2004
DOI: 10.2113/52.1.57
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Stratigraphy and paleogeography of a conglomeratic shoreline: the Notikewin Member of the Spirit River Formation in the Wapiti area of west-central Alberta

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Cited by 25 publications
(10 citation statements)
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“…The juxtaposition of marine rocks (Notikewin) above the Falher indicates the presence of a transgression surface, and Schmidt and Pemberton (2003) showed that a transgressive systems tract, bounded below and above by a transgression surface and a maximum flooding surface respectively, can be mapped using core and logs in an area immediately west of our study area. We identified their stratigraphic units in our data.…”
Section: Lithofacies VII -Carbonatesmentioning
confidence: 71%
“…The juxtaposition of marine rocks (Notikewin) above the Falher indicates the presence of a transgression surface, and Schmidt and Pemberton (2003) showed that a transgressive systems tract, bounded below and above by a transgression surface and a maximum flooding surface respectively, can be mapped using core and logs in an area immediately west of our study area. We identified their stratigraphic units in our data.…”
Section: Lithofacies VII -Carbonatesmentioning
confidence: 71%
“…The Notikewin Member had previously been described as a barrier island complex that had prograded as much as 150 km, although modern barrier islands generally form in transgressive environments. Schmidt & Pemberton's (2004) work demonstrated, however, that the barrier deposits formed in Notikewin time did not prograde a great distance as a barrier island/lagoon complex; instead sandstones and conglomerates of limited lateral extent were deposited in an orientation that was approximately parallel to the shoreline. The most prolific Notikewin Member wells occur in a narrow east -west trend through Township 67 from ranges 8 to 13W6.…”
Section: Falher Membermentioning
confidence: 97%
“…Notikewin Member Schmidt & Pemberton (2004) state that the Notikewin Member is the youngest member of the Spirit River Formation, and is underlain by the Falher and Wilrich Members, respectively. During deposition, the Western Canada Foreland Basin was inundated by the Boreal Sea, resulting in the formation of a shallow epeiric seaway.…”
Section: Falher Membermentioning
confidence: 99%
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“…Simultaneously, conglomerate reservoirs have become increasingly important and gaining more attention worldwide (Arnott, 2003;Hart and Plint, 2003;Hong et al, 2007;Liang et al, 2000;Rogers, 2007;Ş en et al, 2009;Wang et al, 2006;Zhu et al, 2003aZhu et al, , 2003bZonneveld and Moslow, 2004). For example, the lower Cretaceous Falher Member shoreface conglomerates, that are the most prolific natural gas reservoirs of the Alberta and British Columbia Deep Basin in Western Canada, have been studied for aspects of sequence stratigraphy, sedimentology, outcrop and palaeontology (Arnott, 2003;Clifton, 2003;Hart and Plint, 2003;Maceachern and Hobbs, 2004;Moslow and Zonneveld, 2004;Schmidt and Pemberton, 2004;Zonneveld and Moslow, 2004). The Garfield conglomerate pool in central Kansas (USA) was studied to develop a new reservoir model (Rogers, 2007).…”
Section: Introductionmentioning
confidence: 99%