Ocean Drilling Program Scientific Results Volume 104
ABSTRACT Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Vdring Plateau, eastern Norwegian Sea. The ice-rafted associations contain frequent Inoceramus (Bivalvia) prisms and rare occurrences of both benthic and plankt...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1069.3883 2023-05-15T16:27:50+02:00 Ocean Drilling Program Scientific Results Volume 104 O Eldholm J Thiede E Taylor The Pennsylvania State University CiteSeerX Archives 1989 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1069.3883 http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1069.3883 http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf text 1989 ftciteseerx 2020-04-26T00:17:25Z ABSTRACT Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Vdring Plateau, eastern Norwegian Sea. The ice-rafted associations contain frequent Inoceramus (Bivalvia) prisms and rare occurrences of both benthic and planktonic foraminifers of Miocene, Oligocene, and Maastrichtian to Campanian age. As source areas, shallow outcrops on the Norwegian Continental Shelf as well as the Greenland Shelf and the North and Baltic Seas have to be considered. Text Greenland Norwegian Sea Unknown Greenland Norwegian Sea |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
ABSTRACT Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Vdring Plateau, eastern Norwegian Sea. The ice-rafted associations contain frequent Inoceramus (Bivalvia) prisms and rare occurrences of both benthic and planktonic foraminifers of Miocene, Oligocene, and Maastrichtian to Campanian age. As source areas, shallow outcrops on the Norwegian Continental Shelf as well as the Greenland Shelf and the North and Baltic Seas have to be considered. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
O Eldholm J Thiede E Taylor |
spellingShingle |
O Eldholm J Thiede E Taylor Ocean Drilling Program Scientific Results Volume 104 |
author_facet |
O Eldholm J Thiede E Taylor |
author_sort |
O Eldholm |
title |
Ocean Drilling Program Scientific Results Volume 104 |
title_short |
Ocean Drilling Program Scientific Results Volume 104 |
title_full |
Ocean Drilling Program Scientific Results Volume 104 |
title_fullStr |
Ocean Drilling Program Scientific Results Volume 104 |
title_full_unstemmed |
Ocean Drilling Program Scientific Results Volume 104 |
title_sort |
ocean drilling program scientific results volume 104 |
publishDate |
1989 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1069.3883 http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf |
geographic |
Greenland Norwegian Sea |
geographic_facet |
Greenland Norwegian Sea |
genre |
Greenland Norwegian Sea |
genre_facet |
Greenland Norwegian Sea |
op_source |
http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1069.3883 http://www-odp.tamu.edu/publications/104_SR/VOLUME/CHAPTERS/sr104_36.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766017387258183680 |