Recognition of wave-dominated, tide-influenced shoreline systems in the rock record: Variations from a microtidal shoreline model

Vakarelov, Boyan K.; Ainsworth, R. Bruce; MacEachern, James A.

doi:10.1016/j.sedgeo.2011.03.004

Cited by 104 publications

(92 citation statements)

References 59 publications

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“…In contrast, the low-angle cross-bedded, very fine-to fine grained sandstone beds of facies F6a are interpreted as the expression in core of HCS (Scott, 1992), which resulted from storm wave action (Dott and Bourgeois, 1982;Duke, 1985;Keen et al, 2012). The paired laminae in these beds can be interpreted to reflect the daily inequality of semi-diurnal tides (Vakarelov et al, 2012;Wei et al, 2016). However, assuming that a single HCS bed is deposited by a single event ( Figure 6B) implies that a single bed containing 30 paired laminae ( Figure 6B) represents a storm with a duration of at least one month.…”

Section: Discussionmentioning

confidence: 99%

Depositional evolution of a progradational to aggradational, mixed-influenced deltaic succession: Jurassic Tofte and Ile formations, southern Halten Terrace, offshore Norway

Cappelle

Ravnås

Hampson

et al. 2017

Marine and Petroleum Geology

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Hightlights:• Core-based sedimentology of Jurassic deltaic strata from offshore Norway• Facies analysis of tide-influenced deltaic and estuarine petroleum reservoirs represented by an overall upward decrease in grain size, decrease in fluvial influence and increase in tidal influence. This evolution is attributed to an allogenic increase in the rate of accommodation space generation relative to sediment supply due to tectonic activity of the rift basin. In addition, during progradation, there was also an autogenic increase in sediment storage on the coastal plain, resulting in a gradual autoretreat of the depositional system. This is manifested in the subsequent aggradation of the system, when coarse-grained sandstones were trapped in proximal locations, while only finer grained sediment reached the coastline, where it was readily reworked by tidal and wave processes.

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Section: Discussionmentioning

confidence: 99%

Depositional evolution of a progradational to aggradational, mixed-influenced deltaic succession: Jurassic Tofte and Ile formations, southern Halten Terrace, offshore Norway

Cappelle

Ravnås

Hampson

et al. 2017

Marine and Petroleum Geology

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show abstract

“…The presence of hummocky cross stratified sandstone and amalgamated layers swaley cross stratified sandstone suggest recurrence of storms in shallow marine environment (Harms et al 1975, Dott & Bourgeois 1983, Duke 1985, Dumas & Arnott 2006, Vakarelov et al 2012. Coastal environments were installed on the border of Amazon Craton, and the occurrence of storms suggests subtropical paleolatitude.…”

Section: Discussionmentioning

confidence: 99%

Sedimentology and stratigraphy of Neoproterozoic-lower Paleozoic carbonate-siliciclastic succession of the southwesternmost Amazon Craton, state of Rondônia, Brazil

Afonso

Nogueira

2018

Braz. J. Geol.

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“…Both Curvolithus (Fürsich and Heinberg, 1983;Ma ples and Suttner, 1990;Buatois and Mángano, 2011) Al though Macaronichnus may be re garded as most typ i cal of fore shore to shoreface (es pe cially up per shoreface) en vi ronments (Clifton and Thomp son, 1978), but it can oc cur also in lower shoreface (Curran, 1985;D'Alessandro and Uchman, 2007;Rygel et al, 2008;Vakarelov et al, 2012), off shore settings (Ma ples and Suttner, 1990;Pol lard et al, 1993) and even deep-sea (Greene et al, 2012). Uchman and Kenmayr (2004) and Bromley et al (2009) no ticed prob lems with en vi ron men tal in ter pre ta tion of Macaronichnus.…”

Section: Reconstruction Of the Middle Turonian Environment On The Basmentioning

confidence: 99%

Middle Turonian trace fossils from the Bystrzyca and Długopole sandstones

Chrząstek

2013

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The Mid dle Turonian sed i ments of the Nysa K³odzka Graben (Bystrzyca Sand stone in the Stara Bystrzyca out crop and the D³ugopole Sand stone in D³ugopole Górne Quarry) con tain trace fos sils, which in clude Curvolithus sim plex, ?Macaronichnus isp., Ophiomorpha nodosa, Ophiomorpha isp., Palaeophycus tubularis, Thalassinoides cf. paradoxicus, T. suevicus and Thalassinoides isp. The as sem blage of trace fos sils points to the prox i mal Cruziana ichnofacies, that char ac ter izes the dis tal lower shoreface and the ar che typal Cruziana ichnofacies, typ i cal of up per off shore set tings. The trace fos sils ev i dence implies that sed i men ta tion took place in a shal low ba sin with pe ri ods of a sud den sed i ment in put, good ox y gen a tion and nor mal sa lin ity. The Bystrzyca and D³ugopole sand stones are de pos its of the shal low epicontinental sea that were de pos ited between the fair-weather and storm-wave base, in the dis tal lower shoreface-up per off shore set ting. The Bystrzyca Sand stone is rec og nized as storm-orig i nated de pos its, whereas the D³ugopole Sand stone is prob a bly the part of prograding "ac cu mu lation ter race". The source of ma te rial for the sand stone was the East Sudetic Is land and prob a bly also the Orlica-Bystrzyca Up lift. The stud ied sand stones are re lated to a re gres sion that started in the early/mid dle Mid dle Turonian and caused a rel ative up lift of the sur round ing land.

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Recognition of wave-dominated, tide-influenced shoreline systems in the rock record: Variations from a microtidal shoreline model

Cited by 104 publications

References 59 publications

Depositional evolution of a progradational to aggradational, mixed-influenced deltaic succession: Jurassic Tofte and Ile formations, southern Halten Terrace, offshore Norway

Depositional evolution of a progradational to aggradational, mixed-influenced deltaic succession: Jurassic Tofte and Ile formations, southern Halten Terrace, offshore Norway

Sedimentology and stratigraphy of Neoproterozoic-lower Paleozoic carbonate-siliciclastic succession of the southwesternmost Amazon Craton, state of Rondônia, Brazil

Middle Turonian trace fossils from the Bystrzyca and Długopole sandstones

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