Готові списки джерел за темами / Barres de shoreface / Статті в журналах
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Статті в журналах з теми "Barres de shoreface"

Автор: Grafiati
Опубліковано: 31 січня 2024

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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 (<3 m height, <40 m length, <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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11

Certain, Raphaël, and Jean-Paul Barusseau. "Conceptual modelling of sand bars morphodynamics for a microtidal beach (Sète, France)." Bulletin de la Société Géologique de France 176, no. 4 (2005): 343–54. http://dx.doi.org/10.2113/176.4.343.

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Abstract The sandy littoral of Sète, with its barred shoreface, is one of the three studied sites of the thematic action “Morphodynamics of sandy beaches” of the French Programme National d’Environnement Côtier (PNEC), selected because of its microtidal wave-dominated characteristics and of the long time series of available data. During the PNEC program, the principal results obtained show that the morphological evolution of the sedimentary bars can be synthesized according to two conceptual models, in reaction to hydrodynamic variability. (1) The model of “oscillation around a position of e
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12

Nik Ramli (2). "Depositional Model of a Miocene Barred Wave- and Storm-Dominated Shoreface and Shelf, Southeastern Malay Basin, Offshore West Malaysia." AAPG Bulletin 70 (1986). http://dx.doi.org/10.1306/9488561f-1704-11d7-8645000102c1865d.

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13

ZONNEVELD, JOHN-PAUL, THOMAS F. MOS. "Abstract: Evolution Of A Barred Barrier Island Shoreface Succession: Doig, Halfway & Basal Charlie Lake Formations (Triassic), British Columbia, Canada." AAPG Bulletin 83 (1999) (1999). http://dx.doi.org/10.1306/c9ebcd15-1735-11d7-8645000102c1865d.

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14

Waziri, E. U., E. E. Udensi, C. I. Unuevho, et al. "Geophysical Well Log Appraisal of Okpella Field within Offshore Niger Delta Basin of Nigeria." Journal of Geography, Environment and Earth Science International, May 18, 2022, 28–49. http://dx.doi.org/10.9734/jgeesi/2022/v26i530350.

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The Production data of Okpella Field, located within the Offshore Niger Delta Basin, Nigeria, revealed that the Okpella Field attained peak annual hydrocarbon production of 430175 MBO (Million Barrel of Oil) in 2008, and the production has presently dropped to 7839 MBO per annum. Therefore, an appraisal study was conducted to identify opportunities for reversing the low production. The sought opportunities were bypassed reservoirs with pay zones. This study uses geophysical Well log data, Biostratigraphic data, and Production data to appraise Okpella Field. The hydrocarbon production data were
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15

VEIGA, Fernando Alvim, Rodolfo José ANGULO, Eduardo MARONE, and Frederico Pereira BRANDINI. "CARACTERÍSTICAS SEDIMENTOLÓGICAS DA PLATAFORMA CONTINENTAL INTERNA RASA NA PORÇÃO CENTRAL DO LITORAL PARANAENSE." Boletim Paranaense de Geociências 55 (December 31, 2004). http://dx.doi.org/10.5380/geo.v55i0.4285.

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O objetivo deste trabalho é caracterizar os sedimentos da plataforma continental interna paranaense entre as profundidades de 5 a 15 m entre os estuários de Guaratuba, ao sul e Paranaguá, ao norte da área de estudo. Informações batimétricas, análises granulométricas e determinação de teores de carbonato e matéria orgânica de amostras de sedimentos de fundo permitiram a geração dos mapas temáticos. Observou-se uma grande predominância de areia fina, porém a média granulométrica dos sedimentos varia do silte grosso até a areia grossa. Foram identificados cinco padrões distintos de sedimentos na
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