads to deltaic progradation and upstream fluvial incision. Most coastal plain fluvial wedges result from two processes: sea-level rise, with the drowning and filling of estuaries, and active source-area tectonism. Major tectonic events adjacent to foreland basins, such as terrane collisions, lead to the development of sequences of third-order type (duration approximately 1-15 m.y.). Changes in intraplate stress regimes resulting from changes in regional plate kinematics have a similar episodicity and can be shown to be responsible for some third-order cycles on extensional continental margins. Examination of the chronostratigraphic basis of the Mesozoic-Cenozoic Cycle Chart of Haq and coworkers reveals internal inconsistencies and an unrealistic downplaying of the built-in potential for error. This chart is not an approved global standard, and it should be used with extreme caution.<\/jats:p>","DOI":"10.1306\/d4267744-2b26-11d7-8648000102c1865d","type":"journal-article","created":{"date-parts":[[2003,1,19]],"date-time":"2003-01-19T19:21:18Z","timestamp":1043004078000},"page":"497-505","source":"Crossref","is-referenced-by-count":30,"title":["Stratigraphic sequences and their chronostratigraphic correlation"],"prefix":"10.2110","volume":"61","author":[{"given":"Andrew D.","family":"Miall","sequence":"first","affiliation":[{"name":"Univ. Toronto, Geol. Dep., Toronto, ON, Canada"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"860","published-online":{"date-parts":[[1991,7,1]]},"container-title":["Journal of Sedimentary Research"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/pubs.geoscienceworld.org\/sepm\/jsedres\/article-pdf\/61\/4\/497\/2810764\/497.pdf","content-type":"application\/pdf","content-version":"vor","intended-application":"syndication"},{"URL":"https:\/\/pubs.geoscienceworld.org\/sepm\/jsedres\/article-pdf\/61\/4\/497\/2810764\/497.pdf","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2026,5,27]],"date-time":"2026-05-27T20:37:32Z","timestamp":1779914252000},"score":1,"resource":{"primary":{"URL":"https:\/\/pubs.geoscienceworld.org\/jsedres\/article\/61\/4\/497\/98301\/Stratigraphic-sequences-and-their"},"secondary":[{"URL":"http:\/\/jsedres.geoscienceworld.org\/cgi\/doi\/10.1306\/D4267744-2B26-11D7-8648000102C1865D","label":"geoscienceworld"}]},"subtitle":[],"short-title":[],"issued":{"date-parts":[[1991,7,1]]},"references-count":0,"journal-issue":{"issue":"4","published-online":{"date-parts":[[1991,7,1]]},"published-print":{"date-parts":[[1991,7,1]]}},"URL":"https:\/\/doi.org\/10.1306\/d4267744-2b26-11d7-8648000102c1865d","relation":{},"ISSN":["1938-3681","1527-1404"],"issn-type":[{"value":"1938-3681","type":"electronic"},{"value":"1527-1404","type":"print"}],"subject":[],"published-other":{"date-parts":[[1991,7,1]]},"published":{"date-parts":[[1991,7,1]]}}}