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Earnley Magnetozone

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Journal Article
Published: 01 September 1986
Journal of the Geological Society (1986) 143 (5): 729–735.
... be identified as Chron C23N. (e) The Earnley magnetozone This normal polarity event is recorded in the Earnley Division of the Bracklesham Beds exposed at Alum Bay, Whitecliff Bay nd Bracklesham Bay (Townsend & Hailwood 1985). At these latter two localities this event respectively occurs in Fisher Beds VI to IX...
Journal Article
Published: 01 December 1985
Journal of the Geological Society (1985) 142 (6): 957–982.
... of the Bracklesham Group (represented by the Wittering, Earnley, Selsey and Huntingbridge Divisions) are significantly diachronous. In relation to the absolute time planes provided by the magnetozone boundaries it is clear that the Bracklesham Group transgressive events occurred systematically earlier in the east...
Journal Article
Published: 01 December 1985
Journal of the Geological Society (1985) 142 (6): 1179–1188.
... are conceivable-the Earnley magnetozone, for example, might be a composite representing 22 and 21, with a hiatus masking the intervening reversal. Indications from DSDP cores and the Gubbio sequences on the biostratigraphic ages of anomalies 22 to 20 are ambiguous, as Berggren et al. (1985, p. 193) note...
Journal Article
Published: 01 September 1997
Journal of the Geological Society (1997) 154 (5): 897–912.
... a vermiform texture until they recrystallize (discussed below). In contrast with older Fig. 1. Location map and outline stratigraphy of the Eocene succession at WhitecliV Bay. The map shows approximate shorelines for (1) Wittering Formation, second sequence (2) Earnley Formation (3) Selsey Formation. HF...
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...