Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica
Abstract Seismic reflection and borehole data are used to create structure maps of four regional and three local unconformities that constrain the post middle Miocene evolution of the Victoria Land Basin (VLB), which is located in the western Ross Sea within the Late Cretaceous through Quaternary We...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
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Wiley
2020-03-01
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| Series: | Geochemistry, Geophysics, Geosystems |
| Subjects: | |
| Online Access: | https://doi.org/10.1029/2019GC008568 |
| _version_ | 1797638088202125312 |
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| author | Christopher P. Wenman Dennis L. Harry Sumant Jha |
| author_facet | Christopher P. Wenman Dennis L. Harry Sumant Jha |
| author_sort | Christopher P. Wenman |
| collection | DOAJ |
| description | Abstract Seismic reflection and borehole data are used to create structure maps of four regional and three local unconformities that constrain the post middle Miocene evolution of the Victoria Land Basin (VLB), which is located in the western Ross Sea within the Late Cretaceous through Quaternary West Antarctic Rift System. Isochore maps of the strata between unconformities show that rifting was mostly amagmatic between 12 to 7.6 Ma, with subsidence controlled by faults bordering the northwest margin of the basin and in a tectonic zone along the southern basin axis known as the Terror Rift. Depocenters surrounding volcanic features in strata younger than 4.3 Ma indicate an increasing influence of flexure due to volcanic loading on the subsidence pattern in the southern VLB after this time. The intervening period, from 7.6 to 4.3 Ma, was a transitional period during which both extensional tectonism and magmatism exerted strong influences on basin morphology. Since 4.3 Ma, a series of flexural subbasins formed successively at different times and positions as the different volcanic centers that built Ross Island erupted. In composite, these subbasins form a flexural moat surrounding Ross Island and smaller volcanic centers immediately to the north. The widths of these basins indicate that the flexural rigidity of the lithosphere ranges from 0.20 × 1019 to 12.96 × 1019 N‐m (elastic thickness 0.6 to 2.4 km). |
| first_indexed | 2024-03-11T12:58:38Z |
| format | Article |
| id | doaj.art-82aa98cfa14c4d459257173189051910 |
| institution | Directory Open Access Journal |
| issn | 1525-2027 |
| language | English |
| last_indexed | 2024-03-11T12:58:38Z |
| publishDate | 2020-03-01 |
| publisher | Wiley |
| record_format | Article |
| series | Geochemistry, Geophysics, Geosystems |
| spelling | doaj.art-82aa98cfa14c4d4592571731890519102023-11-03T16:55:58ZengWileyGeochemistry, Geophysics, Geosystems1525-20272020-03-01213n/an/a10.1029/2019GC008568Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West AntarcticaChristopher P. Wenman0Dennis L. Harry1Sumant Jha2Department of Geosciences Colorado State University Fort Collins CO USADepartment of Geosciences Colorado State University Fort Collins CO USADepartment of Geosciences Colorado State University Fort Collins CO USAAbstract Seismic reflection and borehole data are used to create structure maps of four regional and three local unconformities that constrain the post middle Miocene evolution of the Victoria Land Basin (VLB), which is located in the western Ross Sea within the Late Cretaceous through Quaternary West Antarctic Rift System. Isochore maps of the strata between unconformities show that rifting was mostly amagmatic between 12 to 7.6 Ma, with subsidence controlled by faults bordering the northwest margin of the basin and in a tectonic zone along the southern basin axis known as the Terror Rift. Depocenters surrounding volcanic features in strata younger than 4.3 Ma indicate an increasing influence of flexure due to volcanic loading on the subsidence pattern in the southern VLB after this time. The intervening period, from 7.6 to 4.3 Ma, was a transitional period during which both extensional tectonism and magmatism exerted strong influences on basin morphology. Since 4.3 Ma, a series of flexural subbasins formed successively at different times and positions as the different volcanic centers that built Ross Island erupted. In composite, these subbasins form a flexural moat surrounding Ross Island and smaller volcanic centers immediately to the north. The widths of these basins indicate that the flexural rigidity of the lithosphere ranges from 0.20 × 1019 to 12.96 × 1019 N‐m (elastic thickness 0.6 to 2.4 km).https://doi.org/10.1029/2019GC008568AntarcticaWest Antarctic RiftVictoria Land BasinRoss Seaflexurecontinental rift |
| spellingShingle | Christopher P. Wenman Dennis L. Harry Sumant Jha Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica Geochemistry, Geophysics, Geosystems Antarctica West Antarctic Rift Victoria Land Basin Ross Sea flexure continental rift |
| title | Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica |
| title_full | Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica |
| title_fullStr | Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica |
| title_full_unstemmed | Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica |
| title_short | Post Middle Miocene Tectonomagmatic and Stratigraphic Evolution of the Victoria Land Basin, West Antarctica |
| title_sort | post middle miocene tectonomagmatic and stratigraphic evolution of the victoria land basin west antarctica |
| topic | Antarctica West Antarctic Rift Victoria Land Basin Ross Sea flexure continental rift |
| url | https://doi.org/10.1029/2019GC008568 |
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