Authors / CoAuthors
Close, D. | Stagg, H.M.J. | O'Brien, P.E.
Abstract
Seismic reflection data show the existence of two major sedimentary basins along the continental margin of Wilkes Land and Terre Adélie, East Antarctica, that contain more than 5 s TWT (> 9 km) of sediments. Four seismic megasequences are identified (MS4 to MS1) that are bounded by: basement, unconformities of interpreted Turonian, Maastrichtian and early Middle Eocene age, and the seafloor. The 4-5 km thick rift and pre-rift sediments are concentrated in a margin-parallel basin (Sabrina Basin). On the basis of seismic correlation with the Australian margin, this basin is interpreted to be of Late Jurassic to mid-Cretaceous age. The post-rift sediments are generally thick along the margin and in the adjacent deep-ocean basin, but are particularly thick in a major depocentre off west Wilkes Land, named here the Budd Coast Basin (BCB). The BCB contains a maximum observed thickness of 5 s TWT (9 km) of post-rift sediments and its location suggests that the sediments were largely derived from a sub-glacial basin currently occupied by the Totten Glacier.
Product Type
nonGeographicDataset
eCat Id
70223
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Custodian
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
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Keywords
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- External PublicationScientific Journal Paper
- ( Theme )
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- Antarctic data
- ( Theme )
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- stratigraphy
- ( Theme )
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- sedimentology
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- marine
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- geomorphology
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- AQ
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_External
Publication Date
2006-01-01T00:00:00
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Topic Category
geoscientificInformation
Series Information
239
Lineage
Unknown
Parent Information
Extents
[-69.0, -60.0, 110.0, 154.0]
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