Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ...
The Mississippian to Eocene Sverdrup Basin in the Canadian Arctic has long been considered to have originated as a rift following the collapse of the Devonian to Mississippian Ellesmerian Orogen. From latest Pennsylvanian to Middle Permian time, several tectonic events were accompanied by outpouring...
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Online Access: | https://dx.doi.org/10.11575/prism/32656 https://prism.ucalgary.ca/handle/1880/107474 |
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ftdatacite:10.11575/prism/32656 2023-11-05T03:38:50+01:00 Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... Alonso Torres, Daniel 2018 https://dx.doi.org/10.11575/prism/32656 https://prism.ucalgary.ca/handle/1880/107474 en eng Graduate Studies University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Permian Sverdrup Basin Tectonics Geochronology Basin inversion Back arc Geology FOS Earth and related environmental sciences article master thesis CreativeWork Other 2018 ftdatacite https://doi.org/10.11575/prism/32656 2023-10-09T10:53:34Z The Mississippian to Eocene Sverdrup Basin in the Canadian Arctic has long been considered to have originated as a rift following the collapse of the Devonian to Mississippian Ellesmerian Orogen. From latest Pennsylvanian to Middle Permian time, several tectonic events were accompanied by outpouring of volcanic material and the addition of a northern sediment source, presently lying beneath the Arctic Ocean. This thesis encompasses geochronological, stratigraphic and structural analyses with a focus on Pennsylvanian to Lower Triassic strata and deformational events on the northern portion of the Sverdrup Basin. Northerly-sourced sediments contain a syndepositional zircon sub-population, deposited in an area that experienced multiple Pennsylvanian to Triassic uplift and deformation pulses, providing evidence for the existence of a magmatically and tectonically active margin to the north. In contrast to the passive margin setting traditionally assumed for northern Laurentia, these results require a ... Master Thesis Arctic Arctic Ocean Axel Heiberg Island sverdrup basin DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Permian Sverdrup Basin Tectonics Geochronology Basin inversion Back arc Geology FOS Earth and related environmental sciences |
spellingShingle |
Permian Sverdrup Basin Tectonics Geochronology Basin inversion Back arc Geology FOS Earth and related environmental sciences Alonso Torres, Daniel Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
topic_facet |
Permian Sverdrup Basin Tectonics Geochronology Basin inversion Back arc Geology FOS Earth and related environmental sciences |
description |
The Mississippian to Eocene Sverdrup Basin in the Canadian Arctic has long been considered to have originated as a rift following the collapse of the Devonian to Mississippian Ellesmerian Orogen. From latest Pennsylvanian to Middle Permian time, several tectonic events were accompanied by outpouring of volcanic material and the addition of a northern sediment source, presently lying beneath the Arctic Ocean. This thesis encompasses geochronological, stratigraphic and structural analyses with a focus on Pennsylvanian to Lower Triassic strata and deformational events on the northern portion of the Sverdrup Basin. Northerly-sourced sediments contain a syndepositional zircon sub-population, deposited in an area that experienced multiple Pennsylvanian to Triassic uplift and deformation pulses, providing evidence for the existence of a magmatically and tectonically active margin to the north. In contrast to the passive margin setting traditionally assumed for northern Laurentia, these results require a ... |
format |
Master Thesis |
author |
Alonso Torres, Daniel |
author_facet |
Alonso Torres, Daniel |
author_sort |
Alonso Torres, Daniel |
title |
Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
title_short |
Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
title_full |
Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
title_fullStr |
Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
title_full_unstemmed |
Permian tectonism in the Sverdrup Basin, Axel Heiberg Island, Arctic Canada ... |
title_sort |
permian tectonism in the sverdrup basin, axel heiberg island, arctic canada ... |
publisher |
Graduate Studies |
publishDate |
2018 |
url |
https://dx.doi.org/10.11575/prism/32656 https://prism.ucalgary.ca/handle/1880/107474 |
genre |
Arctic Arctic Ocean Axel Heiberg Island sverdrup basin |
genre_facet |
Arctic Arctic Ocean Axel Heiberg Island sverdrup basin |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/prism/32656 |
_version_ |
1781694591625330688 |