The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution
The separation of Northeast Greenland and Svalbard is the result of large-scale strike slip movements during Cenozoic times. Geological evidence for these movements can be found onshore both on North Greenland and Svalbard. However, the role of the submarine Yermak Plateau (YP) in this process is un...
Published in: | Geophysical Journal International |
---|---|
Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
2011
|
Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/187/3/1334 https://doi.org/10.1111/j.1365-246X.2011.05197.x |
id |
fthighwire:oai:open-archive.highwire.org:gji:187/3/1334 |
---|---|
record_format |
openpolar |
spelling |
fthighwire:oai:open-archive.highwire.org:gji:187/3/1334 2023-05-15T14:59:56+02:00 The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution Geissler, W. H. Jokat, W. Brekke, H. 2011-12-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/187/3/1334 https://doi.org/10.1111/j.1365-246X.2011.05197.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/187/3/1334 http://dx.doi.org/10.1111/j.1365-246X.2011.05197.x Copyright (C) 2011, Oxford University Press Marine geosciences and applied geophysics TEXT 2011 fthighwire https://doi.org/10.1111/j.1365-246X.2011.05197.x 2016-11-16T19:08:26Z The separation of Northeast Greenland and Svalbard is the result of large-scale strike slip movements during Cenozoic times. Geological evidence for these movements can be found onshore both on North Greenland and Svalbard. However, the role of the submarine Yermak Plateau (YP) in this process is unclear. The compilation of available multichannel reflection and wide-angle seismic data give new insights into the sedimentary and crustal structure and evolution of the plateau. The flat surface of the present-day plateau is a quite young feature. Up to 2 km of Cenozoic sediments cover a rough basement, which show similarities to the rough topography and strike of geological structures of Spitsbergen Island. In some basins more than 4 km of sedimentary rocks could be mapped. The most pronounced structure is the Sverdrup Bank, which appears to be part of a larger crustal block. P -wave velocities of about 4.5 km s-1 derived from sonobuoy data indicate that its uppermost part is most probably composed of sedimentary or volcanic rocks. We have made a correlation of previously defined seismic units across the YP to outline the history of sediment deposition in the area. The existing graben structures on the plateau might have provided early shallow pathways for water exchange between the Arctic and the Atlantic Oceans. A chaotic sedimentary apron east of the Sverdrup Bank and bright reflections near the Mosby Seamount interpreted as magmatic sills suggest tectonic and magmatic events during the Miocene. Text Arctic Arctic Ocean Greenland North Greenland Svalbard Yermak plateau Spitsbergen HighWire Press (Stanford University) Arctic Arctic Ocean Svalbard Greenland Yermak Plateau ENVELOPE(5.000,5.000,81.250,81.250) Geophysical Journal International 187 3 1334 1362 |
institution |
Open Polar |
collection |
HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
Marine geosciences and applied geophysics |
spellingShingle |
Marine geosciences and applied geophysics Geissler, W. H. Jokat, W. Brekke, H. The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
topic_facet |
Marine geosciences and applied geophysics |
description |
The separation of Northeast Greenland and Svalbard is the result of large-scale strike slip movements during Cenozoic times. Geological evidence for these movements can be found onshore both on North Greenland and Svalbard. However, the role of the submarine Yermak Plateau (YP) in this process is unclear. The compilation of available multichannel reflection and wide-angle seismic data give new insights into the sedimentary and crustal structure and evolution of the plateau. The flat surface of the present-day plateau is a quite young feature. Up to 2 km of Cenozoic sediments cover a rough basement, which show similarities to the rough topography and strike of geological structures of Spitsbergen Island. In some basins more than 4 km of sedimentary rocks could be mapped. The most pronounced structure is the Sverdrup Bank, which appears to be part of a larger crustal block. P -wave velocities of about 4.5 km s-1 derived from sonobuoy data indicate that its uppermost part is most probably composed of sedimentary or volcanic rocks. We have made a correlation of previously defined seismic units across the YP to outline the history of sediment deposition in the area. The existing graben structures on the plateau might have provided early shallow pathways for water exchange between the Arctic and the Atlantic Oceans. A chaotic sedimentary apron east of the Sverdrup Bank and bright reflections near the Mosby Seamount interpreted as magmatic sills suggest tectonic and magmatic events during the Miocene. |
format |
Text |
author |
Geissler, W. H. Jokat, W. Brekke, H. |
author_facet |
Geissler, W. H. Jokat, W. Brekke, H. |
author_sort |
Geissler, W. H. |
title |
The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
title_short |
The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
title_full |
The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
title_fullStr |
The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
title_full_unstemmed |
The Yermak Plateau in the Arctic Ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
title_sort |
yermak plateau in the arctic ocean in the light of reflection seismic data-implication for its tectonic and sedimentary evolution |
publisher |
Oxford University Press |
publishDate |
2011 |
url |
http://gji.oxfordjournals.org/cgi/content/short/187/3/1334 https://doi.org/10.1111/j.1365-246X.2011.05197.x |
long_lat |
ENVELOPE(5.000,5.000,81.250,81.250) |
geographic |
Arctic Arctic Ocean Svalbard Greenland Yermak Plateau |
geographic_facet |
Arctic Arctic Ocean Svalbard Greenland Yermak Plateau |
genre |
Arctic Arctic Ocean Greenland North Greenland Svalbard Yermak plateau Spitsbergen |
genre_facet |
Arctic Arctic Ocean Greenland North Greenland Svalbard Yermak plateau Spitsbergen |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/187/3/1334 http://dx.doi.org/10.1111/j.1365-246X.2011.05197.x |
op_rights |
Copyright (C) 2011, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.2011.05197.x |
container_title |
Geophysical Journal International |
container_volume |
187 |
container_issue |
3 |
container_start_page |
1334 |
op_container_end_page |
1362 |
_version_ |
1766332056141299712 |