SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS

A b s t r a c t Magnetic zones of normal and reverse polarity measured in the field by means of a compass show the middle and upper lava series of the Tertiary Faroese basalts to be reversely magnetized, while in the lower lava series there are at least three magnetic zones of alternating polarity....

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Main Author: Niels Abrahamsen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.1250
http://2dgf.dk/xpdf/bull17-03-371-384.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.533.1250 2023-05-15T16:10:43+02:00 SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS Niels Abrahamsen The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.1250 http://2dgf.dk/xpdf/bull17-03-371-384.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.1250 http://2dgf.dk/xpdf/bull17-03-371-384.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull17-03-371-384.pdf text ftciteseerx 2016-01-08T10:41:59Z A b s t r a c t Magnetic zones of normal and reverse polarity measured in the field by means of a compass show the middle and upper lava series of the Tertiary Faroese basalts to be reversely magnetized, while in the lower lava series there are at least three magnetic zones of alternating polarity. Cylindrical specimens of 43 samples were studied in the laboratory, 33 of which were found to be magnetically stable, giving a mean position of the paleo-magnetic pole of 80 ° N and 159 ° E, with a 95 % cone of confidence of 9°. The paleomagnetic pole of the middle and upper lava series agrees well with Tertiary poles from Eurasia and poles from the Tertiary igneous rocks of the British Text Faroe Islands Unknown Faroe Islands
institution Open Polar
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description A b s t r a c t Magnetic zones of normal and reverse polarity measured in the field by means of a compass show the middle and upper lava series of the Tertiary Faroese basalts to be reversely magnetized, while in the lower lava series there are at least three magnetic zones of alternating polarity. Cylindrical specimens of 43 samples were studied in the laboratory, 33 of which were found to be magnetically stable, giving a mean position of the paleo-magnetic pole of 80 ° N and 159 ° E, with a 95 % cone of confidence of 9°. The paleomagnetic pole of the middle and upper lava series agrees well with Tertiary poles from Eurasia and poles from the Tertiary igneous rocks of the British
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Niels Abrahamsen
spellingShingle Niels Abrahamsen
SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
author_facet Niels Abrahamsen
author_sort Niels Abrahamsen
title SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
title_short SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
title_full SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
title_fullStr SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
title_full_unstemmed SOME PALEOMAGNETIC INVESTIGATIONS IN THE FAROE ISLANDS
title_sort some paleomagnetic investigations in the faroe islands
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.1250
http://2dgf.dk/xpdf/bull17-03-371-384.pdf
geographic Faroe Islands
geographic_facet Faroe Islands
genre Faroe Islands
genre_facet Faroe Islands
op_source http://2dgf.dk/xpdf/bull17-03-371-384.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.1250
http://2dgf.dk/xpdf/bull17-03-371-384.pdf
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