Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau
Valdivia Bank is an oceanic plateau in the South Atlantic formed by hot spot magmatism at the Mid-Atlantic Ridge during the Late Cretaceous. It is part of the Walvis Ridge, an aseismic ridge and seamount chain widely considered to be formed by age-progressive volcanism from the Tristan-Gough plume....
Published in: | Geochemistry, Geophysics, Geosystems |
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Language: | English |
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AGU (American Geophysical Union)
2022
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Online Access: | https://oceanrep.geomar.de/id/eprint/57410/ https://oceanrep.geomar.de/id/eprint/57410/1/ContrerasetalG3_2022.pdf https://doi.org/10.1029/2022GC010624 |
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ftoceanrep:oai:oceanrep.geomar.de:57410 2024-02-11T10:08:38+01:00 Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau Contreras, E. García, P. Jiménez Sager, W. W. Thoram, S. Hoernle, Kaj Sarralde, R. Zhou, H. 2022-11-04 text https://oceanrep.geomar.de/id/eprint/57410/ https://oceanrep.geomar.de/id/eprint/57410/1/ContrerasetalG3_2022.pdf https://doi.org/10.1029/2022GC010624 en eng AGU (American Geophysical Union) Wiley https://oceanrep.geomar.de/id/eprint/57410/1/ContrerasetalG3_2022.pdf Contreras, E., García, P. J., Sager, W. W., Thoram, S., Hoernle, K. , Sarralde, R. and Zhou, H. (2022) Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau. Open Access Geochemistry, Geophysics, Geosystems, 23 (11). Art.Nr. e2022GC010624. DOI 10.1029/2022GC010624 <https://doi.org/10.1029/2022GC010624>. doi:10.1029/2022GC010624 cc_by_nc_nd_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed info:eu-repo/semantics/article 2022 ftoceanrep https://doi.org/10.1029/2022GC010624 2024-01-15T00:26:28Z Valdivia Bank is an oceanic plateau in the South Atlantic formed by hot spot magmatism at the Mid-Atlantic Ridge during the Late Cretaceous. It is part of the Walvis Ridge, an aseismic ridge and seamount chain widely considered to be formed by age-progressive volcanism from the Tristan-Gough plume. To better understand the formation and history of this edifice, we developed a bathymetric map of Valdivia Bank by merging available multibeam echosounder data sets with a bathymetry grid based mainly on satellite altimetry (SRTM15+). The bathymetric map reveals previously unresolved features including extensive rift grabens, volcanic mounds and knolls, and large-scale sediment transport systems. After Valdivia Bank was emplaced and probably eroded at sea level, it underwent a period of rifting, followed by a secondary magmatic pulse that caused regional uplift to sea-level, followed by subsidence to current depths. Shallow banks at depths of ∼1,000 m are the result of a thick sediment pile atop uplifted volcanic crust. Several shallower mounds (∼1,000–520 m) and a guyot (∼220 m) likely resulted from coral reef growth atop one or more volcanic pedestals formed during the younger Cenozoic magmatic event. As sediments accumulated on the shallow platforms, sediment transport systems developed as gullies, channels and mass transport deposits carved valleys and troughs, shedding sediment into abyssal fans at the plateau base. The new bathymetric map demonstrates that oceanic plateaus are geologically active long after initial emplacement. Key Points - A bathymetry map was constructed for Valdivia Bank from multibeam data merged with satellite altimetry-predicted depths - Valdivia Bank experienced extension, forming rifts, and secondary volcanism, uplift, and exposure, then was capped by carbonate sediments - Valdivia Bank shows evidence of mass wasting, partly triggered by Cenozoic uplift and erosion, but also owing to sediment cap instability Article in Journal/Newspaper South Atlantic Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Gough ENVELOPE(159.367,159.367,-81.633,-81.633) Mid-Atlantic Ridge Tristan ENVELOPE(140.900,140.900,-66.735,-66.735) Geochemistry, Geophysics, Geosystems 23 11 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Valdivia Bank is an oceanic plateau in the South Atlantic formed by hot spot magmatism at the Mid-Atlantic Ridge during the Late Cretaceous. It is part of the Walvis Ridge, an aseismic ridge and seamount chain widely considered to be formed by age-progressive volcanism from the Tristan-Gough plume. To better understand the formation and history of this edifice, we developed a bathymetric map of Valdivia Bank by merging available multibeam echosounder data sets with a bathymetry grid based mainly on satellite altimetry (SRTM15+). The bathymetric map reveals previously unresolved features including extensive rift grabens, volcanic mounds and knolls, and large-scale sediment transport systems. After Valdivia Bank was emplaced and probably eroded at sea level, it underwent a period of rifting, followed by a secondary magmatic pulse that caused regional uplift to sea-level, followed by subsidence to current depths. Shallow banks at depths of ∼1,000 m are the result of a thick sediment pile atop uplifted volcanic crust. Several shallower mounds (∼1,000–520 m) and a guyot (∼220 m) likely resulted from coral reef growth atop one or more volcanic pedestals formed during the younger Cenozoic magmatic event. As sediments accumulated on the shallow platforms, sediment transport systems developed as gullies, channels and mass transport deposits carved valleys and troughs, shedding sediment into abyssal fans at the plateau base. The new bathymetric map demonstrates that oceanic plateaus are geologically active long after initial emplacement. Key Points - A bathymetry map was constructed for Valdivia Bank from multibeam data merged with satellite altimetry-predicted depths - Valdivia Bank experienced extension, forming rifts, and secondary volcanism, uplift, and exposure, then was capped by carbonate sediments - Valdivia Bank shows evidence of mass wasting, partly triggered by Cenozoic uplift and erosion, but also owing to sediment cap instability |
format |
Article in Journal/Newspaper |
author |
Contreras, E. García, P. Jiménez Sager, W. W. Thoram, S. Hoernle, Kaj Sarralde, R. Zhou, H. |
spellingShingle |
Contreras, E. García, P. Jiménez Sager, W. W. Thoram, S. Hoernle, Kaj Sarralde, R. Zhou, H. Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
author_facet |
Contreras, E. García, P. Jiménez Sager, W. W. Thoram, S. Hoernle, Kaj Sarralde, R. Zhou, H. |
author_sort |
Contreras, E. |
title |
Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
title_short |
Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
title_full |
Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
title_fullStr |
Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
title_full_unstemmed |
Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau |
title_sort |
bathymetry of valdivia bank, walvis ridge, south atlantic ocean: implications for structure and geologic history of a hot spot plateau |
publisher |
AGU (American Geophysical Union) |
publishDate |
2022 |
url |
https://oceanrep.geomar.de/id/eprint/57410/ https://oceanrep.geomar.de/id/eprint/57410/1/ContrerasetalG3_2022.pdf https://doi.org/10.1029/2022GC010624 |
long_lat |
ENVELOPE(159.367,159.367,-81.633,-81.633) ENVELOPE(140.900,140.900,-66.735,-66.735) |
geographic |
Gough Mid-Atlantic Ridge Tristan |
geographic_facet |
Gough Mid-Atlantic Ridge Tristan |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
https://oceanrep.geomar.de/id/eprint/57410/1/ContrerasetalG3_2022.pdf Contreras, E., García, P. J., Sager, W. W., Thoram, S., Hoernle, K. , Sarralde, R. and Zhou, H. (2022) Bathymetry of Valdivia Bank, Walvis Ridge, South Atlantic Ocean: Implications for Structure and Geologic History of a Hot Spot Plateau. Open Access Geochemistry, Geophysics, Geosystems, 23 (11). Art.Nr. e2022GC010624. DOI 10.1029/2022GC010624 <https://doi.org/10.1029/2022GC010624>. doi:10.1029/2022GC010624 |
op_rights |
cc_by_nc_nd_4.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2022GC010624 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
23 |
container_issue |
11 |
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1790608063175065600 |