Table 1: Station data for the entire survey, including coordinates and description of BPBASE ...
During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimsto...
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Online Access: | https://dx.doi.org/10.1594/pangaea.763366 https://doi.pangaea.de/10.1594/PANGAEA.763366 |
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ftdatacite:10.1594/pangaea.763366 2024-09-15T18:35:30+00:00 Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... Redfield, Tim Behrendt, John Damaske, Detlef Delisle, Georg Möller, Dieter Sievers, Joachim 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.763366 https://doi.pangaea.de/10.1594/PANGAEA.763366 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Station label LATITUDE LONGITUDE ELEVATION Sea ice thickness Correction Bouguer anomaly Gravimetry dataset Supplementary Dataset Dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.763366 2024-08-01T11:01:17Z During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimstone Peak, near the western end of the regional profile. The survey south of the Drygalski has been connected to northern gravity data (GANOVEX V) by a survey line of 12 points. All data have been terrain corrected, and are further constrained by satellite elevation (GPS) and radar ice-thickness measurements. A pronounced regional Bouguer gravity gradient decreasing to the west by approximately 3 mgal/km is superimposed over a coast-parallel belt of granitoid basement rock. West of this belt the local gravity fields become mote variable. Over Beta Peak (Ferrar dolerite) a 50 mgal spike is obser- ved. Within this area, the Ferrar sills are exposed at the surface. West of Brimstone Peak (Ferrar/Kirk patrick ... : Supplement to: Redfield, Tim; Behrendt, John; Damaske, Detlef; Delisle, Georg; Möller, Dieter; Sievers, Joachim (1992): 21. Gravity transect across the Transantarctic Mountains South of the Drygalski lce Tongue. Polarforschung, 60(2), 143-151 ... Dataset Sea ice Victoria Land DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Station label LATITUDE LONGITUDE ELEVATION Sea ice thickness Correction Bouguer anomaly Gravimetry |
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Event label Station label LATITUDE LONGITUDE ELEVATION Sea ice thickness Correction Bouguer anomaly Gravimetry Redfield, Tim Behrendt, John Damaske, Detlef Delisle, Georg Möller, Dieter Sievers, Joachim Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
topic_facet |
Event label Station label LATITUDE LONGITUDE ELEVATION Sea ice thickness Correction Bouguer anomaly Gravimetry |
description |
During GANOVEX VI new gravity data were collected along an east-west profile in North Victoria Land south of the Drygalski Ice Tongue, extending 150 km across the Transantarctic Mountains, and comprising 21 data points. Thirty five additional data points were collected over a small area near Brimstone Peak, near the western end of the regional profile. The survey south of the Drygalski has been connected to northern gravity data (GANOVEX V) by a survey line of 12 points. All data have been terrain corrected, and are further constrained by satellite elevation (GPS) and radar ice-thickness measurements. A pronounced regional Bouguer gravity gradient decreasing to the west by approximately 3 mgal/km is superimposed over a coast-parallel belt of granitoid basement rock. West of this belt the local gravity fields become mote variable. Over Beta Peak (Ferrar dolerite) a 50 mgal spike is obser- ved. Within this area, the Ferrar sills are exposed at the surface. West of Brimstone Peak (Ferrar/Kirk patrick ... : Supplement to: Redfield, Tim; Behrendt, John; Damaske, Detlef; Delisle, Georg; Möller, Dieter; Sievers, Joachim (1992): 21. Gravity transect across the Transantarctic Mountains South of the Drygalski lce Tongue. Polarforschung, 60(2), 143-151 ... |
format |
Dataset |
author |
Redfield, Tim Behrendt, John Damaske, Detlef Delisle, Georg Möller, Dieter Sievers, Joachim |
author_facet |
Redfield, Tim Behrendt, John Damaske, Detlef Delisle, Georg Möller, Dieter Sievers, Joachim |
author_sort |
Redfield, Tim |
title |
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
title_short |
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
title_full |
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
title_fullStr |
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
title_full_unstemmed |
Table 1: Station data for the entire survey, including coordinates and description of BPBASE ... |
title_sort |
table 1: station data for the entire survey, including coordinates and description of bpbase ... |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://dx.doi.org/10.1594/pangaea.763366 https://doi.pangaea.de/10.1594/PANGAEA.763366 |
genre |
Sea ice Victoria Land |
genre_facet |
Sea ice Victoria Land |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.763366 |
_version_ |
1810478683069087744 |