Age of the youngest Palaeogene flood basalts in East Greenland

Intra-basaltic sediments 50 m below the top of the Paleogene lava succession at Kap Dalton, East Greenland, contain dinoflagellate cysts of late Ypresian-earliest Lutetian age, while sediments immediately above the lavas contain an assemblage of early Lutetian age. Combined with paleomagnetic result...

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Published in:Newsletters on Stratigraphy
Main Authors: Heilmann-Clausen, C., Piasecki, Stefan, Abrahamsen, Niels, Larsen, M., Stemmerik, Lars
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Kap
Online Access:https://curis.ku.dk/portal/da/publications/age-of-the-youngest-palaeogene-flood-basalts-in-east-greenland(0ad00570-a65c-11dd-b5e9-000ea68e967b).html
https://doi.org/10.1127/0078-0421/2008/0043-0055
id ftcopenhagenunip:oai:pure.atira.dk:publications/0ad00570-a65c-11dd-b5e9-000ea68e967b
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spelling ftcopenhagenunip:oai:pure.atira.dk:publications/0ad00570-a65c-11dd-b5e9-000ea68e967b 2023-06-18T03:40:25+02:00 Age of the youngest Palaeogene flood basalts in East Greenland Heilmann-Clausen, C. Piasecki, Stefan Abrahamsen, Niels Larsen, M. Stemmerik, Lars 2008 https://curis.ku.dk/portal/da/publications/age-of-the-youngest-palaeogene-flood-basalts-in-east-greenland(0ad00570-a65c-11dd-b5e9-000ea68e967b).html https://doi.org/10.1127/0078-0421/2008/0043-0055 eng eng info:eu-repo/semantics/restrictedAccess Heilmann-Clausen , C , Piasecki , S , Abrahamsen , N , Larsen , M & Stemmerik , L 2008 , ' Age of the youngest Palaeogene flood basalts in East Greenland ' , Newsletters on Stratigraphy , vol. 43 , no. 1 , pp. 55-63 . https://doi.org/10.1127/0078-0421/2008/0043-0055 /dk/atira/pure/core/keywords/TheFacultyOfScience Faculty of Science Øst Grønland Basalt geologi paleogene flood basalts East Greenland geology article 2008 ftcopenhagenunip https://doi.org/10.1127/0078-0421/2008/0043-0055 2023-06-07T23:47:41Z Intra-basaltic sediments 50 m below the top of the Paleogene lava succession at Kap Dalton, East Greenland, contain dinoflagellate cysts of late Ypresian-earliest Lutetian age, while sediments immediately above the lavas contain an assemblage of early Lutetian age. Combined with paleomagnetic results, this constrains the termination of the East Greenland Paleogene Igneous Province to the Early-Middle Eocene transition (nannoplankton chronozones NP13-NP14/earliest NP15). This is 6-8 Ma younger than according to previous biostratigraphic age assignments. The new data show that flood basalt volcanism occurred simultaneously with major intrusions occurring further to the south. This corroborates previous assumptions of an important melting event much younger than the continental break-up. Article in Journal/Newspaper East Greenland Greenland Grønland University of Copenhagen: Research Greenland Kap ENVELOPE(23.567,23.567,65.533,65.533) Kap Dalton ENVELOPE(-24.100,-24.100,69.417,69.417) Newsletters on Stratigraphy 43 1 55 63
institution Open Polar
collection University of Copenhagen: Research
op_collection_id ftcopenhagenunip
language English
topic /dk/atira/pure/core/keywords/TheFacultyOfScience
Faculty of Science
Øst Grønland
Basalt
geologi
paleogene flood basalts
East Greenland
geology
spellingShingle /dk/atira/pure/core/keywords/TheFacultyOfScience
Faculty of Science
Øst Grønland
Basalt
geologi
paleogene flood basalts
East Greenland
geology
Heilmann-Clausen, C.
Piasecki, Stefan
Abrahamsen, Niels
Larsen, M.
Stemmerik, Lars
Age of the youngest Palaeogene flood basalts in East Greenland
topic_facet /dk/atira/pure/core/keywords/TheFacultyOfScience
Faculty of Science
Øst Grønland
Basalt
geologi
paleogene flood basalts
East Greenland
geology
description Intra-basaltic sediments 50 m below the top of the Paleogene lava succession at Kap Dalton, East Greenland, contain dinoflagellate cysts of late Ypresian-earliest Lutetian age, while sediments immediately above the lavas contain an assemblage of early Lutetian age. Combined with paleomagnetic results, this constrains the termination of the East Greenland Paleogene Igneous Province to the Early-Middle Eocene transition (nannoplankton chronozones NP13-NP14/earliest NP15). This is 6-8 Ma younger than according to previous biostratigraphic age assignments. The new data show that flood basalt volcanism occurred simultaneously with major intrusions occurring further to the south. This corroborates previous assumptions of an important melting event much younger than the continental break-up.
format Article in Journal/Newspaper
author Heilmann-Clausen, C.
Piasecki, Stefan
Abrahamsen, Niels
Larsen, M.
Stemmerik, Lars
author_facet Heilmann-Clausen, C.
Piasecki, Stefan
Abrahamsen, Niels
Larsen, M.
Stemmerik, Lars
author_sort Heilmann-Clausen, C.
title Age of the youngest Palaeogene flood basalts in East Greenland
title_short Age of the youngest Palaeogene flood basalts in East Greenland
title_full Age of the youngest Palaeogene flood basalts in East Greenland
title_fullStr Age of the youngest Palaeogene flood basalts in East Greenland
title_full_unstemmed Age of the youngest Palaeogene flood basalts in East Greenland
title_sort age of the youngest palaeogene flood basalts in east greenland
publishDate 2008
url https://curis.ku.dk/portal/da/publications/age-of-the-youngest-palaeogene-flood-basalts-in-east-greenland(0ad00570-a65c-11dd-b5e9-000ea68e967b).html
https://doi.org/10.1127/0078-0421/2008/0043-0055
long_lat ENVELOPE(23.567,23.567,65.533,65.533)
ENVELOPE(-24.100,-24.100,69.417,69.417)
geographic Greenland
Kap
Kap Dalton
geographic_facet Greenland
Kap
Kap Dalton
genre East Greenland
Greenland
Grønland
genre_facet East Greenland
Greenland
Grønland
op_source Heilmann-Clausen , C , Piasecki , S , Abrahamsen , N , Larsen , M & Stemmerik , L 2008 , ' Age of the youngest Palaeogene flood basalts in East Greenland ' , Newsletters on Stratigraphy , vol. 43 , no. 1 , pp. 55-63 . https://doi.org/10.1127/0078-0421/2008/0043-0055
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1127/0078-0421/2008/0043-0055
container_title Newsletters on Stratigraphy
container_volume 43
container_issue 1
container_start_page 55
op_container_end_page 63
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