Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount
The area to the northwest of Svalbard was affected by repeated tectono-magmatic processes starting from the Cretaceous formation of the High Arctic Large Igneous Province, to Late Cretaceous/early Cenozoic birth of the Eurasian Basin towards the establishment of a full seafloor-spreading regime alon...
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ftawi:oai:epic.awi.de:45003 2024-09-15T17:51:11+00:00 Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount Geissler, Wolfram Estrada, Solveig Riefstahl, Florian O'Connor, John Spiegel, Cornelia Van den Boogard, Paul Klügel, Andreas 2017 https://epic.awi.de/id/eprint/45003/ https://hdl.handle.net/10013/epic.51664 unknown Geissler, W. orcid:0000-0001-6807-555X , Estrada, S. , Riefstahl, F. , O'Connor, J. , Spiegel, C. , Van den Boogard, P. and Klügel, A. (2017) Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount , GeoBremen 2017, Bremen, 24 September 2017 - 29 September 2017 . hdl:10013/epic.51664 EPIC3GeoBremen 2017, Bremen, 2017-09-24-2017-09-29 Conference notRev 2017 ftawi 2024-06-24T04:17:43Z The area to the northwest of Svalbard was affected by repeated tectono-magmatic processes starting from the Cretaceous formation of the High Arctic Large Igneous Province, to Late Cretaceous/early Cenozoic birth of the Eurasian Basin towards the establishment of a full seafloor-spreading regime along the Lena Trough/Fram Strait in Middle Miocene. These processes also affected the Sophia Basin located in-between the Yermak Plateau and the northern Svalbard Shelf. In 2013 a little piece of basalt could be dredged from the southern flank of the Mosby Seamount, the central landmark within the Sophia Basin. Geochemical analyses support our assumption that the rock fragment has a local origin and that it was not rafted towards the sample site by ice. The trace element composition implies that the basalt had incorporated marine sediments and also Fe-Mn crusts or nodules. According to geochronological data the basalt erupted ~13 Ma, contemporaneous to incipient seafloor spreading in the nearby Lena Trough and volcanic activity in northern Svalbard. Assuming a link of the dredged basalt with seismic indication of sediment covered lava flows and sill intrusion around Mosby Seamount, its middle Miocene age can be used to better constrain the regional seismo-stratigraphy. Conference Object Arctic Arctic Ocean Fram Strait Svalbard Yermak plateau Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The area to the northwest of Svalbard was affected by repeated tectono-magmatic processes starting from the Cretaceous formation of the High Arctic Large Igneous Province, to Late Cretaceous/early Cenozoic birth of the Eurasian Basin towards the establishment of a full seafloor-spreading regime along the Lena Trough/Fram Strait in Middle Miocene. These processes also affected the Sophia Basin located in-between the Yermak Plateau and the northern Svalbard Shelf. In 2013 a little piece of basalt could be dredged from the southern flank of the Mosby Seamount, the central landmark within the Sophia Basin. Geochemical analyses support our assumption that the rock fragment has a local origin and that it was not rafted towards the sample site by ice. The trace element composition implies that the basalt had incorporated marine sediments and also Fe-Mn crusts or nodules. According to geochronological data the basalt erupted ~13 Ma, contemporaneous to incipient seafloor spreading in the nearby Lena Trough and volcanic activity in northern Svalbard. Assuming a link of the dredged basalt with seismic indication of sediment covered lava flows and sill intrusion around Mosby Seamount, its middle Miocene age can be used to better constrain the regional seismo-stratigraphy. |
format |
Conference Object |
author |
Geissler, Wolfram Estrada, Solveig Riefstahl, Florian O'Connor, John Spiegel, Cornelia Van den Boogard, Paul Klügel, Andreas |
spellingShingle |
Geissler, Wolfram Estrada, Solveig Riefstahl, Florian O'Connor, John Spiegel, Cornelia Van den Boogard, Paul Klügel, Andreas Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
author_facet |
Geissler, Wolfram Estrada, Solveig Riefstahl, Florian O'Connor, John Spiegel, Cornelia Van den Boogard, Paul Klügel, Andreas |
author_sort |
Geissler, Wolfram |
title |
Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
title_short |
Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
title_full |
Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
title_fullStr |
Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
title_full_unstemmed |
Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount |
title_sort |
middle miocene magmatic activity in the sophia basin, arctic ocean – evidence from dredged basalt at the flanks of mosby seamount |
publishDate |
2017 |
url |
https://epic.awi.de/id/eprint/45003/ https://hdl.handle.net/10013/epic.51664 |
genre |
Arctic Arctic Ocean Fram Strait Svalbard Yermak plateau |
genre_facet |
Arctic Arctic Ocean Fram Strait Svalbard Yermak plateau |
op_source |
EPIC3GeoBremen 2017, Bremen, 2017-09-24-2017-09-29 |
op_relation |
Geissler, W. orcid:0000-0001-6807-555X , Estrada, S. , Riefstahl, F. , O'Connor, J. , Spiegel, C. , Van den Boogard, P. and Klügel, A. (2017) Middle Miocene magmatic activity in the Sophia Basin, Arctic Ocean – evidence from dredged basalt at the flanks of Mosby Seamount , GeoBremen 2017, Bremen, 24 September 2017 - 29 September 2017 . hdl:10013/epic.51664 |
_version_ |
1810293014712549376 |