Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report
ABSTRACT: Palaeomagnetic investigation of the Upper Carboniferous clastic Hyrnefjellet Formation from opposite limbs of the Hyrnefjellet Anticline in southern Spitsbergen (Sval− bard Archipelago) uncovered two components of NRM. Direction C1 (D = 224.6°; I = –27.9°; = 22.40; 95 % = 5.6°) is of prefo...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.600.4828 2023-05-15T15:08:39+02:00 Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report Krzysztof Michalski Marek Lewandowski The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.4828 http://www.polar.pan.pl/ppr25/ppr25-169.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.4828 http://www.polar.pan.pl/ppr25/ppr25-169.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.polar.pan.pl/ppr25/ppr25-169.pdf Key words Arctic Spitsbergen Palaeozoic palaeomagnetism palaeogeography tectonics text 2004 ftciteseerx 2016-01-08T14:01:05Z ABSTRACT: Palaeomagnetic investigation of the Upper Carboniferous clastic Hyrnefjellet Formation from opposite limbs of the Hyrnefjellet Anticline in southern Spitsbergen (Sval− bard Archipelago) uncovered two components of NRM. Direction C1 (D = 224.6°; I = –27.9°; = 22.40; 95 % = 5.6°) is of prefolding origin and most probably of near−primary origin. High Tb spectra above 575°C indicate hematite as the carrier of C1. Acquisition of the C1 component may be related to an early diagenetic crystallization of hematite, not excluding a detrital origin of the NRM. A paleopole calculated for the C1 component ( = 23.3°N; = 147.7°E) falls into the Late Devonian–Early Carboniferous sector of APWP for Baltica. This result suggests that Svalbard remained in the present day orientation with respect to Baltica since the Carboniferous time. A second component with intermediate unblocking temperatures, determined in the Hyrnefjellet Formation deposits, is labelled C2. Its mean ori− entation for in situ position is D = 11.2°; I = 69.2 ° ( = 44.05; 95 % = 6.3°), thus being similar to Late Mesozoic directions for Baltica. After 100 % tectonic correction for tilting of anticline limbs and axis, the C2 component orientation is D = 265.7°; I = 59.7°, thus being distant from any directions for Baltica. Detailed analysis suggest that the C2 component is most probably of synfolding origin, and it was formed during the Tertiary Alpine Tectonic Event. Text Arctic Hornsund Svalbard Spitsbergen Unknown Arctic Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Hyrnefjellet ENVELOPE(16.214,16.214,77.033,77.033) Svalbard Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Key words Arctic Spitsbergen Palaeozoic palaeomagnetism palaeogeography tectonics |
spellingShingle |
Key words Arctic Spitsbergen Palaeozoic palaeomagnetism palaeogeography tectonics Krzysztof Michalski Marek Lewandowski Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
topic_facet |
Key words Arctic Spitsbergen Palaeozoic palaeomagnetism palaeogeography tectonics |
description |
ABSTRACT: Palaeomagnetic investigation of the Upper Carboniferous clastic Hyrnefjellet Formation from opposite limbs of the Hyrnefjellet Anticline in southern Spitsbergen (Sval− bard Archipelago) uncovered two components of NRM. Direction C1 (D = 224.6°; I = –27.9°; = 22.40; 95 % = 5.6°) is of prefolding origin and most probably of near−primary origin. High Tb spectra above 575°C indicate hematite as the carrier of C1. Acquisition of the C1 component may be related to an early diagenetic crystallization of hematite, not excluding a detrital origin of the NRM. A paleopole calculated for the C1 component ( = 23.3°N; = 147.7°E) falls into the Late Devonian–Early Carboniferous sector of APWP for Baltica. This result suggests that Svalbard remained in the present day orientation with respect to Baltica since the Carboniferous time. A second component with intermediate unblocking temperatures, determined in the Hyrnefjellet Formation deposits, is labelled C2. Its mean ori− entation for in situ position is D = 11.2°; I = 69.2 ° ( = 44.05; 95 % = 6.3°), thus being similar to Late Mesozoic directions for Baltica. After 100 % tectonic correction for tilting of anticline limbs and axis, the C2 component orientation is D = 265.7°; I = 59.7°, thus being distant from any directions for Baltica. Detailed analysis suggest that the C2 component is most probably of synfolding origin, and it was formed during the Tertiary Alpine Tectonic Event. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Krzysztof Michalski Marek Lewandowski |
author_facet |
Krzysztof Michalski Marek Lewandowski |
author_sort |
Krzysztof Michalski |
title |
Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
title_short |
Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
title_full |
Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
title_fullStr |
Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
title_full_unstemmed |
Palaeomagnetic results from the Middle Carboniferous rocks of the Hornsund region, southern Spitsbergen: preliminary report |
title_sort |
palaeomagnetic results from the middle carboniferous rocks of the hornsund region, southern spitsbergen: preliminary report |
publishDate |
2004 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.4828 http://www.polar.pan.pl/ppr25/ppr25-169.pdf |
long_lat |
ENVELOPE(15.865,15.865,76.979,76.979) ENVELOPE(16.214,16.214,77.033,77.033) ENVELOPE(-54.065,-54.065,49.700,49.700) |
geographic |
Arctic Hornsund Hyrnefjellet Svalbard Tilting |
geographic_facet |
Arctic Hornsund Hyrnefjellet Svalbard Tilting |
genre |
Arctic Hornsund Svalbard Spitsbergen |
genre_facet |
Arctic Hornsund Svalbard Spitsbergen |
op_source |
http://www.polar.pan.pl/ppr25/ppr25-169.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.4828 http://www.polar.pan.pl/ppr25/ppr25-169.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766339974643318784 |