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  • 1995-1999  (5)
  • 1
    Unknown
    London : The Geological Society
    Keywords: Schelf ; Siliziklastisches Gestein ; Coasts ; Continental shelf ; Marine sediments ; Submarine geology
    Description / Table of Contents: Stratigraphy and Sedimentary Geology of Siliciclastic Shelves --- O. Michelsen and M. Danielsen: Sequence and systems tract interpretation of the epicontinental Oligocene deposits in the Danish North Sea / Geological Society, London, Special Publications, 117:1-13, doi:10.1144/GSL.SP.1996.117.01.01 --- P. B. Konradi: Foraminiferal biostratigraphy of the post-mid-Miocene in the Danish Central Trough, North Sea / Geological Society, London, Special Publications, 117:15-22, doi:10.1144/GSL.SP.1996.117.01.02 --- P. Jacobs and M. De Batist: Sequence stratigraphy and architecture on a ramp-type continental shelf: the Belgian Palaeogene / Geological Society, London, Special Publications, 117:23-48, doi:10.1144/GSL.SP.1996.117.01.03 --- D. Mellere and R. J. Steel: Tidal sedimentation in Inner Hebrides half grabens, Scotland: the Mid-Jurassic Bearreraig Sandstone Formation / Geological Society, London, Special Publications, 117:49-79, doi:10.1144/GSL.SP.1996.117.01.04 --- L. A. Spalletti: Estuarine and shallow-marine sedimentation in the Upper Cretaceous-Lower Tertiary west-central Patagonian Basin (Argentina) / Geological Society, London, Special Publications, 117:81-93, doi:10.1144/GSL.SP.1996.117.01.05 --- Modern siliciclastic Shelves: Architecture, Sea Level, Tectonics and Sediment Supply --- J. B. Anderson, K. Abdulah, S. Sarzalejo, F. Siringan, and M. A. Thomas: Late Quaternary sedimentation and high-resolution sequence stratigraphy of the east Texas shelf / Geological Society, London, Special Publications, 117:95-124, doi:10.1144/GSL.SP.1996.117.01.06 --- G. Ercilla and B. Alonso: Quaternary siliciclastic sequence stratigraphy of western Mediterranean passive and tectonically active margins: the role of global versus local controlling factors / Geological Society, London, Special Publications, 117:125-137, doi:10.1144/GSL.SP.1996.117.01.07 --- F. J. Hernández-Molina, L. Somoza, and J. Rey: Late Pleistocene-Holocene high-resolution sequence analysis on the Alboran Sea continental shelf / Geological Society, London, Special Publications, 117:139-154, doi:10.1144/GSL.SP.1996.117.01.08 --- A. Correggiari, M. E. Field, and F. Trincardi: Late Quaternary transgressive large dunes on the sediment-starved Adriatic shelf / Geological Society, London, Special Publications, 117:155-169, doi:10.1144/GSL.SP.1996.117.01.09 --- P. J. Bart and J. B. Anderson: Seismic expression of depositional sequences associated with expansion and contraction of ice sheets on the northwestern Antarctic Peninsula continental shelf / Geological Society, London, Special Publications, 117:171-186, doi:10.1144/GSL.SP.1996.117.01.10 --- H. P. Sejrup, E. L. King, I. Aarseth, H. Haflidason, and A. Elverhøi: Quaternary erosion and depositional processes: western Norwegian fjords, Norwegian Channel and North Sea Fan / Geological Society, London, Special Publications, 117:187-202, doi:10.1144/GSL.SP.1996.117.01.11 --- G. Lericolais, P. Guennoc, J.-P. Auffret, J.-F. Bourillet, and S. Berne: Detailed survey of the western end of the Hurd Deep (English Channel): new facts for a tectonic origin / Geological Society, London, Special Publications, 117:203-215, doi:10.1144/GSL.SP.1996.117.01.12 --- Nearshore and Coastal Environments --- J. M. L. Dominguez: The São Francisco strandplain: a paradigm for wave-dominated deltas? / Geological Society, London, Special Publications, 117:217-231, doi:10.1144/GSL.SP.1996.117.01.13 --- J. V. Barrie and K. W. Conway: Evolution of a nearshore and coastal macrotidal sand transport system, Queen Charlotte Islands, Canada / Geological Society, London, Special Publications, 117:233-247, doi:10.1144/GSL.SP.1996.117.01.14 --- W. J. Cleary, S. R. Riggs, D. C. Marcy, and S. W. Snyder: The influence of inherited geological framework upon a hardbottom-dominated shoreface on a high-energy shelf: Onslow Bay, North Carolina, USA / Geological Society, London, Special Publications, 117:249-266, doi:10.1144/GSL.SP.1996.117.01.15 --- V. Eitner, R. Kaiser, H. D. Niemeyer, and V. Eitner: Nearshore sediment transport processes due to moderate hydrodynamic conditions / Geological Society, London, Special Publications, 117:267-288, doi:10.1144/GSL.SP.1996.117.01.16 --- New Techniques in Continental Shelf Research --- R. J. De Meijer, I. C. Tánczos, and C. Stapel: Radiometry as a technique for use in coastal research / Geological Society, London, Special Publications, 117:289-297, doi:10.1144/GSL.SP.1996.117.01.17 --- T. Missiaen, T. M. McGee, D. Pearks, G. Ollier, and F. Theilen: An interdisciplinary approach to the evaluation of physical parameters of shallow marine sediments / Geological Society, London, Special Publications, 117:299-322, doi:10.1144/GSL.SP.1996.117.01.18 --- A. M. Davis: Geophysics in offshore site investigation: a review of the state of the art / Geological Society, London, Special Publications, 117:323-338, doi:10.1144/GSL.SP.1996.117.01.19
    Pages: Online-Ressource (VIII, 345 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799713
    Language: English
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  • 2
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The architecture of a tidal sand bank in the south-eastern Celtic Sea was examined using very high-resolution seismic surveys. The bank comprises four depositional units. The lowest unit 1 is characterized by gently dipping (1–8°) strata that strike parallel to the length of the bank. Unit 1 is erosionally overlain by unit 2, which forms the bulk of the bank. This unit consists of stacked sets of downcurrent-dipping (7–12°) master bedding formed by climbing, sinuous-crested tidal dunes that are up to 20 m high. These deposits are locally incised by an anastomosed channel network (unit 3) that may represent a buried swatchway system. The upper part of the bank comprises wave-related deposits that are mainly preserved on the bank flanks (unit 4). The outer bank surface is erosional. The bank is believed to have formed during the last post-glacial sea-level rise. The facies evolution from unit 1 to unit 3 indicates an upward increase in tidal energy, mainly characterized by the thickening of dune cross-bed sets in unit 2. The majority of bank growth is inferred to have occurred in water depths of the order of 60 m. This evolution was controlled by relative sea-level rise, which is likely to have caused an episode of tidal resonance with associated strong tidal currents that were responsible for the incision of the deep, cross-cutting channels of unit 3. The transition to wave-dominated sedimentation in unit 4 is related to the decay of resonance with continued sea-level rise.
    Type of Medium: Electronic Resource
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  • 3
  • 4
  • 5
    Publication Date: 1998-08-01
    Print ISSN: 0025-3227
    Electronic ISSN: 1872-6151
    Topics: Geosciences
    Published by Elsevier
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