A north-east trending structural deformation belt, with major diapiric features near North Hinder in International Colloquy on the Quaternary and Tertiary geology of the Southern Bight, NorthSea. Collected abstracts. Oral presentations.
Atlantique ; Diapirisme ; Géographie physique ; Géomorphologie structurale ; Mer du Nord ; North Hinder ; Tectonique
Stratigraphy and transgressive-regressive cycles of the Belgian Paleocene Early Eocene, compared to the Central and Northern NorthSea in International Colloquy on the Quaternary and Tertiary geology of the Southern Bight, NorthSea. Collected
Cenozoic trans-and regressions at the Belgian end of the NorthSea in International Colloquy on the Quaternary and Tertiary geology of the Southern Bight, NorthSea. Collected abstracts. Oral presentations.
The present state of knowledge on NorthSea subtidal meiofauna is discussed. From an ecological point of view, mainly the hardbodied meiofauna taxa Nematoda and Copepoda have been studied to any extent. A short review of relevant taxonomic studies
of these groups is also presented, together with a list of the known NorthSea nematode and harpacticoid species. (Les AA.).
The NorthSea and the Northern Atlantic: natural resources and the influence of Man
Europe ; Fishing ; Hydrocarbon ; International agreement ; Management ; Maritime law ; NorthSea ; Resource management ; Sea ; Sea transport ; Storage site ; Waste ; Western Europe
This paper considers the sea use management in the NorthSea with reference to the re-structuring of the global and European economies; the sectoral activities including maritime transport and strategic issues, fisheries and hydrocarbons
Modern deposits, quasi-deposits and some Holocene sequences in the Southern Bight, NorthSea in The Quaternary and Tertiary geology of the Southern Bight, NorthSea.
The varied types of modern deposit of the present-day Southern Bight are used as a partial guide for a review of the diachronous deposits of the Holocene marine transgression. The flooding of the barrier separating the Southern Bight from the North
Sea seems to be associated with a period of erosion that is recognisable at least in the vicinity of the Zeeland Ridges.
of the NorthSea. This morphology seems to be slightly controlled by the lithology and structure of the Tertiary substratum. Some remarkable planation surfaces, paleovalleys and other morphological features have been identified.
The NorthSea and northeastern Bering Sea: a comparative study of the occurrence and geometry of sand bodies of two shallow epicontinental shelves
The occurrence, geometry and formation of large sand bodies in the southern bight of the NorthSea and the Chirikov Basin in the northeastern Bering Sea are discussed. The large sand bodies consist of a lower sequence of sand banks and an upper
sequence of stacked sand waves. The geometry and arrangement of the different lithotypes are not only controlled by the latest sea level rise, but also by the basin geometry.
Last interglacial-glacial north-south geosoil traverse (from stratotypes in the NorthSea Basin and in the eastern Mediterranean)
On the basis of a number of lithostratotype sections in the southern NorthSea Belt, Sardinia and southern Greece the Last Interglacial/Glacial geosoil (fossil soils, paleosols) cycles have been comparatively studied and correlated along a north
A compilation of 93 sedimentation rate determinations based on Pb 210 dating has been carried out for the NorthSea - Baltic Sea transition area from a database containing 165 determinations carried out by Danish institutions. Sedimentationrates
significantly increase with depth indicating that the Skagerrak and northern part of the Kattegat as well as the deep basins in the Baltic Sea act as depocenters for fine-grained sediments. Apparently, sedimentation rates have increased in recent years.
Middle and Upper pleistocene and Holocene stratigraphy in the southern NorthSea between 52o and 54o N, 2o to 4o E in The Quaternary and Tertiary geology of the Southern Bight, NorthSea.
There was no connection across the southern NorthSea between the Saalian and Weichselian ice sheets of northern Europe and eastern England. Periglacial conditions prevailed offshore during both of these glacial periods, except in the northwest
, where up to 15 m of till was deposited during late Weichselian times. Marine sands and clays were deposited in the southern NorthSea during the Holsteinian and Eemian interglacial periods. The sediments of the Holocene transgression have been subdivided
The Quaternary and Tertiary geology of the Southern Bight, NorthSea.
A Monography initiated by the International Colloquy on the Quaternary and Tertiary Geology of the Southern Bight, NorthSea, Ghent, Belgium, May 28-30 1984.
Quantitative and qualitative data are given for 276 pebble (4-64 mm) and cobble (64-256 mm) specimens from eight localities of the Belgian NorthSea beach. The change in concentration of Paniselian sandstone since 1954 suggests a change
confirm the usefulness of salt-marsh foraminifera as sea-level indicators in NorthSea salt marshes.
This paper presents the data of 27 surface samples, collected from the Kjelst Enge salt marsh in Ho Bugt, Jutland, to investigate the potential use of salt-marsh foraminifera as sea-level indicators in Holocene intertidal deposits. The results
This study describes the spatial distribution of suspended particulate matter (SPM) in the NorthSea-Baltic Sea transition in autumn 2002 based on cruises in August, September, and October. The cruises comprised CTD and optical backscatter