GPS Surveys to detect active faulting in the Transantarctic Mountains
Summary The Transantarctic Mountains Deformation (TAMDEF) network is a GPS array deployed on bedrock throughout the Victoria Land region of Antarctica, aimed at investigating modern vertical and horizontal crustal motions. Embedded within this network are three local GPS arrays established around kn...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.537.8698 2023-05-15T13:52:00+02:00 GPS Surveys to detect active faulting in the Transantarctic Mountains S. A. Konfal T. J. Wilson M. J. Willis The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.8698 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.8698 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf text ftciteseerx 2016-01-08T10:53:56Z Summary The Transantarctic Mountains Deformation (TAMDEF) network is a GPS array deployed on bedrock throughout the Victoria Land region of Antarctica, aimed at investigating modern vertical and horizontal crustal motions. Embedded within this network are three local GPS arrays established around known or potential neotectonic faults to test for modern fault displacements. These local fault arrays were surveyed a minimum of three times between the 1996-97 and 2005-06 austral summer field seasons. Preliminary analysis of baseline length changes is consistent with active extension, suggesting there may be modern tectonic activity in the West Antarctic Rift System. Text Antarc* Antarctic Antarctica Victoria Land Unknown Antarctic Austral Transantarctic Mountains Victoria Land |
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ftciteseerx |
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English |
description |
Summary The Transantarctic Mountains Deformation (TAMDEF) network is a GPS array deployed on bedrock throughout the Victoria Land region of Antarctica, aimed at investigating modern vertical and horizontal crustal motions. Embedded within this network are three local GPS arrays established around known or potential neotectonic faults to test for modern fault displacements. These local fault arrays were surveyed a minimum of three times between the 1996-97 and 2005-06 austral summer field seasons. Preliminary analysis of baseline length changes is consistent with active extension, suggesting there may be modern tectonic activity in the West Antarctic Rift System. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
S. A. Konfal T. J. Wilson M. J. Willis |
spellingShingle |
S. A. Konfal T. J. Wilson M. J. Willis GPS Surveys to detect active faulting in the Transantarctic Mountains |
author_facet |
S. A. Konfal T. J. Wilson M. J. Willis |
author_sort |
S. A. Konfal |
title |
GPS Surveys to detect active faulting in the Transantarctic Mountains |
title_short |
GPS Surveys to detect active faulting in the Transantarctic Mountains |
title_full |
GPS Surveys to detect active faulting in the Transantarctic Mountains |
title_fullStr |
GPS Surveys to detect active faulting in the Transantarctic Mountains |
title_full_unstemmed |
GPS Surveys to detect active faulting in the Transantarctic Mountains |
title_sort |
gps surveys to detect active faulting in the transantarctic mountains |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.8698 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf |
geographic |
Antarctic Austral Transantarctic Mountains Victoria Land |
geographic_facet |
Antarctic Austral Transantarctic Mountains Victoria Land |
genre |
Antarc* Antarctic Antarctica Victoria Land |
genre_facet |
Antarc* Antarctic Antarctica Victoria Land |
op_source |
http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.537.8698 http://pubs.usgs.gov/of/2007/1047/ea/of2007-1047ea021.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766256158847270912 |