Comment on: Middle and Late Weichselian (Devensian) glaciation history of south-western Norway, North Sea and eastern UK by H.P. Sejrup, A. Nygård, A.M. Hall, and H. Haflidason

2009 ◽  
Vol 28 (19-20) ◽  
pp. 2017
Author(s):  
J.D. Peacock
Keyword(s):  
North Sea ◽  
Western Norway ◽  
History Of ◽  
Late Weichselian

Middle and Late Weichselian (Devensian) glaciation history of south-western Norway, North Sea and eastern UK

2009 ◽  
Vol 28 (3-4) ◽  
pp. 370-380 ◽  
Author(s):  
H.P. Sejrup ◽  
A. Nygård ◽  
A.M. Hall ◽  
H. Haflidason
Keyword(s):  
North Sea ◽  
Western Norway ◽  
History Of ◽  
Late Weichselian

Late Weichselian glaciation history of the northern North Sea

Boreas ◽  
2008 ◽  
Vol 23 (1) ◽  
pp. 1-13 ◽  
Author(s):  
HANS PETTER SEJRUP ◽  
HAFLIDI HAFLIDASON ◽  
INGE AARSETH ◽  
EDWARD KING ◽  
CARL FREDRIK FORSBERG ◽  
...  
Keyword(s):  
North Sea ◽  
History Of ◽  
Late Weichselian ◽  
Northern North Sea ◽  
Weichselian Glaciation

A Case History of Casing Directional Drilling in the Norwegian Sector of the North Sea

2008 ◽  
Author(s):  
Kevin Arthur Bourassa ◽  
Tove Husby ◽  
Rick Deuane Watts ◽  
Dale Oveson ◽  
Tommy M. Warren ◽  
...  
Keyword(s):  
North Sea ◽  
Case History ◽  
Directional Drilling ◽  
The North ◽  
History Of ◽  
The North Sea

The history and future of the North Sea benthos

1978 ◽  
Vol 76 (1-3) ◽  
pp. 193-200
Author(s):  
P. E. P. Norton
Keyword(s):  
North Sea ◽  
Bottom Type ◽  
The North ◽  
Late Tertiary ◽  
Long Term Changes ◽  
History Of ◽  
The North Sea ◽  
Temperature Depth

SynopsisThis is a brief review intended to supply bases for prediction of future changes in the North Sea Benthos. It surveys long-term changes which are affecting the benthos. Any prediction must take into account change in temperature, depth, bottom type, tidal patterns, current patterns and zoogeography of the sea and the history of these is briefly touched on from late Tertiary times up to the present. From a prediction of changes in the benthos, certain information concerning the pelagic and planktonic biota could also be derived.

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