On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren
With evidence from planktonic foraminifera, it is shown that the Lower Selandian (which overlies the Danien in the type area) belongs to the Globorotalia angulata biozone. Since ROSENKRANTZ (1924) proposed the preliminary stage name Selandian for the glauconitic marls and clays deposited upon the Up...
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1968
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.554.4353 2023-05-15T18:00:47+02:00 On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren Hans Jørgen Hansen The Pennsylvania State University CiteSeerX Archives 1968 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.554.4353 http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.554.4353 http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf text 1968 ftciteseerx 2016-01-08T11:42:43Z With evidence from planktonic foraminifera, it is shown that the Lower Selandian (which overlies the Danien in the type area) belongs to the Globorotalia angulata biozone. Since ROSENKRANTZ (1924) proposed the preliminary stage name Selandian for the glauconitic marls and clays deposited upon the Upper Danian lime-stones and overlain by the Ypresian ash layers, much doubt has existed as to the stratigraphical age of the deposits. The lithology of the Selandian sediments was described in detail by GRY (1935). The lithological development of the Selandian sediments starts with a basal conglomerate containing a large amount of redeposited Upper Danian fossils. The conglomerate is followed by glauconitic calcareous sand which displays gradually decreasing grain size upwards. These layers are followed by the Kerteminde Marl which, in its upper part becomes non-calcareous. The clay mineralogy of the Selandian sediments was described Text Planktonic foraminifera Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
With evidence from planktonic foraminifera, it is shown that the Lower Selandian (which overlies the Danien in the type area) belongs to the Globorotalia angulata biozone. Since ROSENKRANTZ (1924) proposed the preliminary stage name Selandian for the glauconitic marls and clays deposited upon the Upper Danian lime-stones and overlain by the Ypresian ash layers, much doubt has existed as to the stratigraphical age of the deposits. The lithology of the Selandian sediments was described in detail by GRY (1935). The lithological development of the Selandian sediments starts with a basal conglomerate containing a large amount of redeposited Upper Danian fossils. The conglomerate is followed by glauconitic calcareous sand which displays gradually decreasing grain size upwards. These layers are followed by the Kerteminde Marl which, in its upper part becomes non-calcareous. The clay mineralogy of the Selandian sediments was described |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Hans Jørgen Hansen |
spellingShingle |
Hans Jørgen Hansen On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
author_facet |
Hans Jørgen Hansen |
author_sort |
Hans Jørgen Hansen |
title |
On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
title_short |
On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
title_full |
On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
title_fullStr |
On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
title_full_unstemmed |
On the biostratigraphical age of the lower Selandian of Denmark. Meddr dansk geol. Foren |
title_sort |
on the biostratigraphical age of the lower selandian of denmark. meddr dansk geol. foren |
publishDate |
1968 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.554.4353 http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.554.4353 http://2dgf.dk/xpdf/bull18-03-04-277-285.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766170026972282880 |