Tertiary flood basalts outcrop extensively in
Measurements have been made of the natural remanent magnetisation of Lower Tertiary basalts from Kangerdlugssuaq on the Blosseville Kyst of central East Greenland. The samples were taken from the base of a 9 km sequence of flows and are associated with fossüiferous marine sediments of uppermost Pala...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.579.3134 2023-05-15T15:45:00+02:00 Tertiary flood basalts outcrop extensively in Angela M. Faller The Pennsylvania State University CiteSeerX Archives 1975 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.579.3134 http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.579.3134 http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf text 1975 ftciteseerx 2016-01-08T12:54:20Z Measurements have been made of the natural remanent magnetisation of Lower Tertiary basalts from Kangerdlugssuaq on the Blosseville Kyst of central East Greenland. The samples were taken from the base of a 9 km sequence of flows and are associated with fossüiferous marine sediments of uppermost Palaeocene age. The reversed polarity, mean stable rema-nence direction (D = 159°, I =-63°, 095 = 9°), and corresponding palaeomagnetic pole position (185 ° E, 63 ° N), are in close agreement with those found by previous workers who sampled higher parts of the basalt pile. The implications concerning the age of the opening of the North-east Atlantic and the geomagnetic polarity time scale are discussed. Text Blosseville kyst East Greenland Greenland North East Atlantic Unknown Blosseville Kyst ENVELOPE(-26.417,-26.417,68.750,68.750) Greenland |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
Measurements have been made of the natural remanent magnetisation of Lower Tertiary basalts from Kangerdlugssuaq on the Blosseville Kyst of central East Greenland. The samples were taken from the base of a 9 km sequence of flows and are associated with fossüiferous marine sediments of uppermost Palaeocene age. The reversed polarity, mean stable rema-nence direction (D = 159°, I =-63°, 095 = 9°), and corresponding palaeomagnetic pole position (185 ° E, 63 ° N), are in close agreement with those found by previous workers who sampled higher parts of the basalt pile. The implications concerning the age of the opening of the North-east Atlantic and the geomagnetic polarity time scale are discussed. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Angela M. Faller |
spellingShingle |
Angela M. Faller Tertiary flood basalts outcrop extensively in |
author_facet |
Angela M. Faller |
author_sort |
Angela M. Faller |
title |
Tertiary flood basalts outcrop extensively in |
title_short |
Tertiary flood basalts outcrop extensively in |
title_full |
Tertiary flood basalts outcrop extensively in |
title_fullStr |
Tertiary flood basalts outcrop extensively in |
title_full_unstemmed |
Tertiary flood basalts outcrop extensively in |
title_sort |
tertiary flood basalts outcrop extensively in |
publishDate |
1975 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.579.3134 http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf |
long_lat |
ENVELOPE(-26.417,-26.417,68.750,68.750) |
geographic |
Blosseville Kyst Greenland |
geographic_facet |
Blosseville Kyst Greenland |
genre |
Blosseville kyst East Greenland Greenland North East Atlantic |
genre_facet |
Blosseville kyst East Greenland Greenland North East Atlantic |
op_source |
http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.579.3134 http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766379369652027392 |