Literatura académica sobre el tema "Barres de shoreface"
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Artículos de revistas sobre el tema "Barres de shoreface"
Angus, Lynsey, Gary J. Hampson, Francesco Palci y 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, n.º 3 (27 de marzo de 2020): 313–35. http://dx.doi.org/10.2110/jsr.2020.19.
Texto completoLiu, James T. y Gary A. Zarillo. "Simulation of grain-size abundances on a barred upper shoreface". Marine Geology 109, n.º 3-4 (enero de 1993): 237–51. http://dx.doi.org/10.1016/0025-3227(93)90063-2.
Texto completoOsborne, Philip D. y Brian Greenwood. "Frequency dependent cross-shore suspended sediment transport. 2. A barred shoreface". Marine Geology 106, n.º 1-2 (abril de 1992): 25–51. http://dx.doi.org/10.1016/0025-3227(92)90053-k.
Texto completoOjeda, E., B. G. Ruessink y J. Guillen. "Morphodynamic response of a two-barred beach to a shoreface nourishment". Coastal Engineering 55, n.º 12 (diciembre de 2008): 1185–96. http://dx.doi.org/10.1016/j.coastaleng.2008.05.006.
Texto completoIsla, Manuel F., Ernesto Schwarz y Gonzalo D. Veiga. "Record of a nonbarred clastic shoreline". Geology 48, n.º 4 (31 de enero de 2020): 338–42. http://dx.doi.org/10.1130/g46800.1.
Texto completoOsborne, Philip D. y Brian Greenwood. "Frequency dependent cross-shore suspended sediment transport. 1. A non-barred shoreface". Marine Geology 106, n.º 1-2 (abril de 1992): 1–24. http://dx.doi.org/10.1016/0025-3227(92)90052-j.
Texto completoChen, W. L. y N. Dodd. "A nonlinear perturbation study of a shoreface nourishment on a multiply barred beach". Continental Shelf Research 214 (febrero de 2021): 104317. http://dx.doi.org/10.1016/j.csr.2020.104317.
Texto completoHerbers, D. S., R. B. MacNaughton, E. R. Timmer, M. K. Gingras y 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, n.º 4 (diciembre de 2016): 538–54. http://dx.doi.org/10.2113/gscpgbull.64.4.538.
Texto completoJohannessen, Peter N. y 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 (29 de noviembre de 2006): 17–20. http://dx.doi.org/10.34194/geusb.v10.4882.
Texto completoGreenwood, Brian, Allana Permanand-Schwartz y 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, n.º 1 (19 de septiembre de 2007): 31–47. http://dx.doi.org/10.7202/016363ar.
Texto completoTesis sobre el tema "Barres de shoreface"
Grunnet, Nicholas M. "Morphodynamics of a shoreface nourishment in a barred nearshore zone /". Utrecht : Royal Dutch Geographical Society [u.a.], 2004. http://www.loc.gov/catdir/toc/fy0602/2005424561.html.
Texto completoTraoré, Kalil. "Architecture de couverture sédimentaire et enregistrement des fluctuations climatiques : baie de Sant-Brieuc". Electronic Thesis or Diss., Lorient, 2022. http://www.theses.fr/2022LORIS626.
Texto completoThe morphology and internal structure of the Horaine banner bank are described using multibeam and high- resolution seismic reflection data, coupled with vibro-coring and radiocarbon dating. The internal structure of the bank reveals 4 seismic units (U1-U4) on a proterozoic basement (U0). The basal unit U1 is interpreted as reworked lowstand fluvial sediments those infilled micro incised valleys during a rise in sea level. This unit is overlain by paleo-coastal barrier sand-spit (U2) whose development was controlled by swell in the context of a rapid rise in sea level. The successive prograding unit (U3) is interpreted as flooding deposits in continuity with unit U2. The unit U4 is characterized by oblique reflectors oriented in two opposite directions. This last unit, dated between 3800 and 3500 yr. BP, corresponds to migrating dunes superimposed on the bank and observable in the high-resolution bathymetric data. The strong correlation between tidal currents and the apparent clockwise migration of dune crests suggests the presence of a tidal gyre controlling the present- day dynamics of most of the Horaine bank dunes. A significant filling of the bay intern part by sand bar migration (100m/year on average), and dispersive flood regime is observed thanks to satellite imagery and UAV SfM photogrammetry. The cross-check with the exploratory analysis of the ERA5 climate data of the Copernicus program allowed to specify that in the medium term (decadal scale), the migration of the bars is controlled by the tidal dynamics (hydraulic power, immersion time of the bars) and in the short term (seasonal scale) the control of the intertidal dynamics seems to be ensured by the swell, and the storms. This study proposes a new integrated approach (sea-land) for monitoring bay dynamics
Libros sobre el tema "Barres de shoreface"
Morphodynamic of a shoreface nourishment in a barred nearshore zone. Utrecht: Royal Dutch Geographical Society, 2004.
Buscar texto completoGrunnet, Nicholas M. Morphodynamic of a shoreface nourishment in a barred nearshore zone. Utrecht: Royal Dutch Geographical Society, 2005.
Buscar texto completoCapítulos de libros sobre el tema "Barres de shoreface"
Cowell, Peter J. y Michael A. Kinsela. "Shoreface Controls on Barrier Evolution and Shoreline Change". En Barrier Dynamics and Response to Changing Climate, 243–75. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-68086-6_8.
Texto completoActas de conferencias sobre el tema "Barres de shoreface"
Dubey, Pranav, Adrian Okpere, Gideon Sanni y Ifeanyi Onyeukwu. "A Cost Effective, Fit-for-Purpose Single Well Producer-Injector Completion Strategy for Improved Recovery of Oil: Case Study in Niger Delta". En SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2533899-ms.
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