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Article: Recognition of chron C25n in the upper paleocene upnor formation of the London Basin, UK

TitleRecognition of chron C25n in the upper paleocene upnor formation of the London Basin, UK
Authors
Issue Date1996
PublisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/sp
Citation
Geological Society Special Publication, 1996, v. 101, p. 185-193 How to Cite?
AbstractLithostratigraphic studies of four borehole cores drilled through the late Paleocene Lambeth Group (Upnor, Woolwith and Reading Formations) and basal London Clay Formation of central London have been supplemented with palaeomagnetic, calcareous nannoplankton and palynological data. The Woolwich and Rending Formations and the lower London Clay Formation are reversely magnetized and were deposited during the early part of Chron C24r. The first record of both NP9 and Chron C25n, hitherto missing from the Paleogene record in southern England, has been identified in the Upnor Formation (formerly the Woolwich Bottom Bed). It provides a key reference marker for linking events associated with the Paleocene-Eocene boundary (positioned within Chron C24r) to the type area of the internationally recognized Thanetian and Ypresian Stages.
Persistent Identifierhttp://hdl.handle.net/10722/151260
ISSN
2015 SCImago Journal Rankings: 0.747
References

 

DC FieldValueLanguage
dc.contributor.authorEllison, RAen_US
dc.contributor.authorAli, JRen_US
dc.contributor.authorHine, NMen_US
dc.contributor.authorJolley, DWen_US
dc.date.accessioned2012-06-26T06:19:31Z-
dc.date.available2012-06-26T06:19:31Z-
dc.date.issued1996en_US
dc.identifier.citationGeological Society Special Publication, 1996, v. 101, p. 185-193en_US
dc.identifier.issn0305-8719en_US
dc.identifier.urihttp://hdl.handle.net/10722/151260-
dc.description.abstractLithostratigraphic studies of four borehole cores drilled through the late Paleocene Lambeth Group (Upnor, Woolwith and Reading Formations) and basal London Clay Formation of central London have been supplemented with palaeomagnetic, calcareous nannoplankton and palynological data. The Woolwich and Rending Formations and the lower London Clay Formation are reversely magnetized and were deposited during the early part of Chron C24r. The first record of both NP9 and Chron C25n, hitherto missing from the Paleogene record in southern England, has been identified in the Upnor Formation (formerly the Woolwich Bottom Bed). It provides a key reference marker for linking events associated with the Paleocene-Eocene boundary (positioned within Chron C24r) to the type area of the internationally recognized Thanetian and Ypresian Stages.en_US
dc.languageengen_US
dc.publisherGeological Society Publishing House. The Journal's web site is located at http://www.geolsoc.org.uk/spen_US
dc.relation.ispartofGeological Society Special Publicationen_US
dc.titleRecognition of chron C25n in the upper paleocene upnor formation of the London Basin, UKen_US
dc.typeArticleen_US
dc.identifier.emailAli, JR:jrali@hku.hken_US
dc.identifier.authorityAli, JR=rp00659en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.1144/GSL.SP.1996.101.01.11en_US
dc.identifier.scopuseid_2-s2.0-5244280156en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-5244280156&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume101en_US
dc.identifier.spage185en_US
dc.identifier.epage193en_US
dc.publisher.placeUnited Kingdomen_US
dc.identifier.scopusauthoridEllison, RA=7102803984en_US
dc.identifier.scopusauthoridAli, JR=7102266465en_US
dc.identifier.scopusauthoridHine, NM=6603933356en_US
dc.identifier.scopusauthoridJolley, DW=24316966400en_US

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