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Article: Magnetostratigraphic correlation of paleogene sequences from northwest Europe and North America

TitleMagnetostratigraphic correlation of paleogene sequences from northwest Europe and North America
Authors
Issue Date1999
PublisherGeological Society of America. The Journal's web site is located at http://www.geosociety.org/pubs/
Citation
Geology, 1999, v. 27 n. 5, p. 451-454 How to Cite?
AbstractUsing all available biostratigraphic information and our own extensive magnetostratigraphic database, we have attempted to assess the synchronicity of depositional cycles recorded in the Paleogene epicontinental deposits on both sides of the North Atlantic as stage two of a ; four-stage global assessment of the eustatic sea-level model. Our conclusion is that the depositional histories of the U.S. Gulf of Mexico-Atlantic coastal plain and the North Sea basin show many similarities, on a variety of time scales, over the interval 60-46 Ma. Considering the tectonic imprint of the northeast Atlantic opening on the North Sea basin sea-level record for part of this time, it must give some weight to the claim that eustasy is the dominant mechanism controlling deposition on passive continental margins.
Persistent Identifierhttp://hdl.handle.net/10722/73042
ISSN
2015 Impact Factor: 4.548
2015 SCImago Journal Rankings: 3.278
References

 

DC FieldValueLanguage
dc.contributor.authorRhodes, GMen_HK
dc.contributor.authorAli, JRen_HK
dc.contributor.authorHailwood, EAen_HK
dc.contributor.authorKing, Cen_HK
dc.contributor.authorGibson, TGen_HK
dc.date.accessioned2010-09-06T06:47:30Z-
dc.date.available2010-09-06T06:47:30Z-
dc.date.issued1999en_HK
dc.identifier.citationGeology, 1999, v. 27 n. 5, p. 451-454en_HK
dc.identifier.issn0091-7613en_HK
dc.identifier.urihttp://hdl.handle.net/10722/73042-
dc.description.abstractUsing all available biostratigraphic information and our own extensive magnetostratigraphic database, we have attempted to assess the synchronicity of depositional cycles recorded in the Paleogene epicontinental deposits on both sides of the North Atlantic as stage two of a ; four-stage global assessment of the eustatic sea-level model. Our conclusion is that the depositional histories of the U.S. Gulf of Mexico-Atlantic coastal plain and the North Sea basin show many similarities, on a variety of time scales, over the interval 60-46 Ma. Considering the tectonic imprint of the northeast Atlantic opening on the North Sea basin sea-level record for part of this time, it must give some weight to the claim that eustasy is the dominant mechanism controlling deposition on passive continental margins.en_HK
dc.languageengen_HK
dc.publisherGeological Society of America. The Journal's web site is located at http://www.geosociety.org/pubs/en_HK
dc.relation.ispartofGeologyen_HK
dc.titleMagnetostratigraphic correlation of paleogene sequences from northwest Europe and North Americaen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0091-7613&volume=27&spage=451&epage=454&date=1999&atitle=Magnetostratigraphic+correlation+of+Paleogene+sequences+from+northwest+Europe+and+North+Americaen_HK
dc.identifier.emailAli, JR:jrali@hku.hken_HK
dc.identifier.authorityAli, JR=rp00659en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-0032876993en_HK
dc.identifier.hkuros46984en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0032876993&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume27en_HK
dc.identifier.issue5en_HK
dc.identifier.spage451en_HK
dc.identifier.epage454en_HK
dc.publisher.placeUnited Statesen_HK
dc.identifier.scopusauthoridRhodes, GM=7101795975en_HK
dc.identifier.scopusauthoridAli, JR=7102266465en_HK
dc.identifier.scopusauthoridHailwood, EA=7004220927en_HK
dc.identifier.scopusauthoridKing, C=7401525600en_HK
dc.identifier.scopusauthoridGibson, TG=7202694620en_HK

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