Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay
The Canadian Shield is one of the largest exposures of Precambrian rocks on Earth. It is a mosaic of several Archean terranes that were brought together during a series of Paleoproterozoic orogens culminating in the so-called Trans-Hudson Orogen (THO), which is thought to have been similar to the Hi...
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Online Access: | https://hdl.handle.net/1983/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://research-information.bris.ac.uk/en/publications/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://doi.org/10.1130/G31396.1 |
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ftubristolcris:oai:research-information.bris.ac.uk:publications/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 2024-01-28T10:04:39+01:00 Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay Bastow, ID Thompson, D.A Wookey, J Kendall, J-M Helffrich, GR Snyder, D Eaton, D Darbyshire, F.A 2011-01 https://hdl.handle.net/1983/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://research-information.bris.ac.uk/en/publications/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://doi.org/10.1130/G31396.1 eng eng info:eu-repo/semantics/restrictedAccess Bastow , ID , Thompson , D A , Wookey , J , Kendall , J-M , Helffrich , GR , Snyder , D , Eaton , D & Darbyshire , F A 2011 , ' Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay ' , Geology , vol. 39 , pp. 91 - 94 . https://doi.org/10.1130/G31396.1 article 2011 ftubristolcris https://doi.org/10.1130/G31396.1 2024-01-04T23:32:56Z The Canadian Shield is one of the largest exposures of Precambrian rocks on Earth. It is a mosaic of several Archean terranes that were brought together during a series of Paleoproterozoic orogens culminating in the so-called Trans-Hudson Orogen (THO), which is thought to have been similar to the Himalayan orogen in scale and nature. The tectonic evolution and lithospheric subdivisions of this region are poorly understood, but new seismic networks in northern Hudson Bay provide fresh opportunity to place constraints on the Precambrian processes that formed and shaped it. We show via a study of seismic anisotropy that the lithosphere of the northern Hudson Bay region retains a strong signature of Archean-to-Paleoproterozoic tectonics. We map the boundary between the upper (Churchill) and lower (Superior) plates that collided ∼1.8 Ga and identify backazimuthdependent splitting parameters (φ, δt) on Baffin Island that indicate complex anisotropy (e.g., dipping fabric) beneath the region. Our results support the view that significant lithospheric deformation occurred during the Paleoproterozoic and that modern-day plate tectonic processes were thus in operation by at least ∼1.8 Ga. The Canadian Shield is one of the largest exposures of Precambrian rocks on Earth. It is a mosaic of several Archean terranes that were brought together during a series of Paleoproterozoic orogens culminating in the so-called Trans-Hudson Orogen (THO), which is thought to have been similar to the Himalayan orogen in scale and nature. The tectonic evolution and lithospheric subdivisions of this region are poorly understood, but new seismic networks in northern Hudson Bay provide fresh opportunity to place constraints on the Precambrian processes that formed and shaped it. We show via a study of seismic anisotropy that the lithosphere of the northern Hudson Bay region retains a strong signature of Archean-to-Paleoproterozoic tectonics. We map the boundary between the upper (Churchill) and lower (Superior) plates that collided ∼1.8 Ga and ... Article in Journal/Newspaper Baffin Island Baffin Hudson Bay University of Bristol: Bristol Research Baffin Island Hudson Hudson Bay Geology 39 1 91 94 |
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Open Polar |
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University of Bristol: Bristol Research |
op_collection_id |
ftubristolcris |
language |
English |
description |
The Canadian Shield is one of the largest exposures of Precambrian rocks on Earth. It is a mosaic of several Archean terranes that were brought together during a series of Paleoproterozoic orogens culminating in the so-called Trans-Hudson Orogen (THO), which is thought to have been similar to the Himalayan orogen in scale and nature. The tectonic evolution and lithospheric subdivisions of this region are poorly understood, but new seismic networks in northern Hudson Bay provide fresh opportunity to place constraints on the Precambrian processes that formed and shaped it. We show via a study of seismic anisotropy that the lithosphere of the northern Hudson Bay region retains a strong signature of Archean-to-Paleoproterozoic tectonics. We map the boundary between the upper (Churchill) and lower (Superior) plates that collided ∼1.8 Ga and identify backazimuthdependent splitting parameters (φ, δt) on Baffin Island that indicate complex anisotropy (e.g., dipping fabric) beneath the region. Our results support the view that significant lithospheric deformation occurred during the Paleoproterozoic and that modern-day plate tectonic processes were thus in operation by at least ∼1.8 Ga. The Canadian Shield is one of the largest exposures of Precambrian rocks on Earth. It is a mosaic of several Archean terranes that were brought together during a series of Paleoproterozoic orogens culminating in the so-called Trans-Hudson Orogen (THO), which is thought to have been similar to the Himalayan orogen in scale and nature. The tectonic evolution and lithospheric subdivisions of this region are poorly understood, but new seismic networks in northern Hudson Bay provide fresh opportunity to place constraints on the Precambrian processes that formed and shaped it. We show via a study of seismic anisotropy that the lithosphere of the northern Hudson Bay region retains a strong signature of Archean-to-Paleoproterozoic tectonics. We map the boundary between the upper (Churchill) and lower (Superior) plates that collided ∼1.8 Ga and ... |
format |
Article in Journal/Newspaper |
author |
Bastow, ID Thompson, D.A Wookey, J Kendall, J-M Helffrich, GR Snyder, D Eaton, D Darbyshire, F.A |
spellingShingle |
Bastow, ID Thompson, D.A Wookey, J Kendall, J-M Helffrich, GR Snyder, D Eaton, D Darbyshire, F.A Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
author_facet |
Bastow, ID Thompson, D.A Wookey, J Kendall, J-M Helffrich, GR Snyder, D Eaton, D Darbyshire, F.A |
author_sort |
Bastow, ID |
title |
Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
title_short |
Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
title_full |
Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
title_fullStr |
Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
title_full_unstemmed |
Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay |
title_sort |
precambrian plate tectonics: seismic evidence from northern, hudson bay |
publishDate |
2011 |
url |
https://hdl.handle.net/1983/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://research-information.bris.ac.uk/en/publications/fefd2840-cbb6-4ee1-b6b5-6f735e51a425 https://doi.org/10.1130/G31396.1 |
geographic |
Baffin Island Hudson Hudson Bay |
geographic_facet |
Baffin Island Hudson Hudson Bay |
genre |
Baffin Island Baffin Hudson Bay |
genre_facet |
Baffin Island Baffin Hudson Bay |
op_source |
Bastow , ID , Thompson , D A , Wookey , J , Kendall , J-M , Helffrich , GR , Snyder , D , Eaton , D & Darbyshire , F A 2011 , ' Precambrian Plate Tectonics: Seismic Evidence from Northern, Hudson Bay ' , Geology , vol. 39 , pp. 91 - 94 . https://doi.org/10.1130/G31396.1 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1130/G31396.1 |
container_title |
Geology |
container_volume |
39 |
container_issue |
1 |
container_start_page |
91 |
op_container_end_page |
94 |
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1789330427328069632 |