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Relevant bibliographies by topics / Barres de shoreface

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Journal articles

Academic literature on the topic 'Barres de shoreface'

Author: Grafiati

Published: 31 January 2024

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Journal articles on the topic "Barres de shoreface"

1

Angus, Lynsey, Gary J. Hampson, Francesco Palci, and Alastair J. Fraser. "Characteristics and context of high-energy, tidally modulated, barred shoreface deposits: Kimmeridgian–Tithonian sandstones, Weald Basin, southern U.K. and northern France." Journal of Sedimentary Research 90, no. 3 (2020): 313–35. http://dx.doi.org/10.2110/jsr.2020.19.

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ABSTRACT The influence of tides on the sedimentology of wave-dominated shorefaces has been emphasized in recent studies of modern shorelines and related facies models, but few ancient examples have been reported to date. Herein, we use a case study from the stratigraphic record to develop a revised facies model and predictive spatio-temporal framework for high-energy, tidally modulated, wave-dominated, barred shorefaces. Kimmeridgian–Tithonian shallow-marine sandstones in the Weald Basin (southern England and northern France) occur as a series of laterally extensive tongues that are 5–24 m thi

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2

Liu, James T., and Gary A. Zarillo. "Simulation of grain-size abundances on a barred upper shoreface." Marine Geology 109, no. 3-4 (1993): 237–51. http://dx.doi.org/10.1016/0025-3227(93)90063-2.

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3

Osborne, Philip D., and Brian Greenwood. "Frequency dependent cross-shore suspended sediment transport. 2. A barred shoreface." Marine Geology 106, no. 1-2 (1992): 25–51. http://dx.doi.org/10.1016/0025-3227(92)90053-k.

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4

Ojeda, E., B. G. Ruessink, and J. Guillen. "Morphodynamic response of a two-barred beach to a shoreface nourishment." Coastal Engineering 55, no. 12 (2008): 1185–96. http://dx.doi.org/10.1016/j.coastaleng.2008.05.006.

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5

Isla, Manuel F., Ernesto Schwarz, and Gonzalo D. Veiga. "Record of a nonbarred clastic shoreline." Geology 48, no. 4 (2020): 338–42. http://dx.doi.org/10.1130/g46800.1.

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Abstract The morphology of wave-dominated clastic shorelines (i.e., foreshore and upper-shoreface sediments) can vary from barred to nonbarred, though the ancient record of nonbarred, sand-dominated shorelines has yet to be recognized. Here, a facies and quantitative architectural analysis of a clastic succession characterized by sandy inclined beds is presented and interpreted as the record of a high-gradient, nonbarred shoreline. Inclined beds dip seaward, have a tangential geometry (&lt;3 m height, &lt;40 m length, &lt;11° dip), and are composed of planar lamination along the fo

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6

Osborne, Philip D., and Brian Greenwood. "Frequency dependent cross-shore suspended sediment transport. 1. A non-barred shoreface." Marine Geology 106, no. 1-2 (1992): 1–24. http://dx.doi.org/10.1016/0025-3227(92)90052-j.

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7

Chen, W. L., and N. Dodd. "A nonlinear perturbation study of a shoreface nourishment on a multiply barred beach." Continental Shelf Research 214 (February 2021): 104317. http://dx.doi.org/10.1016/j.csr.2020.104317.

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8

Herbers, D. S., R. B. MacNaughton, E. R. Timmer, M. K. Gingras, and Steven Hubbard. "Sedimentology and ichnology of an Early-Middle Cambrian storm-influenced barred shoreface succession, Colville Hills, Northwest Territories." Bulletin of Canadian Petroleum Geology 64, no. 4 (2016): 538–54. http://dx.doi.org/10.2113/gscpgbull.64.4.538.

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9

Johannessen, Peter N., and Lars Henrik Nielsen. "Spit-systems – an overlooked target in hydrocarbon exploration: the Holocene to Recent Skagen Odde, Denmark." Geological Survey of Denmark and Greenland (GEUS) Bulletin 10 (November 29, 2006): 17–20. http://dx.doi.org/10.34194/geusb.v10.4882.

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Well-constrained depositional models are essential for successful exploration and field development. The Skagen spitsystem offers a unique possibility for the establishment of a depositional model constrained by excellent outcrops, welldefined palaeogeography, good age control and detailed observations on hydrodynamics and morphology of the prograding part of the spit-system. The model offers a supplementary interpretation of shallow marine sandstones to the existing delta and linear shoreface models. The sand-dominated Skagen spit-system is c.22 km long, 4 km wide and up to 35 m thick, with a

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10

Greenwood, Brian, Allana Permanand-Schwartz, and Christopher A. Houser. "Emergence and Migration of a Nearshore Bar: Sediment Flux and Morphological Change on a Multi-Barred Beach in the Great Lakes." Géographie physique et Quaternaire 60, no. 1 (2007): 31–47. http://dx.doi.org/10.7202/016363ar.

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Abstract Burley Beach (southeastern Lake Huron) exhibits a multi-barred shoreface, the long-term equilibrium morphology characteristic of many low angle, sandy beaches in the Canadian Great Lakes. During a single major storm, a new bar emerged 50-60 m offshore as an irregular trough-crest form, through differential erosion of an existing shore terrace. Emergence, bar growth and offshore migration were associated with: (a) an overall negative sediment balance in the inner surf zone initially (‑2.30 m3>/m beach width), but with a large positive sediment balance (+5.10 m3/m) subsequent to the

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