Top Reservoir Mapping Problems in the United Kingdom Sector of the North Sea

1973 ◽  
Author(s):  
Jack W. Moore
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
The North ◽  
The United Kingdom ◽  
The North Sea

List of Publications Recording the Results of Researches carried out under the Auspices of the Marine Biological Association of the United Kingdom in their Laboratory at Plymouth or on the North Sea Coast from 1886–1900

1900 ◽  
Vol 6 (1) ◽  
pp. 115-135
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Biological Association ◽  
The North ◽  
Marine Biological Association ◽  
The United Kingdom ◽  
The North Sea ◽  
Different Parts ◽  
Sea Coast ◽  
North Sea Coast

The following list has been classified, so far as practicable, according to subjects, in order that it may be useful for purposes of reference. The list does not include publications recording the results of observations made on material supplied by the Association to workers in different parts of the country, of which a considerable amount is sent out each year.

scholarly journals On the Manufacture of Drift Bottles

1922 ◽  
Vol 12 (4) ◽  
pp. 700-716 ◽  
Author(s):  
E. W. Nelson
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Biological Association ◽  
Marine Biological ◽  
The North ◽  
Marine Biological Association ◽  
The United Kingdom ◽  
The North Sea

In the spring of 1920 the Ministry of Agriculture and Fisheries approached the Marine Biological Association of the United Kingdom with a view to the Association undertaking the manufacture of a large number of “Drift Bottles,” to be used in an extensive research into the resultant movements of the waters of the North Sea.

List of Publications Recording the Results of Researches carried out under the Auspices of the Marine Biological Association of the United Kingdom in their Laboratory at Plymouth or on the North Sea Coast from 1886–1907

1908 ◽  
Vol 8 (2) ◽  
pp. 241-264
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Biological Association ◽  
The North ◽  
Marine Biological Association ◽  
The United Kingdom ◽  
The North Sea ◽  
Different Parts ◽  
Sea Coast ◽  
North Sea Coast

The following list has been classified, so far as practicable, according to subjects, in order that it may be useful for purposes of reference. The list does not include publications recording the results of observations made on material supplied by the Association to workers in different parts of the country, of which a considerable amount is sent out each. year.

scholarly journals Stratigraphy of Maastrichtian Foraminiferida from the United Kingdom; the Maastrichtian of Norfolk

2003 ◽  
Vol 82 (3) ◽  
pp. 233-245 ◽  
Author(s):  
M. Hart ◽  
T. Swiecicki
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Upper Cretaceous ◽  
North Coast ◽  
Flood Basalts ◽  
Glacial Sediments ◽  
The North ◽  
The United Kingdom ◽  
The North Sea ◽  
Atlantic Margin

AbstractOnshore Maastrichtian strata in the United Kingdom are limited to a few small, isolated blocks of chalk floating within glacial sediments on the Norfolk coast. Isolated outcrops of Campanian and Maastrichtian chalks used to be available around Norwich but the majority of these exposures are now badly degraded. Offshore, in the North Sea Basin, there are complete chalk successions that range throughout the Upper Cretaceous and Lower Cenozoic. There is a limited succession of Maastrichtian chalks exposed on the north coast of Northern Ireland below the Cenozoic flood basalts. In the Western Approaches Basin, Maastrichtian and Danian chalks are known from exploration wells and core samples. West of the United Kingdom a number of DSDP/ODP boreholes have penetrated the Upper Cretaceous succession.Beginning in the Cenomanian, in southeast England, the whole of the Upper Cretaceous is within the chalk facies, possibly one of the longest intervals of relatively stable environment in the geological record. The Foraminiferida of the chalk have been studied for more than a hundred years and therefore the fauna is exceptionally well known and fully documented. Fifty years ago, the benthonic Foraminiferida were identified as having the potential to provide a viable zonation of the chalk facies and we now have precise, cross-basinal correlation using these taxa.The planktonic fauna is restricted by both palaeolatitude and water depth. The latter appears to be the most influential as the faunas from onshore are more limited than those recorded from the deeper waters of the North Sea Basin and the Atlantic Margin. Even with this restricted fauna, however, it is still possible to develop a general correlation with the standard Tethyan zonation based on planktonic taxa.

List of Publications Recording the Results of Researches carried out under the Auspices of the Marine Biological Association of the United Kingdom in their Laboratory at Plymouth or on the North Sea Coast from 1886–1927

1928 ◽  
Vol 15 (3) ◽  
pp. 753-828 ◽  
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Biological Association ◽  
The North ◽  
Marine Biological Association ◽  
The United Kingdom ◽  
The North Sea ◽  
Different Parts ◽  
Sea Coast ◽  
North Sea Coast

The following list brings up to date a previous publication and has been classified, so far as practicable, according to subjects, in order that it may be useful for purposes of reference. The list does not include publications recording the results of observations made on material supplied by the Association to workers in different parts of the country, of which a considerable amount is sent out each year.

New Seismic Zoning Maps for Norway, the North Sea, and the United Kingdom

2000 ◽  
Vol 71 (6) ◽  
pp. 687-697 ◽  
Author(s):  
H. Bungum ◽  
C. D. Lindholm ◽  
A. Dahle ◽  
G. Woo ◽  
F. Nadim ◽  
...  
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Seismic Zoning ◽  
The North ◽  
The United Kingdom ◽  
The North Sea

A survey of inputs to the North Sea resulting from oil and gas developments

1987 ◽  
Vol 316 (1181) ◽  
pp. 495-509 ◽  
Keyword(s):  
United Kingdom ◽  
North Sea ◽  
Coastal Waters ◽  
Petroleum Hydrocarbons ◽  
Oil And Gas ◽  
The North ◽  
The United Kingdom ◽  
The North Sea ◽  
Offshore Oil And Gas ◽  
Offshore Oil

The annual input of petroleum hydrocarbons to the North Sea has recently been estimated to be between 100 and 170 kt and is derived from a variety of sources. Although there is uncertainty about the size of inputs from some sources, there is general agreement that the atmosphere, rivers and land run-off (including coastal sewage), and coastal oil industry activities combined with shipping, remain sources of major inputs. However, the size of annual inputs from the offshore oil and gas exploration and exploitation activities has recently increased to about 20 kt and these activities now form one of the major sources of petroleum hydrocarbons to the North Sea. This increase is almost entirely due to the use of oil-based drill-muds and the consequent discharge of drill cuttings contaminated with residual mud. At present, experience in the United Kingdom has shown that this input of fresh, unweathered oil rapidly enters otherwise uncontaminated offshore sediments, producing strictly local effects around the point-source discharges. The nature and composition of this input differs from the majority of the inputs to coastal waters and sediments, and from the diffuse atmospheric input to offshore waters. Of the 140 kt of materials other than oil discharged annually to the North Sea from oil and gas developments in the United Kingdom, 98-99% arise from drilling operations, but the vast majority of inputs from this source are biologically inert or derivatives of natural products. Surveys indicate that, of the remaining materials, less than 50 t of the more toxic products (i.e. those with a 96 h LC 50 to Crangon crangon of less than 1 part/10 6 ) are discharged into United Kingdom waters annually. The largely uncontaminated offshore North Sea waters and sediments remain little affected by offshore oil and gas developments, but if these activities enter already contaminated estuarine and coastal waters, the contamination and effects from this source will be harder to distinguish.

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