Oldhaven Magnetozone

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Journal Article
Published: 01 September 1986
Journal of the Geological Society (1986) 143 (5): 729–735.
... and 24B are represented within Divisions D to B2 of the London Clay, and anomaly 26 is represented in the lower part of the Thanet beds. An additional normal polarity magnetozone within the Oldhaven beds is believed to represent a short normal polarity event between anomalies 24B and 25. Anomalies 22...
Journal Article
Published: 01 December 1985
Journal of the Geological Society (1985) 142 (6): 957–982.
.... Eight discrete normal polarity magnetozones have been identified within this dominantly reverse polarity interval. Three of these lie within the Bracklesham Group, three within the London Clay Formation, one in the Oldhaven 'Formation', and one within the lowermost part of the Thanet Formation. Assuming...
Journal Article
Published: 01 December 1985
Journal of the Geological Society (1985) 142 (6): 1179–1188.
... of NPl l [(just above the appearance of Tribrachiatus orthostylus (Lowrie et al. 1982), with confirmation from DSDP cores (see Berggren et al. 1985, pp. 192, 194 The above determinations pose a problem for the identification of the Oldhaven magnetozone, compris- ing the Oldhaven Beds and (locally...
Series: Geological Society, London, Special Reports
Published: 01 January 2016
DOI: 10.1144/SR27.14
EISBN: 9781862397071
... with a normal polarity interval in the Oldhaven Member of Kent, and designated the ‘Oldhaven magnetozone’ (Townsend & Hailwood 1985). Subsequent analysis indicated that this (and other normal polarity intervals at outcrop) are due to a secondary overprint. In unweathered outcrops and subsurface sections...