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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
Ellison, RAAli, JRHine, NMJolley, DW
Issue Date1996
Citation
Correlation Of The Early Paleogene In Northwest Europe, 1996, p. 185-193 How to Cite?
AbstractLithostratigraphic studies of four borehole cores drilled through the late Paleocene Lambeth Group and basal London Clay Formation of central London have been supplemented with palaeomagnetic, calcareous nannoplankton and palynological data. The Woolwich and Reading 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. It provides a key reference marker for linking events associated with the Paleocene-Eocene boundary to the type area of the internationally recognized Thanetian and Ypresian Stages. -from Authors
Persistent Identifierhttp://hdl.handle.net/10722/150984

 

DC FieldValueLanguage
dc.contributor.authorEllison, RAen_US
dc.contributor.authorAli, JRen_US
dc.contributor.authorHine, NMen_US
dc.contributor.authorJolley, DWen_US
dc.date.accessioned2012-06-26T06:15:29Z-
dc.date.available2012-06-26T06:15:29Z-
dc.date.issued1996en_US
dc.identifier.citationCorrelation Of The Early Paleogene In Northwest Europe, 1996, p. 185-193en_US
dc.identifier.urihttp://hdl.handle.net/10722/150984-
dc.description.abstractLithostratigraphic studies of four borehole cores drilled through the late Paleocene Lambeth Group and basal London Clay Formation of central London have been supplemented with palaeomagnetic, calcareous nannoplankton and palynological data. The Woolwich and Reading 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. It provides a key reference marker for linking events associated with the Paleocene-Eocene boundary to the type area of the internationally recognized Thanetian and Ypresian Stages. -from Authorsen_US
dc.languageengen_US
dc.relation.ispartofCorrelation of the early Paleogene in northwest Europeen_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.scopuseid_2-s2.0-0029774161en_US
dc.identifier.hkuros23031-
dc.identifier.spage185en_US
dc.identifier.epage193en_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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