Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ...
The Transantarctic Mountains (TAM) form the high western rift flank of the West Antarctic Rift System (WARS), a region of extended crust that separates East and West Antarctica. Little is known about the structural geology in the southern TAM due to limited accessibility and more ice cover than in t...
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ftdatacite:10.26153/tsw/2786 2024-03-31T07:49:16+00:00 Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... Davis, Marcy B. 2001 electronic https://dx.doi.org/10.26153/tsw/2786 https://repositories.lib.utexas.edu/handle/2152/75682 en eng The University of Texas at Austin Open Copyright © is held by the author. Presentation of this material on the Libraries' web site by University Libraries, The University of Texas at Austin was made possible under a limited license grant from the author who has retained all copyrights in the works. Geomorphology--Antarctica--Transantarctic Mountains Geology, Structural--Antarctica--Transantarctic Mountains Geophysical surveys--Antarctica--Transantarctic Mountains Text article-journal Thesis ScholarlyArticle 2001 ftdatacite https://doi.org/10.26153/tsw/2786 2024-03-04T14:05:02Z The Transantarctic Mountains (TAM) form the high western rift flank of the West Antarctic Rift System (WARS), a region of extended crust that separates East and West Antarctica. Little is known about the structural geology in the southern TAM due to limited accessibility and more ice cover than in the central and northern TAM. The objectives of this study are to characterize the subglacial bedrock morphology interior of the southern TAM and to define the structural geology along the southern TAM Front through analysis of airborne ice-penetrating radar data. The airborne survey extended from the Ross Ice Shelf, southward over the TAM along the 150°W meridian and between the Scott and Reedy Glaciers then over the high plateau and through the South Pole. Approximately 15,000 line km were flown and processed using finite difference migration techniques in a seismic processing software package. Subsequently, the ice and bed surfaces were picked along each line and known geology was interpreted on the radar ... Thesis Antarc* Antarctic Antarctica Ice Shelf Ross Ice Shelf South pole South pole West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic Ross Ice Shelf South Pole Transantarctic Mountains West Antarctica |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Geomorphology--Antarctica--Transantarctic Mountains Geology, Structural--Antarctica--Transantarctic Mountains Geophysical surveys--Antarctica--Transantarctic Mountains |
spellingShingle |
Geomorphology--Antarctica--Transantarctic Mountains Geology, Structural--Antarctica--Transantarctic Mountains Geophysical surveys--Antarctica--Transantarctic Mountains Davis, Marcy B. Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
topic_facet |
Geomorphology--Antarctica--Transantarctic Mountains Geology, Structural--Antarctica--Transantarctic Mountains Geophysical surveys--Antarctica--Transantarctic Mountains |
description |
The Transantarctic Mountains (TAM) form the high western rift flank of the West Antarctic Rift System (WARS), a region of extended crust that separates East and West Antarctica. Little is known about the structural geology in the southern TAM due to limited accessibility and more ice cover than in the central and northern TAM. The objectives of this study are to characterize the subglacial bedrock morphology interior of the southern TAM and to define the structural geology along the southern TAM Front through analysis of airborne ice-penetrating radar data. The airborne survey extended from the Ross Ice Shelf, southward over the TAM along the 150°W meridian and between the Scott and Reedy Glaciers then over the high plateau and through the South Pole. Approximately 15,000 line km were flown and processed using finite difference migration techniques in a seismic processing software package. Subsequently, the ice and bed surfaces were picked along each line and known geology was interpreted on the radar ... |
format |
Thesis |
author |
Davis, Marcy B. |
author_facet |
Davis, Marcy B. |
author_sort |
Davis, Marcy B. |
title |
Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
title_short |
Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
title_full |
Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
title_fullStr |
Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
title_full_unstemmed |
Subglacial morphology and structural geology in the southern Transantarctic Mountains from airborne geophysics ... |
title_sort |
subglacial morphology and structural geology in the southern transantarctic mountains from airborne geophysics ... |
publisher |
The University of Texas at Austin |
publishDate |
2001 |
url |
https://dx.doi.org/10.26153/tsw/2786 https://repositories.lib.utexas.edu/handle/2152/75682 |
geographic |
Antarctic Ross Ice Shelf South Pole Transantarctic Mountains West Antarctica |
geographic_facet |
Antarctic Ross Ice Shelf South Pole Transantarctic Mountains West Antarctica |
genre |
Antarc* Antarctic Antarctica Ice Shelf Ross Ice Shelf South pole South pole West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Shelf Ross Ice Shelf South pole South pole West Antarctica |
op_rights |
Open Copyright © is held by the author. Presentation of this material on the Libraries' web site by University Libraries, The University of Texas at Austin was made possible under a limited license grant from the author who has retained all copyrights in the works. |
op_doi |
https://doi.org/10.26153/tsw/2786 |
_version_ |
1795038375001980928 |