Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution
The Gorringe Bank is a 5000 m high seamount near the Atlantic coast of Iberia characterized by a 9 m high geoid anomaly and a ∼120 mGal Bouguer anomaly relative to the surrounding abyssal plains. It has been linked to a NW directed thrust carrying exhumed upper mantle rocks and transitional crust on...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/80bc7e15-1d4f-4edc-9ebc-2a90ed9a389a 2024-09-15T18:20:17+00:00 Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution Jiménez-Munt, I. Fernàndez, M. Vergés, J. Afonso, J. C. Garcia-Castellanos, D. Fullea, J. 2010-10-01 application/pdf https://researchers.mq.edu.au/en/publications/80bc7e15-1d4f-4edc-9ebc-2a90ed9a389a https://doi.org/10.1029/2009TC002458 https://research-management.mq.edu.au/ws/files/62413161/Publisher%20version%20(open%20access).pdf http://www.scopus.com/inward/record.url?scp=78149342431&partnerID=8YFLogxK eng eng info:eu-repo/semantics/openAccess Jiménez-Munt , I , Fernàndez , M , Vergés , J , Afonso , J C , Garcia-Castellanos , D & Fullea , J 2010 , ' Lithospheric structure of the Gorringe Bank : Insights into its origin and tectonic evolution ' , Tectonics , vol. 29 , no. 5 , TC5019 , pp. 1-16 . https://doi.org/10.1029/2009TC002458 article 2010 ftmacquarieunicr https://doi.org/10.1029/2009TC002458 2024-08-28T23:47:18Z The Gorringe Bank is a 5000 m high seamount near the Atlantic coast of Iberia characterized by a 9 m high geoid anomaly and a ∼120 mGal Bouguer anomaly relative to the surrounding abyssal plains. It has been linked to a NW directed thrust carrying exhumed upper mantle rocks and transitional crust on top of flexed-down Eurasian oceanic crust along the Tagus Abyssal Plain. However, estimations of crustal shortening have yielded dissimilar results, and the deep structure of the ridge remains highly unknown. We present a restored cross section and a new model of the lithospheric structure based on gravity, geoid, elevation, and the presence of serpentinized peridotites. At least 20 km of shortening took place along a flat-ramp-flat thrust fault, and the density structure of the lithosphere is consistent with mantle serpentinization varying from 70% at the surface to 20% at 14 km depth and 0% at 40 km. The topographic relief and gravity anomalies are explained by assuming a flexural isostatic model with an elastic thickness T e of ∼30 km. The evolution of the Gorringe Bank since the Late Jurassic is interpreted in relation to Eurasia-Africa-North America plate motion in four stages: (1) transtension between Newfoundland-Iberia and Africa, which generated small oceanic basins and mantle exhumation; (2) opening of the North Atlantic and seafloor spreading at the NW side of the exhumed Gorringe, which produced gabbro intrusions and serpentinization; (3) a quiescent tectonic period dominated by subsidence and sediment accumulation; and (4) a transpressional plate boundary between Eurasia and Africa with NW directed subcrustal thrusting and generation of the present Gorringe relief. Article in Journal/Newspaper Newfoundland North Atlantic Macquarie University Research Portal Tectonics 29 5 n/a n/a |
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Open Polar |
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Macquarie University Research Portal |
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ftmacquarieunicr |
language |
English |
description |
The Gorringe Bank is a 5000 m high seamount near the Atlantic coast of Iberia characterized by a 9 m high geoid anomaly and a ∼120 mGal Bouguer anomaly relative to the surrounding abyssal plains. It has been linked to a NW directed thrust carrying exhumed upper mantle rocks and transitional crust on top of flexed-down Eurasian oceanic crust along the Tagus Abyssal Plain. However, estimations of crustal shortening have yielded dissimilar results, and the deep structure of the ridge remains highly unknown. We present a restored cross section and a new model of the lithospheric structure based on gravity, geoid, elevation, and the presence of serpentinized peridotites. At least 20 km of shortening took place along a flat-ramp-flat thrust fault, and the density structure of the lithosphere is consistent with mantle serpentinization varying from 70% at the surface to 20% at 14 km depth and 0% at 40 km. The topographic relief and gravity anomalies are explained by assuming a flexural isostatic model with an elastic thickness T e of ∼30 km. The evolution of the Gorringe Bank since the Late Jurassic is interpreted in relation to Eurasia-Africa-North America plate motion in four stages: (1) transtension between Newfoundland-Iberia and Africa, which generated small oceanic basins and mantle exhumation; (2) opening of the North Atlantic and seafloor spreading at the NW side of the exhumed Gorringe, which produced gabbro intrusions and serpentinization; (3) a quiescent tectonic period dominated by subsidence and sediment accumulation; and (4) a transpressional plate boundary between Eurasia and Africa with NW directed subcrustal thrusting and generation of the present Gorringe relief. |
format |
Article in Journal/Newspaper |
author |
Jiménez-Munt, I. Fernàndez, M. Vergés, J. Afonso, J. C. Garcia-Castellanos, D. Fullea, J. |
spellingShingle |
Jiménez-Munt, I. Fernàndez, M. Vergés, J. Afonso, J. C. Garcia-Castellanos, D. Fullea, J. Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
author_facet |
Jiménez-Munt, I. Fernàndez, M. Vergés, J. Afonso, J. C. Garcia-Castellanos, D. Fullea, J. |
author_sort |
Jiménez-Munt, I. |
title |
Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
title_short |
Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
title_full |
Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
title_fullStr |
Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
title_full_unstemmed |
Lithospheric structure of the Gorringe Bank:Insights into its origin and tectonic evolution |
title_sort |
lithospheric structure of the gorringe bank:insights into its origin and tectonic evolution |
publishDate |
2010 |
url |
https://researchers.mq.edu.au/en/publications/80bc7e15-1d4f-4edc-9ebc-2a90ed9a389a https://doi.org/10.1029/2009TC002458 https://research-management.mq.edu.au/ws/files/62413161/Publisher%20version%20(open%20access).pdf http://www.scopus.com/inward/record.url?scp=78149342431&partnerID=8YFLogxK |
genre |
Newfoundland North Atlantic |
genre_facet |
Newfoundland North Atlantic |
op_source |
Jiménez-Munt , I , Fernàndez , M , Vergés , J , Afonso , J C , Garcia-Castellanos , D & Fullea , J 2010 , ' Lithospheric structure of the Gorringe Bank : Insights into its origin and tectonic evolution ' , Tectonics , vol. 29 , no. 5 , TC5019 , pp. 1-16 . https://doi.org/10.1029/2009TC002458 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2009TC002458 |
container_title |
Tectonics |
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29 |
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5 |
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1810458654439112704 |