On the Origin of the Dogger Bank, in the North Sea
- 1 February 1959
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 96 (1) , 33-44
- https://doi.org/10.1017/s0016756800059197
Abstract
A reversed seismic refraction station and some cores taken on the Dogger Bank, in the North Sea, are described. The absence of compacted sediments within the bank and the finding of only glacial or post-glacial sediments at its surface strongly suggest that the bank is a large moraine.Keywords
This publication has 13 references indexed in Scilit:
- Velocity of Compressional Waves for a Stratigraphic Profile of Chalk at Flamborough, YorkshireNature, 1957
- The Pleistocene Epoch in EnglandQuarterly Journal of the Geological Society, 1955
- Survey of Two Drowned River Valleys in DevonGeological Magazine, 1955
- Shell accumulation in underwater sediments and their relation to the thickness of the traction zone; discussionJournal of Sedimentary Research, 1954
- Seismic prospecting in the English Channel and its geological interpretationQuarterly Journal of the Geological Society, 1953
- SEISMIC VELOCITY AS A FUNCTION OF DEPTH AND GEOLOGIC TIMEGeophysics, 1951
- Seismic experiments on the North German explosions, 1946 to 1947Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1949
- Geophysical explorationPublished by Biodiversity Heritage Library ,1946
- Seismic investigations on the Palaeozoic floor of east EnglandPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1940
- Shelly Clay Dredged from the Dogger BankQuarterly Journal of the Geological Society, 1912