On the apparent eastward migration of the spreading ridge in Iceland
The part of the north Atlantic where Iceland is currently forming has functioned as a tectonic divide since the opening of the ocean, and has persistently featured paired spreading ridges and intervening microplates. At the time of ocean opening a ~ 100-km long, right-stepping transform fault, the F...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.493.497 2023-05-15T16:46:11+02:00 On the apparent eastward migration of the spreading ridge in Iceland G. R. Foulger The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.493.497 http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.493.497 http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf text ftciteseerx 2020-10-04T00:15:57Z The part of the north Atlantic where Iceland is currently forming has functioned as a tectonic divide since the opening of the ocean, and has persistently featured paired spreading ridges and intervening microplates. At the time of ocean opening a ~ 100-km long, right-stepping transform fault, the Faeroe transform fault (FTF), formed where the new spreading ridge crossed the Caledonian suture [Bott, 1985] (Figure 1a). Tectonic complexities subsequently rafted several continental blocks into the ocean, including Jan Mayen, the Jan Mayen microcontinent (JMM) and the Faeroe block. Text Iceland Jan Mayen North Atlantic Unknown Jan Mayen |
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ftciteseerx |
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English |
description |
The part of the north Atlantic where Iceland is currently forming has functioned as a tectonic divide since the opening of the ocean, and has persistently featured paired spreading ridges and intervening microplates. At the time of ocean opening a ~ 100-km long, right-stepping transform fault, the Faeroe transform fault (FTF), formed where the new spreading ridge crossed the Caledonian suture [Bott, 1985] (Figure 1a). Tectonic complexities subsequently rafted several continental blocks into the ocean, including Jan Mayen, the Jan Mayen microcontinent (JMM) and the Faeroe block. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
G. R. Foulger |
spellingShingle |
G. R. Foulger On the apparent eastward migration of the spreading ridge in Iceland |
author_facet |
G. R. Foulger |
author_sort |
G. R. Foulger |
title |
On the apparent eastward migration of the spreading ridge in Iceland |
title_short |
On the apparent eastward migration of the spreading ridge in Iceland |
title_full |
On the apparent eastward migration of the spreading ridge in Iceland |
title_fullStr |
On the apparent eastward migration of the spreading ridge in Iceland |
title_full_unstemmed |
On the apparent eastward migration of the spreading ridge in Iceland |
title_sort |
on the apparent eastward migration of the spreading ridge in iceland |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.493.497 http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf |
geographic |
Jan Mayen |
geographic_facet |
Jan Mayen |
genre |
Iceland Jan Mayen North Atlantic |
genre_facet |
Iceland Jan Mayen North Atlantic |
op_source |
http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.493.497 http://www.mantleplumes.org/Penrose/PenPDFAbstracts/Foulger_Gillian_abs2.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766036301736312832 |