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Article: Recognition of Chron C25n in the Upper Paleocene Upnor Formation of the London Basin, UK
Title | Recognition of Chron C25n in the Upper Paleocene Upnor Formation of the London Basin, UK |
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Authors | |
Issue Date | 1996 |
Citation | Correlation Of The Early Paleogene In Northwest Europe, 1996, p. 185-193 How to Cite? |
Abstract | Lithostratigraphic 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 Identifier | http://hdl.handle.net/10722/150984 |
DC Field | Value | Language |
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dc.contributor.author | Ellison, RA | en_US |
dc.contributor.author | Ali, JR | en_US |
dc.contributor.author | Hine, NM | en_US |
dc.contributor.author | Jolley, DW | en_US |
dc.date.accessioned | 2012-06-26T06:15:29Z | - |
dc.date.available | 2012-06-26T06:15:29Z | - |
dc.date.issued | 1996 | en_US |
dc.identifier.citation | Correlation Of The Early Paleogene In Northwest Europe, 1996, p. 185-193 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/150984 | - |
dc.description.abstract | Lithostratigraphic 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 | en_US |
dc.language | eng | en_US |
dc.relation.ispartof | Correlation of the early Paleogene in northwest Europe | en_US |
dc.title | Recognition of Chron C25n in the Upper Paleocene Upnor Formation of the London Basin, UK | en_US |
dc.type | Article | en_US |
dc.identifier.email | Ali, JR:jrali@hku.hk | en_US |
dc.identifier.authority | Ali, JR=rp00659 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.scopus | eid_2-s2.0-0029774161 | en_US |
dc.identifier.hkuros | 23031 | - |
dc.identifier.spage | 185 | en_US |
dc.identifier.epage | 193 | en_US |
dc.identifier.scopusauthorid | Ellison, RA=7102803984 | en_US |
dc.identifier.scopusauthorid | Ali, JR=7102266465 | en_US |
dc.identifier.scopusauthorid | Hine, NM=6603933356 | en_US |
dc.identifier.scopusauthorid | Jolley, DW=24316966400 | en_US |