Thanet 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.
... and magnetically interpolated dates appear to be notably discordant. The Thanet Formation, England (type Thanetian), and anomalies 25 and 26 The Thanet magnetozone (Townsend & Hailwood 1985; Fig. 4) occurs in the lower half of the Thanet Formation at Pegwell Bay, Kent, dated (where calcareous) as NP8. Aubry (1983...
Series: Geological Society, London, Special Reports
Published: 01 January 2016
DOI: 10.1144/SR27.14
EISBN: 9781862397071
.... 118 ). The Thanet Formation at Dedham Mill and Flatford (south Suffolk) is, however, included in the ‘London Basin’ section for similar reasons. The Tertiary and early Quaternary of this area comprise two packages separated by a major unconformity. Mid-Paleocene-Early Eocene deposits, dominantly mid...
Journal Article
Published: 01 June 2003
Micropaleontology (2003) 49 (Suppl_1): 179–212.
... to the time span between the top of the Thanet Sands (= top of the Thanetian Stage in England) and the base of the Ieper Clay (= base of the Ypresian Stage in Belgium). The time span between the two stages is ~2.2 my, between ~56.6 Ma (estimated age of the top of the Thanet Sands, within Chron C25r...
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Journal Article
Published: 01 September 2006
Geological Magazine (2006) 143 (5): 561–608.
... of the Cretaceous Anglo-Paris Basin. Cliff sections in east Kent near Folkestone and Dover (Fig. 1 ; UK national grid reference TR 26153830–38014767; N 51°05′58″ E 01°13′43′–N 51°10′43″E 01°24′14″), and on the Isle of Thanet between Ramsgate and Margate (TR 3668 6408–3835 7162; N 51°19′36″E 01°23′45″–N 51°23′37″E...
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Series: SEPM Concepts in Sedimentology and Paleontology
Published: 01 January 2021
DOI: 10.2110/sepmcsp.14.141
EISBN: 978-1-56576-377-7
... et al. (2010, fig. 10) who showed the Lowest Common Occurrence of the species slightly above the Chron C27n/C26r magnetozonal boundary in the Blaja section (Bulgaria). These are the oldest levels from which B. elegans has been reported. However, these two reports are questionable. The single...
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