File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: The 'Oldhaven magnetozone' in East Anglia: A revised interpretation

TitleThe 'Oldhaven magnetozone' in East Anglia: A revised interpretation
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. 195-203 How to Cite?
AbstractA palaeomagnetic study has been carried out on the type Harwich Formation and basal London Clay Formation in the Ispwich area of East Anglia. Both units were deposited during the middle part of geomagnetic Chron C24r. The normal polarity magnetization previously identified in the upper part of the Harwich Formation at Wrabness (Townsend & Hailwood 1985, Journal of the Geological Society; London, 142, 1-27), and called the 'Oldhaven magnetozone' by these author, is now regarded as a recent overprint. The new information is critical in linking the Paleocene-Eocene boundary to NW Europe where the internationally recognized early Eocene Ypresian stage stratotype is defined.
Persistent Identifierhttp://hdl.handle.net/10722/151261
ISSN
2015 SCImago Journal Rankings: 0.747
References

 

DC FieldValueLanguage
dc.contributor.authorAli, JRen_US
dc.contributor.authorHailwood, EAen_US
dc.contributor.authorKing, Cen_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. 195-203en_US
dc.identifier.issn0305-8719en_US
dc.identifier.urihttp://hdl.handle.net/10722/151261-
dc.description.abstractA palaeomagnetic study has been carried out on the type Harwich Formation and basal London Clay Formation in the Ispwich area of East Anglia. Both units were deposited during the middle part of geomagnetic Chron C24r. The normal polarity magnetization previously identified in the upper part of the Harwich Formation at Wrabness (Townsend & Hailwood 1985, Journal of the Geological Society; London, 142, 1-27), and called the 'Oldhaven magnetozone' by these author, is now regarded as a recent overprint. The new information is critical in linking the Paleocene-Eocene boundary to NW Europe where the internationally recognized early Eocene Ypresian stage stratotype is defined.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.titleThe 'Oldhaven magnetozone' in East Anglia: A revised interpretationen_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.1996.101.01.12en_US
dc.identifier.scopuseid_2-s2.0-5244311328en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-5244311328&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume101en_US
dc.identifier.spage195en_US
dc.identifier.epage203en_US
dc.publisher.placeUnited Kingdomen_US
dc.identifier.scopusauthoridAli, JR=7102266465en_US
dc.identifier.scopusauthoridHailwood, EA=7004220927en_US
dc.identifier.scopusauthoridKing, C=7401525600en_US

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats