Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia
Published online: 16 Oct 2018. Recently acquired seismic data in the eastern portion of the Amadeus Basin of central Australia have enabled disconformities at the base of both the Sturt and Elatina glaciogenic sequences within the Neoproterozoic succession to be mapped on a semi-regional scale. On a...
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Online Access: | http://hdl.handle.net/2440/123599 https://doi.org/10.1080/08120099.2018.1512159 |
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ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/123599 2023-12-17T10:31:46+01:00 Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia Plummer, P. 2019 http://hdl.handle.net/2440/123599 https://doi.org/10.1080/08120099.2018.1512159 en eng Taylor & Francis Australian Journal of Earth Sciences, 2019; 66(1):47-55 0812-0099 1440-0952 http://hdl.handle.net/2440/123599 doi:10.1080/08120099.2018.1512159 Plummer, P. [0000-0002-5134-9945] © 2018 Geological Society of Australia http://dx.doi.org/10.1080/08120099.2018.1512159 Amadeus Basin central Australia Neoproterozoic Areyonga Formation Olympic/Pioneer Formation seismic glaciation disconformity Grounded Zone Wedge Tunnel Valley Journal article 2019 ftunivadelaidedl https://doi.org/10.1080/08120099.2018.1512159 2023-11-20T23:32:39Z Published online: 16 Oct 2018. Recently acquired seismic data in the eastern portion of the Amadeus Basin of central Australia have enabled disconformities at the base of both the Sturt and Elatina glaciogenic sequences within the Neoproterozoic succession to be mapped on a semi-regional scale. On a more detailed scale, along the shallowly shelving eastern flank of the basin, seismic data have revealed features that demarcate the transition from a grounded to floating, or possible absent, Sturt ice-sheet. Coincident with this transition is an extensive mound-like accumulation of glacial debris, some 10 to 15km wide, 300 m high and extending at least 150km subparallel to the northeast–southwest-oriented basin margin. This glacial debris entered the basin subglacially through meandering tunnel valleys, one of which can be mapped seismically. P. Plummer Article in Journal/Newspaper Ice Sheet The University of Adelaide: Digital Library Australian Journal of Earth Sciences 66 1 47 55 |
institution |
Open Polar |
collection |
The University of Adelaide: Digital Library |
op_collection_id |
ftunivadelaidedl |
language |
English |
topic |
Amadeus Basin central Australia Neoproterozoic Areyonga Formation Olympic/Pioneer Formation seismic glaciation disconformity Grounded Zone Wedge Tunnel Valley |
spellingShingle |
Amadeus Basin central Australia Neoproterozoic Areyonga Formation Olympic/Pioneer Formation seismic glaciation disconformity Grounded Zone Wedge Tunnel Valley Plummer, P. Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
topic_facet |
Amadeus Basin central Australia Neoproterozoic Areyonga Formation Olympic/Pioneer Formation seismic glaciation disconformity Grounded Zone Wedge Tunnel Valley |
description |
Published online: 16 Oct 2018. Recently acquired seismic data in the eastern portion of the Amadeus Basin of central Australia have enabled disconformities at the base of both the Sturt and Elatina glaciogenic sequences within the Neoproterozoic succession to be mapped on a semi-regional scale. On a more detailed scale, along the shallowly shelving eastern flank of the basin, seismic data have revealed features that demarcate the transition from a grounded to floating, or possible absent, Sturt ice-sheet. Coincident with this transition is an extensive mound-like accumulation of glacial debris, some 10 to 15km wide, 300 m high and extending at least 150km subparallel to the northeast–southwest-oriented basin margin. This glacial debris entered the basin subglacially through meandering tunnel valleys, one of which can be mapped seismically. P. Plummer |
format |
Article in Journal/Newspaper |
author |
Plummer, P. |
author_facet |
Plummer, P. |
author_sort |
Plummer, P. |
title |
Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
title_short |
Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
title_full |
Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
title_fullStr |
Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
title_full_unstemmed |
Seismic images grounded zone wedge in Neoproterozoic glacials, Amadeus Basin, central Australia |
title_sort |
seismic images grounded zone wedge in neoproterozoic glacials, amadeus basin, central australia |
publisher |
Taylor & Francis |
publishDate |
2019 |
url |
http://hdl.handle.net/2440/123599 https://doi.org/10.1080/08120099.2018.1512159 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://dx.doi.org/10.1080/08120099.2018.1512159 |
op_relation |
Australian Journal of Earth Sciences, 2019; 66(1):47-55 0812-0099 1440-0952 http://hdl.handle.net/2440/123599 doi:10.1080/08120099.2018.1512159 Plummer, P. [0000-0002-5134-9945] |
op_rights |
© 2018 Geological Society of Australia |
op_doi |
https://doi.org/10.1080/08120099.2018.1512159 |
container_title |
Australian Journal of Earth Sciences |
container_volume |
66 |
container_issue |
1 |
container_start_page |
47 |
op_container_end_page |
55 |
_version_ |
1785585164345147392 |