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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Main Author: Angela M. Faller
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1975
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.579.3134
http://2dgf.dk/xpdf/bull24-03-04-173-178.pdf
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spelling 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
institution Open Polar
collection Unknown
op_collection_id 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.
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